EUROPEAN UNION COHESION FUND
Project No. POIS.07.02.00-00-029 / 13 "Modernization of Swinoujscie-Szczecin to a depth of 12.5 m - preparatory work" co-financed by the European Union from the Cohesion Fund under the Operational Program Infrastructure and Environment. Grant agreement POIS.07.02.00-00-029 / 13-00.
MODERNIZACJA fairway ŚWINOUJŚCIE-SZCZECIN FOR DEPTH 12.5 M - PREPARATORY WORK
The report of the environmental impact of the project entitled: "Modernization fairway Śwonoujście - Szczecin to a depth of 12.5 m"
VOLUME III - meeting the requirements of the Water Framework Directive
CLIENT: CONTRACTOR:
Maritime Office SZCZECINIEEuroprojekt Gdańsk ARE Batory Square 4UL. Nadwiślańska 55 70-207 Szczecin80-680 gdańsk
GDA SK S SZCZECIN, November 2 0 1 5
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Reported by:
dr. Dorothy Dybkowska‐Stefek
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
CONTENTS OF STUDY
1. Report on the impact of the project on the environment THIS TO ME ‐ the essential content of the report specifying the environmental conditions, in terms of the impact on the basic elements of the environment for the planned project, VOLUME II ‐ meeting the requirements of Art. 6 (3) and (4) Habitats Directive VOLUME III ‐ meeting the requirements of Water Framework Directive. TOM V ‐ a summary of non‐specialist.
2. DETAILED CONTENTS: 1. Basis report. 6 2. Subject matter and scope of the report. 6 3 Description of the projects planned within the Project and investments related to it. 7 4. Analysis and evaluation of the impact of the Project for the purposes of water conservation. 27 4.1. Stage I. 27 4.1.1. Identification of water bodies and the objectives assigned to them 27 environmental. 4.1.2. Characteristics JCW. 40 4.1.3. Qualification in terms of hydro‐morphological changes. 54 4.1.4. Assessment of the current status of water bodies. 59 4.2. Step II. 84 4.2.1. Identification of factors impact on the quality elements of the Project 84 water. 4.2.2. Determining the list of indicators of water quality that are potentially under85 impact of the identified factors impact. 4.2.3. Evaluation of the impact of the Project on selected indicators of water quality. 86 4.2.4. Evaluation of the impact of the Project on protected areas. 150 4.2.5. Conclusions. 180 5. Design Assessment for fulfillment of the conditions referred to in Article. 4 paragraph. 7 WFD. 181 6. Materials used. 190 Annex 1 card JCWP Świna Estuary. Appendix 2. Card JCWP Szczecin Lagoon. Appendix 3. Measles JCWP card from Párnica to the mouth. Annex 1 card PLGW0001 groundwater bodies. Annex 1 card PLGW0004 groundwater bodies. Annex 1 card PLGW0007 groundwater bodies.
3. TOM IV ‐ Annexes graphic, tabular and textual
ANNEX 1. Location of the project against the local spatial conditions: Fig. 1.1 The projected course of the fairway on the background of local development plans 3
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Fig. 1.2 hydrogeological conditions of land
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
1.2.1. Surveys of the bottom track 1.2.2. hydrogeological conditions Fig. 1.3 Forms of nature protection 1.3.1.1 Special Areas of Conservation and Natura 2000 Sites of Community Importance 1.3.1.2 Special Protection Areas of Natura 2000 1.3.2.1‐3 Forms of nature protection (other than Natura 2000) Fig. 1.4 The results of the inventory of nature with the scope of impact 1.4.1 The area covered by natural inventory. 1.4.2 The range of projected impacts on natural habitats and species of protected plants. 1.4.3 The range of projected impacts of protected animal species. Fig. 1.5 Protective circuits Inpektoratu Regional Marine Fisheries (DIMF) Fig. 1.6 Location trajectory surrounded by historic buildings and areas of archaeological sites. Fig. 1.7 The results of the modeling of pollutant emissions 1.7.1 The results of the modeling of the dispersion of gas and dust in the air during the construction phase 1.7.2 The results of the modeling of the dispersion of gas and dust in the air during the operating phase 1.8 Appendix photo
TABULATED ATTACHMENTS AND TEXT
ANNEX 2 Summary of the parcels covered by the investment and the impact of Annex 3.
The provisions, permits, opinions, administrative decisions Letter WIOŚ 3.1 ‐ current background pollution Scripture West Pomeranian 3.2 Conservator ‐ ws. Archaeological sites in the area of the planned investment 3.3 Scripture City Conservation ‐ ws. The list of sites / buildings listed in the register of monuments in the area of the planned investment 3.4 The letter of the Provincial Office for the Protection of Monuments in Szczecin ws. Provide information on conservation areas and archaeological monuments of moving RDOŚ provision 3.5 ‐ ws. Scope of the report on the environmental impact of the planned project 3.6 Scripture RDOŚ for the availability of the report on the environmental impact for the project. "Reconstruction and expansion of the beach refulacyjnego Chelminek" 3.7 Scripture RDOŚ provide information on bird protection zones West Pomeranian 3.8 Scripture Natural History Society ‐ ws. Ecological corridors 3.9 Scripture Commune Miedzyzdroje ws. Ore development 3.10 Scripture MILEX Sp. Z oo ws. Ore development 3.11 Scripture Seaports Szczecin and Swinoujscie SA ws. Ore development
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
3.12 Letter Group Azoty Z.Ch. "Police" SA ws. Ore development 3.13 Scripture Police Port Authority Sp. Z oo ws. Ore development
ANNEX 4 Detailed data on protected areas 4.1 Analysis of Standard Data Forms for the NATURA 2000 areas 4.2 Existing and proposed forms of nature conservation within a radius of 20 km from the planned investment
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
1. Basis report.
This report, Volume III, is an isolated element of the public contract entrusted by the State Treasury ‐ Director of Maritime Office in Szczecin (hereinafter referred to as the Employer) company EUROPROJEKT GDANSK SA with its registered office at ul. Vistula 55, 80‐680 Gdańsk. It was made as Tom 3. Report of the environmental impact of the project entitled .: "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m.
The recommendations are the basis for the development of the Minister of Infrastructure and Development, the Minister of Environment and the General Director of Environmental Protection for investors / beneficiaries and relevant institutions to verify and ensure compliance of projects financed from EU funds in the 2007‐2013 programming period of the requirements under the Water Framework Directive [75] hereinafter referred to as Guidance.
2. Subject matter and scope of the report.
The subject of Volume III is to assess the impact of the project entitled .: "Modernization of the fairway Swinoujscie Szczecin to a depth of 12.5 m" to achieve the environmental objectives of the Water Framework Directive (WFD) by bodies of water, where the investment concerns. According to the Recommendation [75], the basis for such an assessment should be to analyze the impact of this investment on the individual water quality indicators that make up the biological, hydromorphological and physico‐chemical quality elements of surface waters or on the quantitative and chemical groundwater.
If the result of the analysis determines a negative impact of the investments on indicators of water quality and is found in connection with the danger of failing to achieve the environmental objective for a given body of water in respect of status / potential ecological or chemical status or quantitative status and chemical status, will be effected the possibility of using derogations (derogations from the environmental objectives) Article. 4 paragraph. 7 Water Framework Directive. This assessment will be carried out by verifying the conditions for determining the establishment of such a derogation contained in Article. 4 paragraph. 7 and with reference to Article. 4 paragraph. And Article 8. 4 paragraph. 9 of the Directive.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
3. Description of the projects planned within the Project and investments related to it.
Draft entitled .: "Modernization Swinoujscie‐Szczecin to a depth of 12.5 m" (hereinafter referred to as draft) of the third stage of the modernization Swinoujscie‐Szczecin (Fig. 1). This path ‐ currently holding a minimum depth of 10.5 me a minimum width of 90 meters ‐ runs initially Świna old bed, then two intersecting przekopami island of Usedom ‐ Channel Mielińskim and Piastowski Canal, next ‐ a deep gutter by the lagoon and enter the estuary section of the Oder.
The total length of Swinoujscie‐Szczecin is 67.7 km, counting from the head of the breakwater in Świnoujście in a southerly direction. It consists of a 16.5 km section of land within the islands of Usedom and Wolin, 19.5 km section of track by the lagoon, 8.5 km section of the Glen Odrzańska and the 23.2 km section of the Oder estuary.
Historically, the first shipping lane connecting the city located at the mouth of the Oder to the Baltic ran strait strange. In the thirteenth century, as a result of wars and carried silt Strange, shipping lane was transferred to the foam, which until the beginning of the eighteenth century. Was the only connection between Szczecin and the Baltic Sea. Swina Strait strait was then a very shallow, with many bends shallows. Świna same outlet to the sea divided the shoal of sand, dividing the trough into two branches.
The first attempts to adapt Świny for navigation taken in 1730. [76]. This work lasted until the late nineteenth century. Adverse navigation was very irregular and sinuous course Świna. In order to facilitate the movement of ships built between 1855 and 1880 ÷ current Piastowski Canal, digging the south‐eastern part of the island of Usedom. In the following years it made its extension ‐ Channel Mieliński.
Until World War depth Swinoujscie‐Szczecin for the entire route was 7.0 m. In 1928. Achieved throughout the depth of the waterway to 8.0 m, and 1939. ‐ 9,6 m. During World War II and in the post‐war seaway Swinoujscie‐Szczecin has significantly shallowness. Regular dredging works on the seaway began in 1949., In 1957 to obtain a depth of 9.6 m. Also in the following years, to allow entering the port of Szczecin increasingly larger units, works related not only deepening of the fairway, but its expansion.
Currently, the minimum depth Swinoujscie‐Szczecin is 10.5 m.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Since 2000. Fairway Swinoujscie‐Szczecin is subject to modernization. This upgrade is carried out in stages, as part of separate projects [24]. And yes:
in the years 2000 ÷ 2004 (Phase I) built a new breakwater at the exit Canal Piast Szczecin Lagoon and reconstructed sea defenses Piastowski Canal sections from km 16 + 034 to km 13 + 015 (east side) and from km 16 + 178 to km 12 950 (west side) Swinoujscie-Szczecin, adapting them to the track depth of 12.5 m;
in 2013 ÷ 2015 (Phase II) was reconstructed fortifications Boundary Channel Piastowskie sections from km 13 + 015 to km 9 + 000 (East): and from km 12 + 950 km 9 + 000 (west side) Swinoujscie Szczecin and remodeling and construction of revetments Channel Mielinski sections from 9 km to 000 km + 5 + 400 (east): and from 9 km to 000 km + 5 + 043 (west side) Swinoujscie‐Szczecin. The fortifications were adjusted to track the depth of 12.5 m. Additionally, within the investment eliminated venturi hydraulic km 8 + 050 fairway and converted, or eliminated built quays portion located within the above‐mentioned. channels.
This Motion of stage III modernization Swinoujscie‐Szczecin. Its aim is to obtain a minimum depth of 12.5 meters along the entire length of the track. This project includes the execution of the following measures [58]:
deepening of the fairway section of 5,280 km to 16,500 km (Mieliński channel and channel Piastowski) to a depth of 12.5 m behavior defined in step II modernization waterway width in the bottom;
deepening of the fairway for the section from 16,500 to 67.700 km to a depth of 12.5 m (currently 10.5 m) and increase its width in the bottom of 100 m (currently 90 m) on the straight sections and the curves at 150 m;
modernize three turntables ship: – Police turntable (in the vicinity of the port of Police) measuring axis of 825x350 m, – Isthmus Orla turntable with a diameter of 362 m. – Grabowski turntable channel with a diameter of 220 m;
mijanki embodiment vessels Szczecin Lagoon between the second and third gate Lane, a width of 250 m and a length of 5 km additional segments transition approx. 800 m at both ends, allowing a smooth and safe passage of large vessels (group 1) units of other size categories;
adjacent to the turntable embodiment Police mijanki Police a width of 220 m and a length 1.6 km, allowing large ships to pass each other with small and very small and departing from
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Police turntable link to the path of approach to the Police Port (width in the bottom 100 ml approx. 400 m);
construction of revetments;
Established slope slopes gutter waterway on its various sections are close to the averaged slopes of the currently existing there. The Project adopted the general principle that the slope will not be formed and strengthened everywhere where there is no absolute need to protect the edges and areas of natural land or existing hydraulic structures [25]. In Tab. 1 shows the place in which the slope and depth of the enlarged the fairway or upgraded turntables will interfere with the natural (undeveloped) coastline the Oder River (or the associated channel) between the Police, and the port in Szczecin ‐ so. boundary collisions. On these sections, the retrofitting fairway can be expected subsidence trough banks and silting. – Dig Mieleński ‐ Channel Grabowski, in which the rotating modernized vessels.
Modernized rotating Isthmus Orla interferes with aqueous shunt connecting piercing Mieleński with lake Dąbie called Eagle Isthmus and chamfer forces the northern head of the island Ostrow Grabowski (at the extreme approx. 150 m). Environmental considerations (water exchange between basins, the possibility of runoff of ice) require that the width of the current Isthmus and depth of the Eagle. This means the need for appropriate security Radolin southern tip of the island and the northern promontory of the island and the United Kepa performance in the above. fistula underwater buttresses from the edge of the fairway for a natural depth of the basin ‐ formed with a slope of 1: 3 and strengthened riprap to geotextile. According to [25] spit island Radolin be strengthened by means of anchoring steel sheet piles of oczepami ferroconcrete. The level of the bottom of the cofferdam from the fairway will be ‐ m 6.0 Rel. Cr. Escarpment before cofferdam ‐ a projected slope of 1: 3 ‐ will be strengthened riprap on the geotextile. The cofferdam will pass to the strengthening of boundary type nabrzeżowego. Spit Island United Kepa and receding shore of the island Ostrow Grabowski will be protected slope with a slope of 1: 3, fortified riprap on gewłókninie prism and ending at elevation +1.0 m resp. Cr.
According to [27, 58] the total length of the collision boundary that are not protected by fortifications is 5.585 kilometers. The total length of the edge collision, which will be undergoing umocnieniowe prevent landslides shore and silting fairway is 1.141 km. Summary above. collision boundary, together defining an area of land which they relate, contains tab.1.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Table 1. List of collision edge on the Swinoujscie‐Szczecin and Channel Grabowski indicating the reinforced sections (from [27, 58]).
The length Reference start Reference end definition of of the portion fairway fairway section the mainland / fairway island's name mileage historical mileage historical designed by designed mileage designed mileage mileage Western shore: Great Karwasz 46.675 46.850 46.920 47.095 0.245 long Ostrow 48.980 49.130 49.110 49.240 0.130 54.760 54.975 54.850 55.060 0.090 Crane 55.380 55.590 55.400 55.610 0,020 Island 55.580 55.780 55.670 55.870 0.090 63850 64013 0.164 Ostrow 64.600 64.825 64.850 65.075 0,250 Grabowski 65.150 65.375 65.335 65.560 0.185 65.635 65.860 65.840 66.065 0.205 66.025 66.240 66.065 66.280 0,040 Mieleński Islet 66.425 66.650 66.930 67.150 0.505 66.975 67,200 67,000 67.225 0,025 67.125 67.350 67.300 67.525 0,175 sum: 2,124 including strengthened: 0.164 eastern shore: Raduń 47.610 47.775 47.750 47.925 0.140 Island Raduń 49,500 49.675 49.525 49,700 0,025 55.115 55.325 55.450 55.650 0.335 55.490 55.700 55.530 55.740 0,040 56.400 56.610 56.690 56.890 0.290 56.730 56.950 56.790 56.990 0,060
57.210 57.425 57.290 57.490 0,080 Oakwood 57.790 58,000 57.950 58.170 0,160 58.050 58.260 58.070 58.280 0,020 58.710 58.930 58.940 59.150 0,230 59.350 59.560 59.730 59.950 0.380 60.120 60.325 60.150 60.355 0.030 60.550 60.760 60.570 60.780 0,020 62.050 62.275 62.110 62.335 0,060 Radolin 62.870 63.075 63.330 63.535 0.460
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
The length Reference start Reference end definition of of the portion fairway fairway section the mainland / fairway island's name mileage historical mileage historical designed by designed mileage designed mileage mileage 63.450 63.675 63.970 64.190 0,520 64.010 64.225 64.280 64.490 0,270 United Kepa 64.425 64.630 64.510 64.715 0.085 64.600 64.825 64.620 64.845 0,020 64.910 64.125 65.175 65.380 0.265 65.750 65.960 65.770 65.980 0,020 property 66.185 66.410 66.210 66.435 0,025 67.180 67.400 67.280 67,500 0,100 sum: 3,632 including strengthened: 0.977 unreinforced boundary collisions (including western and eastern 4,615 channel Grabowski definition of Reference start of the Reference end of length the mainland / channel section the channel section island's name designed by mileage designed mileage designed mileage Ostrow 0.368 Grabowski sum: 0.368 including strengthened: 0.368 sea defenses (total): 1,141
reconstruction of existing embankments (HUK strengthening wharf, quay Nautical, navigational aids Base quay, the quay Gnieźnieńskie);
The Project is assumed that the intersection of the plane of the slope of the gutter waterway plane of acceptable depth at the building site HDOP hydro at a distance from the edge less than approx. 1.5 times HDOP poses a threat to the structure. This situation applies covers three piers on the west bank of the Oder, ie. HUK waterfront, waterfront wharf Sailing and Navigation Databases Labeling (OPD) and Gniezno waterfront on the island of Ostrow Grabowski. In [25] presented three variants of securing these wharves.
In one of the variants in the case of piers HUK, nautical, BON work includes: forming the slope of the track with a slope of 1: 3 and strengthening the riprap to geotextile, to strengthen the foot of the slope by filling the bottom of the track ‐ in a strip width of approx. 10 m ‐ rubble to a depth of 14.0 m scoring sheet pile within 2Hdop and before execution of said wall corresponding overhead of rubble or the support structure of the mattress gabion possible execution filling soil between the bank and the wall sealed to the level HDOP, deletion or truncation of the wall tight.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
In the case of quay Gnieźnieńskie, due to the proximity of the turntable the ship and which can perform there intensive water movement, caused by a push / pull of the masses of water through the hull of the rotating vessel and strong currents screwed (tug, ship) are designed forming the slope of the track with a slope of 1: 3 to reinforce its riprap on the geotextile. Strengthening will be ended horizontal flange width. 2 m, a depth limit on the crown at the quayside, ie. On the ordinate m 7.0 Rel. Cr. Grading rate will be enhanced by filling the bottom of the track ‐ in a strip width of approx. 10 m ‐ rubble to a depth of 14.0 m [25].
construction of new or expansion of existing fields refulacyjnych;
When intended to deepen and widen the fairway is extracted approx. 23 212 thousand. m3 dredged materials [58]. While it will be uncontaminated dredged materials, its storage will take place in the designated fields and suitably prepared spoil (refulacyjnych). The Project [28, 39] is considering the construction of: – a large, polygonal boxes adjacent islands Chelminek (old field silting Maritime Office), located in central‐western area of flooding on the east side of the fairway. – a large island, located in central‐western area of flooding on the east side of the fairway. – three islands located in the central zone of the Lagoon ‐ two islands on the eastern side of the fairway and one on the west.
adapting an existing navigational aids to the new geometry fairway meaning moving dolphins 30 defining the eastern edge of the fairway km from 55.950 to 67.525 km path. Because the axis of the fairway will remain essentially unchanged, it is not expected to change the location of the other characters fixed.
Projects related to the project ‐ although planned as a separate investment (hereinafter referred to as accompanying investments) [77, 84] ‐ are:
Deepening Swinoujscie-Szczecin on the section from km 0.000 to km 3.100 to a depth of 14.5 meters (currently 14.3 m), which will be executed within the statutory activities of the Maritime Office in Szczecin;
Development of port infrastructure in the northern part of the peninsula in the Port of Szczecin Ewa (hereinafter referred to as an investment Peninsula Eve), including: – reconstruction of the existing 220‐meter quay Grain it with an extension of 35 m. – Cab Eve peninsula from the north German wharf of 163 m – Ewa development of the peninsula on the east side of 30‐meter section of the wharf into contact with the existing quay Slovakian,
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
– deepening of the basin adjacent to the quays to 10.5 m;
The project was completed in mid‐2015. As a result, it was transformed into a fortified irregular edge of the northern tip of the peninsula in a series of wharves with a total length of 228 m. Reconstruction of the existing quay Cereal was not associated with a shift line on the waterfront toward the water (western arm of the Oder).
Improving access to the port of Szczecin in the Kashubian region Basin (hereinafter investment Swimming Kaszubski) Comprising: – reconstruction of existing embankments: Katowice, Katowice‐stepped, Chorzowskie, Chorzowskie‐Fault a total length of 840.84 m (the length of the mooring line 734.87 m) and a length of 342.8 Bytomskie m in order to increase their load capacity and technical depth (10.5 m to 12.5 m). – deepening the bottom of the pool areas Kaszubskiego to 100 m from the above‐mentioned. berths to 12.5 m, – deepening of the turntable to 12.5 m (260 m in diameter) for vessels located at the entrance to the pool Kaszubskiego. – improvement of hydro technical infrastructure on the peninsula Katowice; Reconstruction of the above. quays will be associated with a shift of the maximum of about 1.5 m to the water. The volume of excavated material obtained from deepening Basin Kashubian will total approx. 395.46 thousand. m3, of which approx. 169 thousand m3 will be used for zalądowienia Pool Noteckiego. Noteć pool will be closed from the water‐tight wall built with a length of 100 m and a depth of 10.5 m technical. The resulting from the zalądowienia Noteckiego Basin will be built square maneuvering and parking. The remaining part of excavated material will be postponed to existing or newly created field silting of the Maritime Office in Szczecin or Seaports Szczecin and Swinoujscie SA (hereinafter referred as the Ports Authority). It is anticipated that any new field silting Ports Authority could arise in the island of Ostrow Grabowski or Mieleński Ostrow.
Improving access to the port of Szczecin with the expansion of port infrastructure in the area of Canal Dębicki (hereinafter referred to as an investment channel Dębicki), including: – reconstruction of the existing wharves Slovak and Czech, with a total length of 1017 m in order to increase their carrying capacity and technical depth (from 10.5 m to 12.5 m) – Temporary construction quay cooperative with a length of 80 m, equipped with a ro‐ro ramp having a length of 27m and a depth of technical 10.5 m – Cooperative reconstruction of quay length including 117.35 to enhance its technical depth to 12.5 meters, – Channel Dębicki widening to a width of 200 m over a length of approx. 900 m, the construction in this section Norwegian quay length of 300 m, and the revetment (Length of approx. 600 m) extending to the proposed strengthening the northern head 13
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
of the island Ostrow Grabowski the turntable Orla isthmus.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
– Channel deepening Dębicki (the width of 200 m and a length of 1200 m) to 12.5 m and strengthen the bottom of the channel at a distance of 50 meters from the quays;
The investment has already been made Transitional Cooperative waterfront along the ro‐ro ramp. As a result of the investment will be the conversion of the existing natural shore Channel Dębicki and islands Ostrow Grabowski length approx. 1100 m. Coastline is revoked approx. 80 m and a length of 300 m built wharf and the section approx. 800 m (ie. To the intended strengthening of the headland of the island at Ostrow Grabowski turntable Orli Isthmus) strengthened. The reconstruction of the above. quays will be associated with a shift of the maximum of about 1.5 m to the water. Widening and deepening the Canal Dębicki extraction means approx. 1 million m3 of excavated material. It will be pushed to existing or newly created field silting of the Maritime Office in Szczecin or the Ports Authority. The bottom of the Channel Dębicki be strengthened on the surface of approx. 120 thousand. m2.
Construction of the quay for handling bulk cargo (waterfront Scandinavian) on the Ostrow Grabowski Przekop Mielenski (hereinafter referred to as an investment Ostrow Grabowski) - as part of this new investment will quay length of 300 m and a depth of 12.5 m technical;
Adapting Infrastructure ferry terminal in Swinoujscie for handling intermodal transport (hereinafter referred to as an investment Ferry Terminal, including m.in .: – reconstruction position ferry 6, consisting in leveling of the line of the quay line position ferry 5, – the construction of the ferry No. 1 position with a length of 242.15 m and a depth of 12.0 m technical;
As a result of this investment will be buildings of the existing natural Świna shore quay with a length of 242.15. There will also shift the built‐up edge of the basin approx. 25 m toward the water for a distance of 130 m (position 6).
Construction of deep-water quays in the port of Swinoujscie (hereinafter referred to as an investment Quay deep), including m.in .: – adaptation of existing berths: dockers (pier and parking), Miners, Miners Transitional, Metallurgists and Chemists, with a total length of 1,267.40 meters to a depth of technical 14.5 m – zalądowienie Pool Trymerskiego and elongation quay Hutników 85 m – Miners‐quay reconstruction of shoulders a length of 156.10 m in order to increase its bearing capacity and technical depth (from 5 m to 14.5 m).
At the moment the concept Location and Software for investment has not yet been developed. It is not excluded that it will be necessary to strengthen the bottom Świna within to 50 m from the upgraded quays, ie. a total length approx. 1,508.5 m. In the case of 15
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
conclusion of the relevant agreements (or purchase the property) will be possible to extend the project for the construction of the quay Armatorski length of 185.0 m
Modernization Seaport Police (hereinafter referred to as an investment Seaport Police), including m.in .: – construction waterfront transshipment length of 220 m and a depth of 12.5 m of technical, – the construction of the quay dalbowego handling of liquid bulk cargo ships with a draft of 10.5 m and a length of 230 m, – corresponding deepening of the basin adjacent to the quays.
Extra investment, which will have to be taken by the Ports Authority to deepen the turntable Przekop Mielenski at the confluence of the River Parnica with a diameter of 300 m to 12.5 m (10.5 m currently). This turntable in accordance with the Regulation of the Minister of Infrastructure and Development of 7 May 2015 on the definition of port areas and public facilities, equipment and installations in the port infrastructure for each port of fundamental importance for the national economy1 now part of the infrastructure of the Port of Szczecin.
Project location projects and investments are shown in the accompanying Figure 1, while basic ‐ necessary for the implementation of the report ‐ data of these projects are summarized in Table 2.
1 OJ of 2015. pos. 732. 16
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Lynx. 1 Location of projects and investments associated with the project (development own).
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Table 2. Basic parameters of the project and investment projects implemented within the accompanying Świna the mouth, the Szczecin and Odra estuary.
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] dredging work The project ‐ seaway Swinoujscie ‐ deepening to 12.5 m at the current width of the 5,100 17,000 11,900 1.48 1,075.75 bottom 17,000 23,000 deepening of 12.5 me to widen at the bottom to 100 m 6,000 0.6 2,270.06 deepening of 12.5 me to widen in the bottom (the 23,000 23,800 0.800 0.14 transition section having a width of 100 m to 250 m) Execution passing place between the second and 23,800 28,800 5,000 1.25 6132.8 third gate machines (depth 12.5 m, the bottom deepening of 12.5 me to widen in the bottom (the 28,800 29,600 0.800 0.14 transition section having a width of 250 m to 100 m) 6,889.41 12.5 deepening and widening in the bottom of 100 29,600 49,400 19,800 2.16 m (at curves and bends to 150 m)
Police embodiment turntable (depth 12.5 m, 49,400 50200 0.800 0.29 333.47 the length of the axis 825 and 350 m)
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] mijanki implementation of the Port of Police (depth 50200 51,800 12.5 m, the bottom width of 220 m) with portions of 1,600 0.34 560.85 the transition varies on width) 12.5 deepening and widening in the bottom of 100 51,800 62900 11,100 1.32 3,076.96 m (cornering to 130 ÷ 150 m) execution of the turntable Orla isthmus (depth 12.5 62900 64,000 1,100 0.23 804.17 m, 362 m diameter) deepening to 12.5 m in the bottom widening to 100 m 64,000 67100 3,100 0.34 1,172.97 in the time of transition sections together: 62,000 8.29 22316.40 The project ‐ other fairways and channels deepening to 12.5 m approach fairway to the Port 0.400 0.02 20.32 Police deepening to 12.5 m Channel Grabowski 0.07 655.41 Channel execution turntable Grabowski 0.04 75.96 Grabowski Canal deepening the waterfront 0.05 143.93 Harvesters together: 0.400 0.180 895.62 accompanying investments deepening Swinoujscie‐to Szczecin 0.000 3,100 3,100 0.47 93.10 14.5 m deepening to 12.5 m Basin Kashubian 395.46 deepening to 12.5 m turntable at the entrance to 0.05 141.40 the Basin Kashubian 21
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] Dębicki Channel deepening to 12.5 m 1,200 0.240 1000.00 deepening the turntable Przekop Mielenski at the 0.07 141.37 confluence of the River Parnica together: 4,300 0.834 1,771.33 together: 66700 9304 24983.35 embodiment shore defenses Design 62880 63340 strengthening of the southern tip of the island Radolin 0.460 63450 63967 strengthening the northern headland of the island of 0517 strengthening the northern headland of the 0532 island of Ostrow Grabowski together: 1,509 accompanying investments Port Szczecin channel Dębicki 0.600
together: 0.600 together: 2.109 Execution bottom fortification Design strengthening the bottom at the southern tip of 62880 63340 0.460 0.014 the island Radolin 22
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] strengthening the bottom Eagle isthmus section 63340 63450 of the edge of the fairway for a natural depth of 0.110 0.006 the fistula strengthening the bottom tip of the island at the 63450 63967 0517 0.028 northern United Kepa strengthening of the floor at the northern tip of the 0.028 island Ostrow Grabowski 59390 59450 strengthening the bottom of the waterfront HUK 0.050 0.001 60060 60260 strengthening the bottom of the waterfront Sailing 0.119 0.006 60960 61,600 strengthening the bottom of the waterfront BON 0.091 0.003 strengthening the bottom of the waterfront Gniezno 0.200 0.006 together: 1,547 0.092 accompanying investments Port Szczecin Peninsula Eve Swimming Kaszubski channel Dębicki 2,400 0.12 Ostrow Grabowski Port Świnoujscie Ferry terminal deep waterfront 1,694 0.084675 together: 4094 0.205 together: 5.641 0.494 23
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of excavated investment fairway [Km] [km2] [tys.m3] landfill construction dredging spoils (alternatively) Design in the form of one island 29,000 W29 having a diameter of 2200 m 3,800 31000.00 in the form of three islands 22,000 W22 having a diameter of 1,250 m 1.230 11200.00 27,000 W27 having a diameter of 1,250 m 1.230 10100.00 28,000 W28 having a diameter of 1,250 m 1.230 10100.00 together: 3.690 31400.00 larger existing field refulacyjnego Chelminek 4.25 31400.00 deposition of dredging spoil in the gutter waterway local leveling trims Channel Mielińskim and no 5,100 17,000 no data Piast level ‐12.5 m data change in the course of the coast line (potential slipping of the edge, to shift the quays zalądowienia magnification basin) Design seaway Swinoujscie‐Szczecin ‐ including 5.585 boundary collisions nieumacniane Channel Grabowski ‐ boundary collisions 3.625 Ostrow Grabowski ‐ beheading the northern headland 0.056 together: 9.21 0.056
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] accompanying investments Port Szczecin Peninsula Eve 0.228 0.005 Swimming Kaszubski ‐ waterfront 1,078 0.0016 Swimming Kaszubski ‐ zalądowienie Basin Noteckiego 0.100 0.021 channel Dębicki ‐ waterfront 1.134 0.002 channel Dębicki ‐ widening of the Canal Dębicki 0.900 0.072 Ostrow Grabowski Port of Swinoujscie Ferry terminal 0.130 0.003 deep waterfront 0.080 0012 together: 3.650 0.117 together: 12860 0.173 reconstruction of the existing wharves accompanying investments Port Szczecin Peninsula Eve 0.220 Swimming Kaszubski 1.184 channel Dębicki 1.134 Ostrow Grabowski 0.000
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
location parameter Project project s mileage and accompanying length surface volume of investment fairway [Km] [km2] [tys.m3] Port Świnoujscie Ferry terminal 0.130 deep waterfront 1,509 together: 4.176 construction of quays accompanying investments Port Szczecin Peninsula Eve 0.228 Swimming Kaszubski 0.000 channel Dębicki 0.407 Ostrow Grabowski 0.300 Port Świnoujscie Ferry terminal 0.242 deep waterfront 0.270 Harbor Police Seaport Police 0.220 together: 1177
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources in accordance with the requirements of the Water Framework Directive
4. Analysis and evaluation of the impact of the Project for the purposes of water conservation.
4.1. Stage I.
4.1.1. Identification of water bodies and their associated environmental objectives.
.: The project entitled "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" refers to the following of surface water bodies (JCWP) [33]:
heavily modified surface water body (JCWP) in the category transitional waters: PLTWVWB7 Estuary Świna, Referred to as JCWP Mouth Świny (Fig. 2). heavily modified surface water body in the category transitional waters: PLTWIWB8 Szczecin Lagoon, Referred to as JCWP Szczecin Lagoon (Fig. 3). heavily modified surface water body in river category: PLRW6000211999 Measles from Párnica to the mouth, Hereinafter referred to as the Oder
JCWP from Párnica to the mouth (Fig. 4), and the following bodies of
groundwater (groundwater bodies):
JCWPd by dividing the current planning cycle in 2009 ÷ 2015 [33] - PLGW67001, PLGW67002, PLGW69007, PLGW690025 or JCWPd by a new division, which will be valid in the planning cycle 2015 ÷ 2021 ‐ PLGW60001 (hereinafter JCWPd 1) PLGW60007 (hereinafter JCWPd 7) PLGW60004 (hereinafter JCWPd NO: 4) (Fig. 5)
located within the catchment area of the Oder, in the aqueous lower Oder and the Coastal West [85].
According to the adopted in Poland typology above water. Single parts of the surface water are assigned [33] the following types:
JCWP Mouth Świna ‐ the type of estuary of sandy substrate (TWV) JCWP Szczecin Lagoon ‐ the type of lagoon with sandy substrate and mułowym (TWI) JCWP Measles from Párnica to the mouth ‐ the type of large lowland river (21).
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources in accordance with the requirements of the Water Framework Directive
Fig. 2. Mouth JCWP Świny (source: based on: [21, 32, 78]). 28
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Lynx. 3.JCWP Szczecin Lagoon (Source: based on: [21, 32, 78]). 29
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Measles JCWP from Párnica to the th
Fig. 4. Measles JCWP from Párnica to the mouth (Source: own study based on: [21, 32, 78]).
th
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources in accordance with the requirements of the Water Framework Directive
PLGW67001 PLGW60001
PLGW67002
PLGW60004
PLGW69025 PLGW69007 PLGW60007
Lynx. 5.Jednolite groundwater bodies groundwater bodies located in the area where the project will be implemented; left ‐ according to the old division of groundwater bodies [33] on the right ‐ according to the new division (source: based on: [21, 32, 78]). 31
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
As approved by the Council of Ministers and published in 2011. Plan of water management in the basin of the Oder [33] in relation to the JCWP Estuary Świna JCWP and Szczecin Lagoon introduced, pursuant to art. 4 (4) ‐3 WFD, the derogation from the requirement to achieve good ecological potential and good chemical status by 2015. It was argued that, due to natural conditions six years is too short a period to be able to improve the state, even the complete elimination of pressure. These are bodies of water contaminants from the receiver because a large area of land and their state is directly dependent on both the status of inland waters, as well as the limitation of the pressure in the interior.
Derogation from the requirement to achieve good ecological potential and good chemical status by 2015 have also been introduced with regard to the JCWP JCWP Odra from Párnica to the mouth. In [33], the following reasoning: "Because of the planned activities of the investment resulting in changes in physical characteristics JCW, for higher social aims, ie. Flood protection, it is impossible to achieve by JCW environmental goals."
According to the provisions of the Plan of water management in the basin of the Oder [33] environmental objective for groundwater bodies PLGW67002 is to maintain good quantitative and chemical status.
Within the limits of the above. water bodies are protected areas within the meaning of the Water Framework Directive, mentioned in the Schedule of bodies of surface water intended for recreational purposes, including bathing (referred to in Art. 113 paragraph. 4 point 2 of the Act of 18 July 2001. ‐ Water Law2), In Schedule of bodies of water intended for the abstraction of water for public supply of water intended for human consumption for drinking (referred to in Art. 113 paragraph. 4 point 1 above. Act) and in the Schedule of areas intended for the protection of habitats or species laid down in the nature Conservation Act, for which the maintenance or improvement of water is an important factor in their protection (referred to in art. 113 paragraph. 4 point 6 above. Act).
The currently applicable Plan of water management in the basin of the Oder [33] environmental objectives for protected areas have not been increased. The rationale is often higher requirements with respect to the limit values of indicators of water quality for a good state / ecological potential than served in the acts governing law requirements for water status within these areas, in the case of Natura 2000 areas ‐ the lack of protection plans or plans of protection tasks.
Under Article. 38f Water Act for the purpose of environmentally protected areas is to achieve the standards and objectives of the specific provisions under which those areas have been created, as long as they do not contain in this respect different provisions.
2 consolidated text ‐ Journal. U. 2015 item. 469.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
In 2013. On request of the National Water Management was realized for the update management plans for the river basin in Poland work entitled .: Determining the environmental objectives for surface water bodies (JCWP), underground (groundwater bodies) and protected areas [62]. As part of this work was developed methodology for determining the manner of determining the environmental objectives for water bodies, taking into account ‐ in the case of the existence within their borders protected areas ‐ a condition To use the most rigorous or indicate additional targets. Based on this methodology, using the results of evaluation of the JCWP for the years 2010 ÷ 2012 made by the Chief Inspectorate of Environmental Protection and the results of the assessment of groundwater bodies made by the Polish Geological Institute ‐ National Research Institute, have been set back environmental objectives for all water bodies and summarized them in a standardized cards water bodies (JCW). These cards were used in the renovation plans for the ongoing management of the river basin and made available to the public consultation, together with draft these documents.
Derived from [81] for the JCW card: surface water body PLTWIWB7 Mouth Świna surface water body PLTWIWB8 Szczecin Lagoon, surface water body PLRW6000211999 Odra from Párnica to the mouth, bodies of groundwater PLGW60001, PLGW60004, PLGW60007, They are, respectively, Annex 1 ÷ 6 hereto. In accordance with the
above. cards JCW environmental objectives are:
in the case of surface water body PLTWIWB7 Estuary Świna: achieve good ecological potential, achieve good chemical status
in the case of surface water body PLTWIWB8 Szczecin Lagoon: achieve good ecological status, achieve good chemical status maintain or restore a favorable conservation status listed in the card depending on the subject matter in waters designated protected areas;
in the case of surface water body PLRW6000211999 from Párnica to Measles the mouth: achieve good ecological potential and the possibility of migration of aquatic organisms achieve good chemical status maintain or restore a favorable conservation status listed in the card depending on the subject matter in waters designated protected areas;
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
in the case of a body of groundwater PLGW60001: the achievement of good quantitative status, achieve good chemical status the quality of underground water, which is charged to the needs of public water supply intended for human consumption should not deteriorate.
in the case of groundwater bodies PLGW60004 and PLGW60007: maintaining a good quantitative status, maintaining good chemical status the quality of underground water, which is charged to the needs of public water supply intended for human consumption should not deteriorate.
The card JCWP Mouth Świna indicated no areas for the protection of habitats or species for which the maintenance or improvement of water is an important factor in their protection.
The Szczecin Lagoon JCWP tab lists the following protected areas designed to protect habitats or species for which the maintenance or improvement is an important factor in their protection:
1. Natura 2000 ‐ a special bird protection area (SPA) Delta Świny (PLB320002) 2. Natura 2000 ‐ a special bird protection area (SPA) Łąkie Skoszewskie (PLB320007) 3. Natura 2000 ‐ a special bird protection area (SPA)) Szczecin Lagoon (PLB320009) 4. Natura 2000 ‐ a special bird protection area (SPA) Forest Goleniowska (PLB320012) 5. Natura 2000 ‐ a special bird protection area (SPA) refuge Wkrzańska (PLB320014) 6. Natura 2000 ‐ A special area of conservation (SAC) Estuary Oder and Szczecin Lagoon (PLH320018) 7. Natura 2000 ‐ A special area of conservation (SAC) Wolin and Usedom (PLH320019) 8. Natura 2000 ‐ A special area of conservation (SAC) Uroczyska Forests Stepnickich (PLH320033) 9. Reserve Białodrzew Kopicki (REZ360) 10. Reserve Karsiborskie Ferns (REZ361) 11. Olszanka Reserve (REZ363) 12. Wolin National Park (WoPN).
Ww. and other protected areas located in the region of Szczecin Lagoon JCWP shown in Fig. 6a, 6d ÷.
The card JCWP Odra from Párnica to the mouth of the following protected areas are listed for protection of habitats or species where the maintenance or improvement is an important factor in their protection:
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
1. Szczecin Landscape Park "Beech Forest" (PK91) 2. Natura 2000 ‐ a special bird protection area (SPA) Lower Oder Valley (PLB320003) 3. Natura 2000 ‐ a special bird protection area (SPA) Szczecin Lagoon (PLB320009) 4. Natura 2000 ‐ a special bird protection area (SPA) Forest Goleniowska (PLB320012) 5. Natura 2000 ‐ A special area of conservation (SAC) Estuary Oder and Szczecin Lagoon (PLH320018) 6. Natura 2000 ‐ A special area of conservation (SAC) Beech Hill (PLH320020) 7. Natura 2000 ‐ A special area of conservation (SAC) Dolna Odra (PLH320037) 8. Beech reserve Zdroje them. Professor Tadeusz Dominik (REZ327).
Ww. and other protected areas located in the area JCWP Odra from Párnica to the mouth shown in Fig. 7a ÷ 7d.
According to the developed in the [62] the method for setting the environmental objectives for water bodies environmental objectives protected area identified on the JCW apply only to those sections of the body of water in which these areas are located, and not the entire body of water. These objectives may, however, have implications well beyond the protected area to which they apply, but only to the extent that is necessary for their achievements in this area.
It should be emphasized that contained in the above. JCW card information, in particular on exemptions from the environmental objectives, subject to certain adjustments yet. The process of public consultation draft renovation plans for management of river basin ended on 22 June. The final versions of these documents, valid for the years 2015 ÷ 2021 are to be ready by the end of the year [81].
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Lynx. 6a.Specjalne areas of conservation (SACs) in the area JCWP Lagoon Fig. 6b. Special Protection Areas (SPAs) in the area JCWP Lagoon Szczecin (Source: [83]). Szczecin (Source: [83]). 36
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Lynx. 6c.Rezerwaty in the area JCWP Szczecin Lagoon (Source: [83]). Fig. 6d. Wolin National Park in the area JCWP Szczecin Lagoon 37
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
(Source: [83]).
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Lynx. 7a.Specjalne areas of conservation (SACs) in the area JCWP from Párnica to the mouth (Source: [83]). measles 39
Fig. 7b. Special Protection Areas (SPAs) in the area of the OdrThe impact assessmenta JCWP of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources Párnica to the mouth (Source: [83]).
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The impact asssessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Beech PSUs them. prof. Tadeusz Dominik
Lynx. 7c.Rezerwaty in the area JCWP Measles from Párnica to the mouth (source: [83].) Fig. 7d. State Parks in the area JCWP Measles from Párnica to the mouth 41
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
(Source: [83]).
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.2. Characteristics JCW.
4.1.2.1. JCWP Świna Estuary.
Heavily modified water bodies in the category of surface waters Estuary Świna a narrow strip of the Pomeranian Bay waters adjacent to the island of Usedom from the state border to the central breakwater (formerly the East) in Swinoujscie, a width of 1 nautical mile and the average length of approx. 4.8 km (Fig. 2). The total area of 8.93 km2 is JCWP.
Within Pomeranian Bay transformation takes place, and river water take place by intense impurity distribution of the basin worn Oder. The yield northern Gulf, separating it from the waters of the Bornholm Basin is a line drawn from Cape Arkona (Rügen) to the lighthouse Gaski, located approx. 20 km east of Kolobrzeg. Pomeranian Bay area is approx. 6 thousand. km2 and the average depth of slightly more than 13 m. In the middle of the bay there is a shallow water (Shoal of Odrzańska), where the depth of the sea does not exceed 8 m. The bottom contours defining the depth of ten meters ‐ except for the region of the mouth of the odd extends approximately parallel to the coastline, at a distance of 1 ÷ 2 mm. It is assumed that the average salinity of the bay is 7.5‐ 8.0 ‰ [36]. Ocean currents in the Pomeranian Bay are dependent on long‐lasting winds and mostly are directed to the east. Their speed along the coast reaches 2 knots (approx. 1 m / s) within 3.5 mm from the edge [19].
Under JCWP Świna Estuary is regularly dredged fairway floating units providing access to the ports of Swinoujscie and Szczecin.
4.1.2.2. JCWP Szczecin Lagoon.
Characteristics of hydrographic. The heavily modified body of transitional waters (JCWP) PLTWIWB8 Szczecin Lagoon includes, among others water (Fig. 3): Grand Lagoon, part of the Gulf Nowowarpieńskie Polish, Glen Oder, lakes Wicko Big, Small Wicko Lake and water strait Świna, including Old Swina, Piastowski Canal and Canal Mieliński.
The total area JCWP Szczecin Lagoon is approx. 407.28 km2, the length of the coastline of this part of the water is approx. 321.76 kilometers.
Szczecin Lagoon is a large reservoir with an area of przymorskim approx. 687 km2, average depth of 3.8 mi average volume of approx. 2.58 km3. Through the middle of the Lagoon, at the border of the natural hydrogeological, the state boundary dividing the area into Polish ‐ Grand Lagoon and part of the German ‐ Little Lagoon.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Szczecin Lagoon is powered mainly waters from the catchment area of the Oder. The share of the waters of the Oder approx. 97% of the total inflow of water into the lagoon. Other major tributaries are: Gowienica, Foam, Swiniec, Wkra Wołczenica and Zarow.
Szczecin Lagoon is separated from the Pomeranian Bay and the islands of Usedom and Wolin connected with the sea by three narrow and elongated straits: Foam (Peenestrom) to the west (Germany), Świna between the islands of Usedom and Wolin, and strange in the east. Through these straits is held bi‐directional exchange of waters between the Lagoon and the sea. The movement of water in the straits has the characteristics of different pulsation frequencies [76]. The estuary section Foam flow direction changes are frequent and evenly distributed throughout the year. The strait Świna in the autumn‐winter season flows are characterized by a high frequency of changes, and in the spring‐summer season there are long periods of continuous outflow of water from the lagoon to the sea, occasionally interrupted inflows. The strait strange, throughout the year there is a clear advantage outflow of water towards the sea.
Currently, the main connecting Szczecin Lagoon from the Baltic Sea is Świna strait, which runs the fairway Swinoujscie‐Szczecin. Previously, a more important role in the exchange of water between the Lagoon and the Baltic Sea Foam meets the strait, which led main shipping route for ships bound for the port of Szczecin. Świna estuary was shallow and the sand content constantly. The situation changed only after the construction of the Piast Canal.
Currently it is estimated from pigs flows total approx. 78% of the water from the lagoon (including 47% Canal Piastowskim and 31% Old swine) foam, ‐ approx. 14% and the least strange ‐ approx. 8% [76].
Characteristics of hydrological and meteorological. Water levels and flows in the JCWP Szczecin Lagoon are formed on one side by the size and nature of the Lagoon tributaries of the river, mainly from the catchment area of the Oder, on the other ‐ by sea level changes in the Pomeranian Bay and the effect of wind on the water bodies.
Simultaneous overlapping influences odmorskich and runoff from the catchment area of the Oder makes the area JCWP Szczecin Lagoon can not talk about the interdependence between states and the water flows. Hydrological characteristics of the body of water so it can be based only on the water levels.
Wodowskazowymi representative cross sections for ‐ located within the area JCWP Szczecin Lagoon ‐ Swinoujscie‐Szczecin stations are water gauge Swinoujscie (ravine Świny) and Trzebiez (Szczecin Lagoon) belonging to the network to monitor the Institute of Meteorology and Water from the Gdynia.
Water gauge in Swinoujscie It was founded in 1810. Location patches and leveling zero gage changed several times. June 20, 1961 on. Zero river gauge placed on the ordinate ‐5.000 m Rel. NN. September 21, 1966 r. Water gauge finally moved to the waterfront 41
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Harbor master (2.3 km Swinoujscie‐Szczecin). After zaniwelowaniu to sea level in Kronshtadt ordinate zero gage is ‐5.080 m resp. Cr.
Characteristics and the maximum annual water levels with a certain probability clearance gage station Swinoujscie, determined on the basis of the data contained in [4] and [69] listed in Table. 3 and tab. 4.
Table 3. Characteristic water levels for the year 2000 (the multi‐year set 1949 ÷ 2000 taking into account the trend for the middle class) station gauges Swinoujscie [4].
Characteristic water levels H [cm] absolute maximum 696 (10.02.1874) maximum Websi 669 (11.04.1995) medium high CSG 596 averag SSW 503 medium low SNW 420 minimum accide 366 (18.10.1967) absolute minimum 366 (18.10.1967)
Table 4. The maximum annual water levels of a certain probability of exceedance in Swinoujscie designated for multi‐year in 1901 ÷ 2006 [69].
Annual maximum water levels [cm] of the probability of exceedance 0.1 0.5 1 2 5 10 50 712.9 683.9 671.3 658.5 641.1 627.4 590.1 * Mean values of the two distributions: Gumbel and Pearson III
Water gauge in Trzebież It is located in the northern part of the basin of the fishing port of Trzebież (36.45 km Swinoujscie‐Szczecin). Water gauge was founded in 1881. On the ordinate or ‐5.000 m. NN. Observations were resumed in 1947. On the ordinate ‐5.040 m NN. In 1953. It changed the position of zero at ‐5.000 m resp. NN. After zaniwelowaniu to sea level in Kronshtadt ordinate gage is zero or ‐5.080 m. Cr.
Characteristics and the maximum annual water levels with a certain probability clearance gage station thinning, determined on the basis of the data contained in [4] and [69] listed in Table. 5 and Tab. 6.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Table 5. Specific conditions for water gauges Trzebiez station for the year 2000 with a multi‐year set 1949 ÷ 2000 taking into account the trend for maximum and medium‐sized states [4].
Characteristic water levels H [cm] absolute maximum * 637 (12.31.1913) maximum Websi 614 (607 11/30/1978) medium high CSG 583 averag SSW 510 medium low SNW 456 minimum accide 429 (02.25.1954) absolute minimum 428 (21.03.1928) * Excluding trend
Table 6. The maximum annual water levels of a specific exceedance probability in the multi‐year Trzebież set for 1948 ÷ 2007 [69].
Annual maximum water levels [cm] of the probability of exceedance 0.1 0.5 1 2 5 10 50 650.9 633.5 625.8 618.0 607.3 598.7 574.5 * Mean values of the two distributions: Gumbel and Pearson III
One of the basic factors determining the hydrodynamics JCWP Szczecin Lagoon is the wind. Variable complex topography and hydrography above. body of water, the presence of two large bodies of water, ie. the Szczecin and the Baltic Sea, for free movement of air masses makes the wind conditions within JCWP are varied. A significant variability in the occurrence of winds the study area is also observed in different seasons. In the spring and summer it is often winds from the northern sector (NE, NW and N), and in the autumn and winter are a step ahead wind direction southern especially SW and S. seasonality occurrence of winds associated with modulation of the Baltic Sea and particularly the variation in temperature between the land and sea. Therefore, in the spring and summer circulation is dominated by a supercharged,
The characteristics of the wind conditions within JCWP Szczecin Lagoon determined on the basis of two meteorological stations, ie. Swinoujscie thinning and reported in [35].
Statistical analysis of wind conditions occurring in Świnoujście multi‐year period 1970 ÷ 1995 indicated that [35]:
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
in the medium most frequent wind direction W (20.62%), SW (19.26%) and S (16.27%) and the least with the direction N (7.39%) and NW (7.42% ) Total silence accounted for 2.90% of all observations, which gives almost 11 days a year with no wind, strong winds exceeding 5O Beaufort (speeds above 10 m / s) blew average of 13 days in the year, representing 3.57% of the total observation the annual average wind speed Swinoujscie was 3.92 m / s, characterized by the highest average speed winds from the northern sector N (5.6 m / s), NE (5.4 m / s) NW (5.1 m / s); the weakest direction winds occur southern S (3.0 m / s) SE (3.3 m / s) and SW (3.3 m / s).
Statistical analysis of wind conditions occurring in the thinning multi‐year period 1970 ÷ 1988 indicated that [35]:
in the middle of the most frequent wind direction SW (20.81%), NW (14.90%) and W (13.86%) and the least likely of the directions E (3.79%) and S (8.99% ) Total silence accounted for 6.14% of all observations, which gives 22.5 days a year with no wind, strong winds in excess of 50 on the Beaufort scale (for speeds above 10 m / s) blew average of 12.7 days in the year, accounting for 3.48% of all observations, the annual average wind speed Trzebiez was 4.69 m / s, characterized by the highest average speed winds from the northern sector N (5.6 m / s), NW (5.4 m / s) W (5.2 m / s); the weakest winds occurred from the south: S (4.4 m / s).
Comparison of the frequency direction and wind velocity and average wind speeds of individual fields designated Swinoujscie thinning and graphically illustrated in Fig. 8 and 9.
Operation of the wind on the surface of Szczecin Bay cause its height differences, without changing the total weight of the water in the tank. The results of the model calculations [76] indicates that at very high wind speeds of about 20 m / s, the difference in water levels in the lagoon on the windward side and the leeward side is maximum 50 cm. The winds of velocities up to 10 m / s will result in much smaller difference in water levels in the Lagoon not exceed several centimeters. Despite almost twice the acceleration, winds latitudinal direction (i. W and E) deniwelują surface of the body of water to a similar extent as the longitudinal direction of the wind (ie. N and S). Decide on the bathymetry of the basin, especially in the direction of extension of latitudinal belt greatest depth,
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
SWINOUJSCIE clearing
75 75 [day NW [days NE NW NE 50 50
25 25
SW SE SW SE
Lynx. 8.Częstotliwości and wind speeds of Swinoujscie and Trzebież (source: [35]).
SWINOUJSCIE SWINOUJSCIE
Lynx. 9.Średnia speed winds Świnoujście Trzebiez (ssource: [35]).
Wind impacting directly on the surface of the water in the form of wind friction also causes waving. Wave height of the wind depends on three main factors: wind speed and direction, duration, and run the wave. Maximum wind waves Szczecin Lagoon observed with winds from the west (W), then the directions E, SE and SW, and the lowest ‐ the directtions N and SW (May). Similarly, the highest average wave perriods arise when the western winds, the smallest ‐ with winds from the northern and south‐western. The maximum measured wave height were 2.0m brine [76], in the summer waves are generally less than 1.4 m. 45
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Wind Ripple caused by moderate and strong winds ‐ due to the shallowness of the lagoon ‐ and reaches the bottom of the water molecules in motion wave abduct sediments, float it and move with the currents. According to [76] during periods of storm water molecules orbital velocity at a depth of 6.0 m may reach up to 1 m / s. Wind wave phenomenon is accompanied by the so‐called. wave currents. The speed of these currents are generally small ‐ to a depth of 6.0 m is approx. 0.05 m / s, but at smaller depths of bottom current speed waveform can be much higher [76].
Characteristics of hydrodynamic. Complexity of the relationship between the drivers of the hydrodynamics JCWP Szczecin lagoon and its complicated system hydrographic make the determination of the flow conditions in the specific sections requires the involvement of appropriate numerical or hydraulic models.
From the point of view of this report, concerning the impact assessment of the Project entitled. "Modernization Swinoujscie‐Szczecin to a depth of 12.5 m" For water protection JCWP Szczecin Lagoon important characteristic is the hydrodynamic conditions occurring both in the strait Świny and Szczecin Lagoon.
The basic size dominate the dynamics of the flow in the carpal Świny is the size and direction of the difference of water levels (bleed) between its ends. The results of long‐term observations carried out in the strait Świny indicate that the frequency of appearance of the positive bleed (drain into the sea) is greater than the negative (inflow from the sea to the Lagoon) and is 56 ÷ 64% [67]. In subsequent years, the ratio of the inflow and outflow of water in the strait depends primarily on the size of the total flow from the top of the Oder catchment. High flows associated wezbraniom on the Oder are reflected in the inhibition of the influx of water from the sea to the lagoon after about 1 ÷ 2 months.
Analysis of bleed in the strait Świny indicates that the most they vary in the range of ‐4 to 5 cm. On average, higher bleeds observed more frequently in the autumn and winter than in spring and summer. Given [67] that in the multi‐year period 1948 ÷ 1957 major bleeds were:
in autumn and winter period for discharge into the sea: 108 cm, the inflow of the Lagoon: ‐98 cm in the spring and summer for the outflow to the sea: 77 cm, for the influx of the Lagoon: ‐60 cm.
Based on the test results ‐ using the results of measurements made in the field and hydraulic models and the results of calculations carried out on numerical models ‐ have been developed at the Institute of Hydraulic Engineering Sciences in Gdańsk [67] curves illustrating the dependence of the flow rate in each channel strait Świna the difference in water level Szczecin Lagoon (Thinning) and the Pomeranian Bay (Swinoujscie). These relationships have been determined for steady flow conditions, which requires the maintenance of a constant
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
difference of water levels at the ends of the strait for a long time. Such situations are quite rare, therefore read the above. flow rate curve should be considered approximate. It should be emphasized that the unsteady flow conditions, eg. During storm surges in flow channels Piastowskim Mielińskim and are often much higher (up to approx. 35%) than that of a flow curves developed for fixed traffic conditions.
Determined by the IBW PAN ‐ based on a mathematical model calculations taking into account the conditions of morphometric the years 1968 ÷ 70 [67] ‐ the above. curves for the Piast Canal and Canal Mielinski shown in Fig. 10.
Analysis of these curves shows that:
at the same absolute values fall between the Szczecin Lagoon and the Gulf Pomeranian flow rate at the outlet of water from the sea it is greater than the inflow of water from the sea to the Lagoon - 6 ÷ 8% in the case of Channel Piastowskie and about 2 to 3% more in the case of Channel Mielinski, the most frequent strait Świny low heads (-4 to 5 cm) flow in the Channel Piastowskim traffic conditions set ranges from approx. -300 m3 / s to approx. 450 m3 / s respectively Channel Mielińskim from approx. ‐270 m3 / s to approx. 350 m3 / s, low heads reaching maximum of 1.5 m, an estimated flow Channel Piastowskim may be approx. 3200 m3 / sec for discharge into the sea and approx. -2900 m3 / s in the case of flow into the lagoon; Channel Mielinski for these flows may be respectively: approx. 2,800 m3 / s and approx. ‐2700 m3 / s.
Szczecin Lagoon is a large but relatively shallow tank, which makes it particularly susceptible to circulate water mass induced by the wind. An important role in shaping the lagoon water circulation systems also play: inflow of water from the catchment area of the Oder, two‐way flow of water in the straits connecting the lagoon with the Pomeranian Bay and bathymetry of the lagoon.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Q [m3 / 3500
3000
2500
2000
1500 Piastowski Canal (outflow to the sea) Channel Piast (inflow of the Lagoon) 1000 Mieliński channel (outflow to the sea)
0 0.00.10.20.30.40.50.60.70.80.91.01.11.21.31.41.5
Lynx. 10.Zależność Flow Channel Piastowskim and the channel difference Mielińskim between water level and the thinning Świnoujście determined traffic conditions (Source: Prepared from [67]).
Landmarks in the Szczecin is the presence of density‐stratified flows, which mixing occurs to fresh water mainly carried out by the Oder salt sea water. Due to the presence of a deep trough fairway Swinoujscie Szczecin mixing processes and exchange of water in brine they are very intense. After wezbraniach strong storm when there are rapid flows of salt water from the sea, and in the deeper parts of the fairway recorded salinity water salinity corresponding Pomeranian Bay ie. ‰ 5 ÷ 7. Range wedge of salt water reaches an average of up to cross in Police (ie, 50 km from Swinoujscie), and water with a salinity of 1.5 ‰ is observed even at the height of the Oder River in Szczecin.
Research on currents made by the Szczecin Lagoon Majewski in the 60s of the twentieth century. [67] indicate that they are characterized by relatively low‐speed measuring an average of 0.05 m / s and a very low stability. Higher average speed occurred only at the entrance to the canal Piastowskie ‐ approx. 0.20 m / sec at the mouth of the Old Świny (0.09 m / s) and at the mouth of the Oder (0.085 ÷ 0.11 m / s). It should be stressed that the highest measured speed currents were greater at the bottom (0.30 m / s) than at the surface (0,25 m / s). The surface layer is highest velocity along the foot of the slopes shallows eastern and northern reservoir in the outlet of the channel and the Old Piastowe Świny, while at the bottom of the greatest speed occur along the fairway, and connecting the gutter Small and Big Lagoon [67].
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
The observed large variation in current direction indicates a large movement of the instability of water within the Lagoon. Among the areas with a highlighting clear to the predominant direction of current Majewski [76] has distinguished water path Swinoujscie‐Szczecin predominantly inflows from the sea bottom to the reservoir and a part of the reservoir between the water line and the south‐western shore of the reservoir with a predominance of current drain.
The study water circulation in the Szczecin Lagoon ran in the 80s of the twentieth century. Water Institute of Building Sciences (IBW PAN) [67]. The results of field measurements and calculations on hydraulic model indicated that the circulating water systems in the Szczecin Lagoon depend primarily on the strength and direction of the wind. The authors [67] provide some general features forming system for circulating brine ‐ schematically them Fig. 11. In both parts of Szczecin Lagoon ‐ ie. In the Large and Small Lagoon ‐ there tends to be two water circulation system and which direction It depends primarily on the direction of the wind and to a lesser extent on the direction of flow in the Strait Świna.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
west wind
east wind
south wind
west wind and intense inflow of water from the sea
west wind and the water outlet to the sea
Fig. 11. Landmarks water circulation systems Szczecin Lagoon according to [67].
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.2.3. Measles JCWP from Párnica to the mouth.
The heavily modified surface water body (JCWP) PLRW6000211999 Oder from Párnica to enter the mouth (Fig. 4): Odra from Párnica to Glen Oder (Odra western arm) with a length of approx. 26.5 km, Regalica (eastern side of the Oder) from Párnica to the lake Dabie with a length of approx. 2.3 km section running through the lake Dabie with Ińskim Nurt length approx. 13.0 km. The length of the courses relevant JCWP is 29.047 kilometers [32, 78].
Measles is the second largest Polish river. Its total length is 840.90 kilometers, of which the Polish borders is 726.48 kilometers. Odra river basin with an area of 119 thousand. km2 characterized by a marked asymmetry of ‐ the surface ratio of the basin left to right is 3: 7. Sources are in the Odra Odra Mountains in the Czech Republic. Odra Odra flows into the Glen which is part of the Szczecin Lagoon, combined with the Pomeranian Bay three straits Świna, strange and Foam.
Hydrological and hydrodynamic conditions in the Odra JCWP from Párnica to the mouth are the result of interactions such phenomena as:
variable sea states causing backwater odmorskie, variable cash flows from the top of the river causing changes in water levels of niżówkowych to flood wind turbines causing backflow causing additional podpiętrzenie (in the case of northern winds) or the lowering of water (in the case of wind Southern) atmospheric pressure changes associated with the passage depressions atmospheric pressure causing transient surges (INFERENCE waves) human activity is changing bathymetry of the river and its hydrographic system.
Simultaneous overlapping influences odmorskich and runoff from the catchment area of the Oder makes the area of the mouth of the Oder can not talk about the interdependence between states of water and flows, Characteristics of hydrological JCWP Odra from Párnica to the mouth based so it can only on the states of the water and not on the flows.
Wodowskazowym section representative for ‐ located within the area JCWP Odra from Párnica to the mouth of Swinoujscie‐Szczecin post wodowskazowy Szczecin Long Bridge is located in the 739.9 km of the river Odra (according to [1, 20] 22.85 km), belonging to the network observation of the Institute of Meteorology and Water Management Branch in Gdynia.
Water gauge in Szczecin (Long Bridge) was established the 1 October 1810. at the former bridge (approx. 300 m below the bridge current) on the ordinate or ‐0528 m. NN. In r. 1936 to zero gage decreased to ‐5.000 m or elevation. NN. During World War II the bridge was destroyed, water gauge, however, has not been destroyed, because it was attached to the wall profile Boulevard bridge. In September of 1958. With the completion of construction of a new road bridge (the current bridge Long) water gauge was moved to his left beachhead, from the bottom and water 51
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
set ‐ in view of the minimum water level drop between the old and new bridge ‐ at the same elevation or ‐5000 m. NN. After performing the leveling 1966 to sea level in Kronstadcie ordinate gage is zero or ‐5123 m. Cr. In 1985, water gauge was moved over the bridge without changing its elevation zero. The catchment area of the Oder to the above. wodowskazowego section is 114,947.38 km2.
Characteristic and maximum annual water levels of a specific exceedance probability for the station gauges Szczecin, determined on the basis of the data contained in [4] and [69] are summarized in Table. 7 and Tab. 8.
Table 7. Specific conditions for water gauges Szczecin designated stations with multi‐year in 1959 ÷ 2000 [4].
Characteristic water levels H [cm] absolute maximum 622 (11.04.1995) maximum Websi 622 (4.11.1995 medium high CSG 587 averag SSW 512 medium low SNW 459 minimum accide 433 (11.14.1993) absolute minimum 433 (11.14.1993)
Table 8. The maximum annual water levels of a certain probability of exceedance in Szczecin designated for multi‐year in 1948 ÷ 2007 [69].
Annual maximum water levels [cm] of the exceedance probability * 0.1 0.5 1 2 5 10 50 665 645 637 628 616 606 580 * Mean values of the two distributions: Gumbel and Pearson III
Information about the volume of water flowing to JCWP Measles from Párnica to the water outlet from the top section of the Oder originated from wodowskazowego Gozdowice located at 645.3 km River (by [1, 20] 117.59 km). It should be emphasized that this is the last water gauge section for which data are given about the flow of the Oder ‐ Odra section below Gozdowice is under the influence of the sea and can not be fixed for him to determine the relationship‐state flow.
Water gauge in Gozdowicach It was founded in 1854. at 3,168 meters elevation relative. NN. At present site was moved in 1878 taking into account the decline ‐ ie. Zero elevation of 3.20 m
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
or. NN. After zaniwelowaniu to sea level in Kronshtadt zero elevation is 3.020 m or. Cr. The catchment area of the Oder to the above. wodowskazowego section is 109,795.07 km2.
Characteristic and the maximum annual flows Odra exceedance probability for a specific station gauges Gozdowice, determined on the basis of the data contained in [4] are summarized in Table. 9 and Tab. 10.
Table 9. Specific movements of stations designated gauges with multi‐year Gozdowice 1952 ÷ 2000 [4].
specific movements Q [m3/ S] maximum WWQ 3180 medium high SWQ 1251 averag SSQ 535 medium low SNQ 252 minimum NNQ 134 (01.06.1954)
Table 10. The maximum annual flows Odra specified exceedance probability in the multi‐year Gozdowicach set for 1952 ÷ 2000 [4].
The maximum annual flow [m3/ S] of the probability of exceedance 0.1 0.5 1 2 5 10 50 3426 2956 2730 2493 2164 1899 1165
4.1.2.4. JCWPd 1, 4, 7
Dolna Odra and Szczecin Lagoon and the Strait of Świna are located in the following three areas of groundwater bodies, dedicated for the development of the Plan of water management in the basin of the Oder: PLGW67001, PLGW67002, PLGW69007, PLGW690025 (Fig. 5).
In the course of the preparatory work for updating management plans in Poland we have developed a new division of the groundwater bodies. According to the implementation of the Project and related projects will be implemented in the area of groundwater bodies: PLGW60001, PLGW60004, PLGW60007.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.3. Qualification in terms of hydro‐morphological changes.
4.1.3.1. JCWP Świna Estuary.
JCWP Estuary Świna at the stage of implementation of the Water Framework Directive and the development of the first water management plans for the river basin was considered heavily modified [33]. Carried out in 2012. By the Regional Water Management Board in Szczecin verification designation of heavily modified and artificial transitional and coastal waters in the area of its operation, this qualification maintained [32, 78].
Ww. verification has been made on the basis of carried out by the Institute of Meteorology and Water Management, National Research Institute, Maritime Branch in Gdynia work entitled .: Development of the methodology to verify the designation of heavily modified and artificial transitional and coastal waters (hereinafter Methodology) [31].
According to the methodology in [70] for JCWP Estuary Świna ‐ as well as for other water bodies transitional area of operation RZGW in Szczecin ‐ the first hydro‐morphological changes were identified and then evaluated the significance of these changes and their impact on ecosystems.
Carried out for the area of transitional measures in Szczecin RZGW expert assessment of the significance of the identified hydrological changes and their impact on ecosystems did not give rise to these waters because of this show as heavily modified. Within the above. Although there has been a change of water flow distribution between the Oder three strait connecting Szczecin Bay of Pomeranian Bay in connection with the adaptation Świny for shipping. However, work in this direction were spread out in a long time. It made changes in hydrological conditions ‐ as well as morphological and chemical ‐ in these areas followed in an evolutionary manner, allowing ecosystems to adapt to them in the same way. Completion of the above. work took place over a century ago, and the available data from the last century do not suggest that during this period there have been significant changes in hydrology.
Morphological changes in the estuary JCWP Świna are associated with both hydro‐technical infrastructure, as well as the work they carry out concerning the maintenance and dredging fairways.
According to the Methodology of assessment of the significance of the above. morphological changes and their influence on the estuary ecosystems Świny was made using the impact indicator WskWp described by the following formula:
n WskWp (WskZn Chg) (1) 100
and DLlubDP
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
where: n ‐ The number of types of morphological changes within the assessed JCWP, WskZn ‐ relevance indicator morphological changes (see table 4 Methodology) d ‐ hydro‐morphological changes expressed by the total surface area [km2] or section length [km], where present, DL the total length of the edge of the area JCWP or reviewed by the [km] DP ‐ surface area subject JCWP or assessment [km2]. it is recommended to use surface active zone
WskWp impact indicator is a measure of the decrease in the resistance of ecosystems the water body transition (or bay) as a result of anthropogenic morphological changes. In Methodology it assumed that the threshold changes in resistance to water transition above which the change of state of classes of organic good at less than 15%.
According to [32, 78] for JCWP Mouth Świny to calculate the impact WskWp, according to the methodologies as evaluated area were taken shallow active zone of the edge profile. According to table 2 Methodology for the present JCWP amounts to 150 m. At the edge length DL = 4.327 km, the surface area of the active DP = 0.649 km 2 [9, 72].
Inventoried under [64] morphological changes within JCWP Mouth Świny Tab.11 summarized in [32, 78]. This table also corresponding to each change signification indices and the calculated partial and total impact indicators.
Table 11. Morphological changes within the JCWP Mouth Świny its assessment [32, 78].
relevance ecosystem kind of change d changes WskWp degree WskZn of change [%]
1 The total area of fairway aggravated * 0.255 0.50 19.65 The total area exposed to changes in bottom 2 sediments violation (trawling, anchoring and 0.15 turntables)
The total area of the stored ore bagrowanego 3 0.19
The total length of the edge Building spurs 4 0.20 piers 5 The total length of the breakwaters 0,300 0.20 1.39
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
6 The total length of the deep fairway at the mouth 0,150 0.10 0.35 7 The total length of the transverse structure 0.25 8 Total length of quays 0.25 9 The total length of the edge bands (reinforcements) 0.20 10 The total length of the supplied bank of 0.08 11 The total length of dikes 0.13 The calculation result of changes in ecosystem resilience [%] 21.39
*) As with the provisions of the surface Methodology seaway ‐ as an area in which a dredging in a constant affect the structure of the bottom ‐ it is multiplied by 10.
Mouth JCWP obtained for index value Świny impact WskWp equal to 21.39%, pre‐qualify the body of water to heavily modified.
Next steps for determining the qualifications JCWP Estuary Świna included:
analyzing the possibility of applying environmental recovery efforts for achieving good ecological status - this analysis showed that the mouth Świna identified for restitution action would have a more negative impact on its ecosystems, rather than leaving this body of water in the state of hydromorphological, analyzing the possibility of using the functional replacement alternatives currently occurring anthropogenic pressures resulting in morphological changes and options which are much better environmentally - this analysis showed no functional alternatives to currently existing in the estuary Świna anthropogenic pressures associated with shipping and securing the edges.
The results of the above. of analysis entitle therefore to the ultimate discretion JCWP Mouth Świna for heavily modified transitional waters.
4.1.3.2. JCWP Szczecin Lagoon.
JCWP Szczecin Lagoon at the stage of implementation of the Water Framework Directive and the development of the first water management plans for the river basin was considered heavily modified [33]. Carried out in 2012. By the Regional Water Management Board in Szczecin ‐ based on the above. Methodology ‐ verification determination of highly modified and artificial transitional and coastal waters in the area of its operation, the classification retained [32, 78].
Morphological changes in JCWP Szczecin Lagoon are associated with both hydro‐ technical infrastructure, as well as the work they carry out concerning the maintenance or dredging waterways and ports of approach.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Inventoried under [68], morphological changes within JCWP Szczecin Lagoon summarized in Tab. 12 [32, 78]. This table also corresponding to each change signification indices and the calculated partial and total impact indicators WskWp. According to [32, 78] in the calculations assume that the total length of the edge JCWP Szczecin Bay equal to DL = 321.76 km, while the area DP = 407.28 km2.
Table 12. Morphological changes within the JCWP Szczecin Lagoon and their evaluation [32, 78].
relevance ecosystem kind of change d changes WskWp degree WskZn of change [%]
1 The total area of fairway aggravated * 43,05 0.67 7.08 The total area exposed to changes in bottom 2 sediments violation (trawling, anchoring and 24.83 0.20 1.22 turntables) **
The total area of the stored ore bagrowanego *** 3 2.30 0.50 0.28
The total length of the edge Building spurs 4 0.25 0.00 piers 5 The total length of the breakwaters 2.54 0.40 0.32 The total length of the fairway for deep lagoons 6 43.75 0.40 5.44
7 The total length of the transverse structure 0.50 0.00 8 Total length of quays 6.68 0.50 1.04 9 The total length of the edge bands (reinforcements) 17.24 0.20 1.07 10 The total length of the supplied bank of 0.08 0.00 11 The total length of dikes 70.03 0.13 2.83 The calculation result of changes in ecosystem resilience [%] 19,28
*) In accordance with the methodology the surface area of the work alter the structure of the bottom is to be multiplied 10. The multiplier was used only for fairway Szczecin‐Swinoujscie (surface area 4.092 km2), Because in this area dredging is carried out continuously. The remaining tracks (an area of 2.131 km2 ) Are carried out as needed. **) In accordance with the Methodology changes bottom surface multiplied by 10, recognizing that they are the work of / objects affecting the bottom. ***) was abandoned by multiplying by 10. It was decided that this work does not affect the bottom continuously. The bottom has been breached only during the construction of the landfill. The calculations take into account the current ‐ and do not target ‐ refulacyjnych fields.
JCWP obtained for index value Szczecin Bay impact WskWp equal to 19.28%, pre‐qualify the body 57
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
of water to heavily modified.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Whereas the results of subsequent stages of verification of qualifications JCWP Szczecin Lagoon, to perform an environmental analysis of the applicability of action for restitution and analysis of the applicability of functional alternatives, have authorized the final discretion JCWP Szczecin Lagoon for heavily modified transitional waters.
The conducted under the [7] analysis shows that the implementation of the second stage of the modernization Swinoujscie‐Szczecin results in an increase of the impact indicator WskWp JCWP Szczecin lagoon to 20.27%. This is due to the increase in surface aggravated fairway (about 0.324 km2) which requires ‐ in view of the structure of the bottom of the continuous violation ‐ multiplying by 10, making approx. 7.12 km revetments and increased by 0.05 km long quays.
Made in [7] of the [31, 68], quantification of the lesions in the JCWP Szczecin Lagoon after the second stage upgrading Swinoujscie‐Szczecin presented in Table 7.
Table 7. Morphological changes within the JCWP Szczecin Lagoon after the second stage upgrading Swinoujscie‐Szczecin its assessment of [7].
relevance ecosystem kind of change d changes WskWp degree WskZn of change [%]
1 The total area of fairway dredged 46,29 0.67 7.62 The total area exposed to changes in bottom 2 sediments violation (trawling, anchoring and 24.83 0.20 1.22 turntables)
The total area of the stored ore bagrowanego 3 2.30 0.50 0.28
The total length of the edge Building spurs 4 0.25 0.00 piers 5 The total length of the breakwaters 2.54 0.40 0.32 The total length of the fairway for deep lagoons 6 43.75 0.40 5.44
7 The total length of the transverse structure 0.50 0.00 8 Total length of quays 6.73 0.50 1.05 9 The total length of the edge bands (reinforcements) 24.36 0.20 1.51 10 The total length of the supplied bank of 0.08 0.00 11 The total length of dikes 70.03 0.13 2.83 The calculation result of changes in ecosystem resilience [%] 20.27
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.3.3. Measles JCWP from Párnica to the mouth.
Measles JCWP from Párnica to the mouth at the stage of implementation of the Water Framework Directive and development of management plans for the river basin was considered heavily modified [33]. According to [2], that classification decided morphological changes associated with buildings elongate trough. According to [32, 78] the total length of watercourses important this JCWP equal to 29.047 kilometers, the total length of the sections where work was carried out control (construction and longitudinal shift is documented) is approx. 15.395 km (approx. 53%). Carried out by the Regional Water Management Board in Szczecin on the need to update those plans to verify the designation of heavily modified and artificial bodies of water above the river. qualification maintained.
4.1.4. Assessment of the current status of water bodies.
The status of identified quality of surface water bodies in the period of 2011 ÷ 2013 was studied by the Provincial Environmental Protection Inspectorate (WIOŚ) in Szczecin:
in the case of JCWP Mouth Świna ‐ three measuring positions: SW, SW‐I, IV; in the case of JCWP Szczecin Lagoon ‐ seven measuring positions C, E, F and H are in the Greater Lagoon, SWR located in the strait Świny, B2 located on Channel Piastowskim JWW and being in the area of the lake Wicko; in the case of JCWP Measles from Párnica to the mouth ‐ on three measuring stations: Western Odra ‐ Long Bridge (Szczecin), Western Odra ‐ Base UMS (Szczecin), Oder ‐ estuary to Glen Oder (Police).
Location above. positions is shown in Fig. 12.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources in accordance with the requirements of the Water Framework Directive
Fig. 12. Posts measuring the State Environmental Monitoring in the area JCWP Estuary Świna JCWP Szczecin Lagoon, Odra JCWP from Párnica to the mouth (own study on the basis of: [40]). 60
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.4.1. JCWP Świna Estuary.
JCWP state Świna Estuary in 2012. Was classified as poor. [72] His assessment was carried out by WIOŚ in Szczecin, according to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and environmental quality standards for priority substances3.
Ww. Regulation ‐ like the current Minister of Environment of 22 October 2014.4 ‐ required to make:
classification of the status / capacity5 organic based on the results of studies of the biological elements and their supporting elements of hydro‐morphological and physicochemical properties, including substances that are particularly harmful to the aquatic environment. the chemical status classification on the basis of measurements of substances and other priority pollutants listed in Annex 9 to Regulation assessment of the results of the classification of state / ecological potential and chemical status.
In the case of transitional water bodies indicators of water quality classification serving state / ecological potential are:
in terms of biological elements: phytoplankton (chlorophyll "a"), macroalgae and angiosperms (index SM), benthic macroinvertebrates (multimetryczny index B) fish fauna;
on the elements hydromorphological: the flow of fresh water (hydrologic balance, including the inputs of fresh water retention time and replacement, variable meteorological) depth variation (shape pool) Quantitative structure and the base bottom (particle size, the content of organic compounds) Tide band structure (covering plants, the plants);
3 OJ 2011 No. 257, item. 1545 4 Dz. U. of 2014. Pos. 1482 5 ecological status is determined for surface water bodies designated as a natural, ecological potential for designated as artificial or heavily modified.
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in terms of physicochemical elements: as indicators characterizing the physical condition: water transparency (Secchi depth) as indices characterizing the oxygen and organic contaminants6: Dissolved oxygen at the bottom7. total organic carbon, oxygen saturation in the layer 0 ÷ 5 m8. salinity9 and as an indicator characterizing acidity: pH; as indicators characterizing the nutrient conditions: ammonium nitrogen, nitrate nitrogen, total nitrogen, phosphate, total phosphorus, nitrogen, mineral, as especially harmful to the aquatic environment (specific impurities synthetic and non-synthetic) formaldehyde, arsenic, barium, boron, chromium, hexavalent chromium general, zinc, copper, phenols, volatile (phenol index), hydrocarbons of petroleum (index mineral oil), aluminum , free cyanides, cyanide-related, molybdenum, selenium, silver, thallium, titanium, vanadium, antimony, fluoride, beryllium, cobalt, tin.
Based on research conducted in 2012 as part of diagnostic monitoring (position SW) and operational (position IV) and study of the fish fauna of 2011 ‐ used based on the principle of inheritance ‐ ecological potential JCWP Mouth Świna was assessed as weak. [80]
Made in 2012. Research chlorophyll "a" and macrozoobenthos showed that these biological elements are respectively II and class IV water quality. Research macroalgae and angiosperms were not performed. In contrast, carried out in 2011. Ichtyofauna studies indicated class II water quality. Based on the above. findings ecological potential JCWP Mouth Świna in the field of biological elements was assessed as weak.
In accordance with the principle that a body of water, not assigned on the basis of reviewing the terms hydromorphological as artificial or modified is suitable in the range of hydromorphological elements class I, whereas the body of water designated as artificial or modified class II potential ecological JCWP Mouth Świny on the elements hydromorphological He was assessed as good.
Ecological potential JCWP Mouth Świna in terms of physico‐chemical elements has been assessed as less than good. Such an evaluation water potential decisive test results
6 The Ordinance of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and environmental quality standards for priority substances as an indicator of this group was even mentioned five‐ biochemical oxygen demand BOD5 7 The minimum values
8 The maximum values
9 It does not set any limits
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
transparency water (Secchi depth), total nitrogen, and soluble forms of nitrogen (nitrate nitrogen and mineral).
The evaluation of the chemical status JCWP Estuary Świna was based on the results of in 2012. In the monitoring diagnostic testing of all indicators of chemical status specified in Annex 9 to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and the environment quality standards for priority substances in water samples taken on two occasions during the season a research position SW. After verification of the measurement results of the assessment were excluded indicators for which the limit of quantification than 100% of the most stringent limit value, and which also occurred at concentrations below the detection limit of the analytical method, ie. Endosulfan and nonylphenols. The assessment included while tributyltin compounds, for which the detection limit is also exceeded 100%. This indicator performed because in concentrations above the limit of quantification.
Chemical status JCWP Mouth Świna was assessed as less than good. The assessment decided exceeding the annual average of the brominated diphenyl octylphenol and the values of average and maximum tributyltin compounds.
The latest available results of estuary waters JCWP 2013 Świna concern. And come up with three positions SWI, SW and IV [71]. They are summarized in Table. 13, specifying limits for individual indicators in accordance with the Regulation of the Minister of the Environment of 22 October 2014. On the classification of surface water bodies and environmental quality standards for priority substances. In the absence of measurements in 2013. Presents the results of 2012. The table shows that in 2013. ‐ just like in 2012. ‐ limits II grade exceeded were for the following indicators: transparency and nutrients: nitrogen, ammonium and total nitrogen, nitrate nitrogen, mineral nitrogen. At the same time there has been a deterioration of water quality in terms of phytoplankton (from Class II to Class IV) and total phosphorus (from class II to class lower). In the table are also given in [41] The SI for fish fauna (class II).
According to [41] assessment of the chemical JCWP Świna estuary in 2013. Has been fully inherited from 2012.
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Table 13. Test results JCWP Świna estuary in 2013. And 2012. (Source: [41, 71, 80]).
the concentration of the concentration limits No. name quality index unit SWI SW IV class I class II class III class IV class V ecological potential 1.1.5 Phytoplankton ‐ chlorophyll "a" mg / l 13.7 16.8 14.8 <5.00 ≤7,50 ≤15,00 ≤25,00 > 25.00
Macroalgae and angiosperms 1.4 ≥0,95 ≥0,80 ≥0,57 ≥0,20 <0.20 ‐ an indicator SM1
benthic macroinvertebrates 1.5 2.38 2.01 > 3.72 ≥3,18 ≥2,70 ≥1,91 <1.91 ‐ multimetryczny index of B *
1.6 Ichthyofauna ‐ indicator SI 3.4 ≥4,4 ≥3,4 ≥2,4 ≥1,4 <1.4 3.1.4 Transparency m 1.5 1.4 1.5 > 5.00 > 3.75
3.2.1 Dissolved oxygen above the mg / l O2 5.28 7.50 8.42 > 6 > 4.2 bottom The total organic carbon (TOC) 3.2.4 mg / l C 7.2 7.8 6.5 ≤5 ≤10
oxygen saturation 3.2.5 % 119.6 117.0 112.7 90‐110 80‐120 ‐ a layer of 0‐5mA 3.5.1 ammonium mg / l N‐ 3.5.3 nitrate nitrogen mg / l N‐ 0.61 0.58 0.54 <0.18 <0.27 3.5.5 total nitrogen mg / l N 0.91 0.86 0.78 <0.35 <0.53
3.5.6 phosphates PPO 4 mg / l P‐PO4 0,025 0.032 0.015 <0.022 <0.035 3.5.7 total phosphorus mg / l P 0.056 0,055 0.049 <0.031 <0.045
Mineral nitrogen [NNO3+ 3.5.9 mg / l N 0.714 0.658 0.583 <0.21 <0.32 N NO2+ NNH4] 64
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
average concentration for concentration limits No. name quality index unit SW class I class II class III class IV class V 3.6.1 formaldehyde mg / l ≤0,05 3.6.2 Arsenic * mg / l As 0.001 ≤0,05 3.6.3 bar * mg / l Ba 0.023 ≤0,5 3.6.4 Bor * mg / l Ba 0.74 ≤2 3.6.5 Chrome 6 * mg / l Cr <0.0005 ≤0,02 3.6.6 Chrome overall Reg. * mg / l Cr <0.0005 ≤0,05 3.6.7 zinc * mg / l Zn 0.015 ≤1 3.6.8 copper * mg / l Cu 0.003 ≤0,05 3.6.9 Phenol index * mg / l 0.0027 ≤0,01 3.6.10 Index Oil * mg / l 0.005 ≤0,2 3.6.11 Aluminum* mg / l Al. 0,009 ≤0,4 3.6.12 Cyanide‐free * mg / l CN 0,002 ≤0,05 mg / l 3.6.13 cyanide‐related ≤0,05 Me 3.6.14 molybdenum mg / l Mo ≤0,04 03/06 Selenium mg / l Se ≤0,02 3.6.16 Silver mg / l Ag ≤0,005 03/06 Thallium mg / l T ≤0,002 3.6.18 Titanium mg / l Ti ≤0,05 06/03 Vanadium mg / l V ≤0,05 06/03 Antimony mg / l Sb ≤0,002 06/03 Fluoride mg / l F ≤1,5 03/06 Beryllium mg / l Be ≤0,0008 03/06 Cobalt mg / l Co ≤0,05
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
chemical status concentration concentration limits No. name quality index unit average max average max allowed 4.1.1 alachlor mg / l <0.005 0.005 0.3 0.7 4.1.2 Anthracene mg / l <0.0005 <0.0005 0.1 0.4 4.1.3 atrazine mg / l <0.055 0,055 0.6 2 4.1.4 Benzene mg / l <0.5 <0.5 8 50 4.1.5 brominated diphenyl mg / l 0.68 0.0002 4.1.6 Cadmium and its compounds mg / l 0.199 0.386 0.2 depending on the hardness of ≤0,05 4.1.7 C10 ‐ 13 ‐chloroalkany mg / l 0 0 0.4 1.4 4.1.8 Chlorofenwifos mg / l <0.045 0,045 0.1 0.3 4.1.9 chlorpyrifos mg / l <0.015 0.015 0.03 0.1 4.1.10 1,2‐dichloroethane (EDC) mg / l <2 10 4.1.11 dichloromethane mg / l <3 20 Phthalate, di (2‐ 4.1.12 mg / l <0.3 1.3 ethylhexyl) 4.1.13 diuron mg / l <0.02 0.02 0.2 1.8 4.1.14 endosulfan mg / l 0.0005 0,004 4.1.15 fluoranthene mg / l 0.00098 0.00164 0.1 1 4.1.16 Hexachlorobenzene (HCB) mg / l <0.0005 0.0005 0.01 0.005 4.1.17 Hexachlorobutadiene (HCBD) mg / l <0.015 0.015 0.1 0.6 4.1.18 Hexachlorocyclohexane (HCH) mg / l 0 0 0,002 0.02 4.1.19 isoproturon mg / l <0.015 0.015 0.3 1.0 4.1.20 Lead and lead compounds mg / l 0.71 7.2 4.1.21 Mercury and its compounds mg / l <0.006 0.021 0.05 0.07
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concentration concentration limits No. name quality index unit average max average max allowed 4.1.22 Naphthalene mg / l <0.0044 1.2 4.1.23 Nickel and its compounds mg / l 1.0 20 4.1.24 nonylphenols mg / l 0.3 2 4.1.25 octylphenol mg / l 0.012 0.01 4.1.26 pentachlorobenzene mg / l <0.0001 0.0007 4.1.27 Pentachlorophenol (PCP) mg / l <0.15 0.15 0.4 1 4.1.28 Benzo (a) pyrene mg / l <0.0005 0.0005 0.05 0.1 4.1.28b Benzo (b) fluoranthene mg / l 4.1.28c Benzo (k) fluoranthene mg / l Sum 0 0.03 4.1.28d Benzo (g, h, i) perylene mg / l 4.1.28 Indeno (1,2,3‐cd) pyrene mg / l Sum 0.0004 0,002 01/04/2 simazine mg / l <0.015 0.015 1 4 4.1.30 tributyltin compounds mg / l 0.0005 0.0016 0.0002 0.0015 4.1.31 Trichlorobenzene (TCB) mg / l 0 0.4 4.1.32 trichloromethane mg / l <0.25 2.5 04/01/3 trifluralin mg / l <0.0005 0.03 4.2.1 tetrachloromethane mg / l <0.25 0.0099 12 4.2.2 Aldrin mg / l 4.2.3 dieldrin mg / l 4.2.4 Endrin mg / l 4.2.5 isodrin mg / l Sum 0 0.005
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
concentration concentration limits No. name quality index unit average max average max allowed 4.2.6 DDT ‐ para‐isomer para mg / l <0.0005 0.01 4.2.6b DDT total mg / l 0 0,025 4.2.7 Trichlorethylene (TRI) mg / l <0.15 10 4.2.8 Tetrachlorethylene (PER) mg / l <0.11 10 *) On the basis of the 2012.
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4.1.4.2. JCWP Szczecin Lagoon.
JCWP state Szczecin Lagoon in 2012. Was classified as poor. [72] His assessment was carried out by WIOŚ in Szczecin, according to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and environmental quality standards for priority substances10.
Classification of ecological potential JCWP Szczecin Lagoon in 2012. Was made on the basis of [71]:
the results of research conducted in 2012. in the monitoring of the operating positions E, C, H, SWR; and ‐ based on the principle of inheritance ‐ on the basis of: the results of studies of the biological elements of 2011. under the surveillance monitoring positions F, B2, JWW (and in the case also of the macrozoobenthos H) Research fish fauna of 2011 r., test results physicochemical elements characterizing the physical state, oxygen and organic contaminants and nutrient conditions from 2011. from positions F, B2, JWW, the results of the testing of substances that are particularly harmful to the aquatic environment of priority in five positions of surveillance monitoring in 2011., i.e. .: C, H, F, B2, JWW.
It was found that almost all positions of the chlorophyll concentration "a" and the value of which is determined for benthic makrokręgowców multimeric index B are in the fourth or fifth quality class. Exceptions in this regard are the position E and SWR, respectively, in which the average concentration of chlorophyll "a" and the index B multimetryczny limits potential moderate (Class III quality). Moderate ecological potential of the waters of the Szczecin Lagoon evaluation results indicate the fish fauna in the study by the Sea Fisheries Institute entitled .: Evaluation of the ecological status of transitional waters for the year 2011. Pursuant to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and environmental quality standards for priority substances. When assessing the ecological potential classification they should be treated as macroalgae and angiosperms. However, due to the lack of recognition of the prevalence of these organisms in the waters of the Szczecin Lagoon, this item was omitted from the assessment. Taking into account the average of the seven positions of the measurement value of the concentration of chlorophyll "a" and the index B ‐
10 OJ 2011 No. 257, item. 1545
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of respectively 38.35 and 2.05 mg / l ‐ the potential ecological JCWP Szczecin Lagoon in the field of biological elements has been classified as weak.
In accordance with the principle that a body of water, not assigned on the basis of reviewing the terms hydromorphological as artificial or modified is suitable in the range of hydromorphological elements class I, whereas the body of water designated as artificial or modified class II potential ecological JCWP Szczecin Lagoon on the elements hydromorphological He has been recognized as good.
Ecological potential JCWP Szczecin Lagoon in the field of physico‐chemical elements was assessed as less than good. Such an evaluation decided to cross the border of good status of the following indicators: the transparency of water, the content of total organic carbon (TOC) and ammonia nitrogen and water oxygen supersaturation recorded. Regarding test in 2011. For the five measurement positions Szczecin Bay (C, H, F, B2, JWW) 11 indicators from a group of substances that are particularly harmful to the aquatic environment, no exceedances of the limit values for good quality.
Evaluation of chemical JCWP Szczecin Lagoon is fully inherited from 2011. This assessment was based on the results of the part of the monitoring diagnostic testing of all the indicators listed in Annex 9 to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of uniform bodies of surface water and environmental quality standards for priority substances in water samples collected twice during the season test in five positions: C, H, F, B2, JWW [40]. After verification of test results were excluded from the evaluation indicators for which the limit of quantification than 100% of the most stringent limit value, and which also occurred at concentrations below the detection limit of the analytical method (i. Diuron, endosulfan, heksachlorocyklobutadien, nonylphenols, simazine). The evaluation included, however, tributyltin compounds, and brominated diphenylethers, for which the detection limit is also exceeded 100%. These indicators, however, occurred in concentrations above the limit of quantification.
Chemical status JCWP Szczecin Lagoon was assessed as less than good. Such an evaluation chosen to exceed the average annual brominated diphenyl octylphenol and the values of average and maximum tributyltin compounds [40].
The latest available results of water JCWP Szczecin Lagoon relate to 2013. And come up with seven positions: C, E, H, F, B2, JWW, SWR [71]. They are presented in tab.14 giving concentrations ‐ the average of all positions, the highest and lowest of the average for the positions and limit values for each class quality indicators, according to the Regulation of the Minister of the Environment of 22 October 2014. On the classification of bodies of surface waters and environmental quality standards for priority substances. In the absence of measurements in 2013. Presents the results of 2012. Or 2011. The table shows that in 2013. ‐ just like in 2012. ‐ Class II limits were exceeded for quality
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the following ratios: transparency, the content of total organic carbon (TOC), and ammoniacal nitrogen. There were also water saturation of oxygen. At the same time there has been a deterioration in water quality in the area: total nitrogen, nitrate nitrogen, mineral nitrogen. In the table are also given in [41] The SI for fish fauna (class III).
According to [41] assessment of the chemical JCWP Szczecin Lagoon in 2013. It has been fully inherited from 2011.
.
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Table 14. Test results from the Szczecin Lagoon JCWP 2013. (In the absence of 2012. Or 2011). (Source: [41, 71, 80]).
the concentration concentration limits No. name quality index unit average the lowest class I class II class III class IV class V highest ecological potential 1.1.5 Phytoplankton ‐ chlorophyll "a" mg / l 34.10 48.2 23.7 <10.0 ≤20,00 ≤30,0 ≤40,0 > 40.00
Macroalgae and angiosperms 1.4 ≥0,95 ≥0,80 ≥0,57 ≥0,20 <0.20 ‐ an indicator SM1
benthic macroinvertebrates 1.5 2.05 2.82 1.17 > 3.72 ≥3,18 ≥2,70 ≥1,91 <1.91 ‐ multimetryczny index of B *
1.6 Ichthyofauna ‐ indicator SI 3.1 ≥4,4 ≥3,4 ≥2,4 ≥1,4 <1.4 3.1.4 Transparency m 1.1 1.8 0.9 > 2.50 > 1.90
3.2.1 Dissolved oxygen above the mg / l O2 7.33 8.42 4.49 > 6 > 4.2 bottom The total organic carbon (TOC) 3.2.4 mg / l C 11.4 12.5 10.8 ≤5 ≤10 * oxygen saturation 3.2.5 % 130.7 160.3 110.4 90‐110 80‐120 ‐ a layer of 0‐5mA mg / l 3.5.1 ammonium 0.072 0.124 0.052 <0.04 <0.06 N mg / l 3.5.3 nitrate nitrogen 1.18 1.56 0.77 <0.60 <0,90 N‐ 3.5.5 total nitrogen mg / l N 2.25 2.63 1.84 <1.25 <1.90
3.5.6 phosphates PPO 4 mg / l P‐ 0.037 0.059 0.021 <0.060 <0.090 No. name quality index unit the concentration concentration limits 72
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
average the lowest class I class II class III class IV class V highest 3.5.7 total phosphorus mg / l P 0.121 0.147 0.096 <0.100 <0.150 Mineral nitrogen 3.5.9 mg / l N 1,265 1,674 0.835 <0.70 <1.05 [NNO3+ NNO2+ 3.6.1 formaldehyde mg / l ≤0,05 3.6.2 Arsenic ** mg / l As 0.0018 0,002 0.001 ≤0,05 3.6.3 bar ** mg / l Ba 0.028 0.032 <0.025 ≤0,5 3.6.4 Bor ** mg / l Ba 0.133 0.18 0,095 ≤2 3.6.5 Chromium 6 ** mg / l Cr <0.0005 <0.0005 <0.0005 ≤0,02 3.6.6 Chrome overall Reg. ** mg / l Cr <0.0005 <0.0005 <0.0005 ≤0,05 3.6.7 zinc ** mg / l Zn 0.0032 0,004 0,002 ≤1 3.6.8 copper ** mg / l Cu 0.0026 0.003 0,002 ≤0,05 3.6.9 Phenol index ** mg / l <0.001 <0.001 <0.001 ≤0,01 3.6.10 Index Oil ** mg / l 0.0444 0.074 0,027 ≤0,2 3.6.11 aluminum ** mg / l Al. 0.0039 0,004 <0.0025 ≤0,4 3.6.12 cyanide free mg / l CN 0.0021 0,004 <0.015 ≤0,05 mg / l 3.6.13 cyanide‐related ≤0,05 Me 3.6.14 molybdenum mg / l Mo ≤0,04 03/06 Selenium mg / l Se ≤0,02 3.6.16 Silver mg / l Ag ≤0,005 03/06 Thallium mg / l T ≤0,002 3.6.18 Titanium mg / l Ti ≤0,05 06/03 Vanadium mg / l V ≤0,05 06/03 Antimony mg / l Sb ≤0,002 No. name quality index unit the concentration concentration limits
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average the highest lowest class I class II class III class IV class V 06/03 Fluoride mg / l F ≤1,5 03/06 Beryllium mg / l Be ≤0,0008 03/06 Cobalt mg / l Co ≤0,05 chemical status concentration concentration limits No. name quality index unit average max average max allowed 4.1.1 alachlor mg / l 0.3 0.7 4.1.2 Anthracen mg / l 0.1 0.4 4.1.3 atrazine mg / l 0.6 2 4.1.4 Benzene mg / l 8 50 4.1.5 brominated diphenyl mg / l 0.0002 4.1.6 Cadmium and its mg / l 0.2 depending on the hardness of ≤0,05 4.1.7 C10 ‐ 13 ‐chloroalkany mg / l 0.4 1.4 4.1.8 Chlorofenwifos mg / l 0.1 0.3 4.1.9 chlorpyrifos mg / l 0.03 0.1 4.1.10 1,2‐dichloroethane (EDC) mg / l 10 4.1.11 dichloromethane mg / l 20 Phthalate, di (2‐ 4.1.12 mg / l 1.3 ethylhexyl) 4.1.13 diuron mg / l 0.2 1.8 4.1.14 endosulfan mg / l 0.0005 0,004 4.1.15 fluoranthene mg / l 0.1 1 4.1.16 Hexachlorobenzene (HCB) mg / l 0.01 0.05 4.1.17 Hexachlorobutadiene (HCBD) mg / l 0.1 0.6 No. name quality index unit concentration concentration limits
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
average max average max allowed 4.1.18 Hexachlorocyclohexane (HCH) mg / l 0,002 0.02 4.1.19 isoproturon mg / l 0.3 1.0 4.1.20 Lead and lead compounds mg / l 7.2 4.1.21 Mercury and its mg / l 0.05 0.07 4.1.22 Naphthalemg / l 1.2 4.1.23 Nickel and its compounds mg / l 20 4.1.24 nonylphenols mg / l 0.3 2 4.1.25 octylphenol mg / l 0.01 4.1.26 pentachlorobenzene mg / l 0.0007 4.1.27 Pentachlorophenol (PCP) mg / l 0.4 1 4.1.28 Benzo (a) pyrene mg / l 0.05 0.1 4.1.28b Benzo (b) fluoranthene mg / l 4.1.28c Benzo (k) fluoranthene mg / l Sum 0.03 4.1.28d Benzo (g, h, i) perylene mg / l 4.1.28 Indeno (1,2,3‐cd) pyrene mg / l Sum 0,002 01/04/2 simazine mg / l 1 4 4.1.30 tributyltin compounds mg / l 0.0002 0.0015 4.1.31 Trichlorobenzene (TCB) mg / l 0.4 4.1.32 trichloromethane mg / l 2.5 04/01/3 trifluralin mg / l 0.03 4.2.1 tetrachloromethane mg / l 12
No. name quality index unit concentration limits
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average max allowed 4.2.2 Aldrin mg / l 4.2.3 dieldrin mg / l 4.2.4 Endrin mg / l 4.2.5 isodrin mg / l Sum 0.005 4.2.6 DDT ‐ para‐isomer para mg / l 0.01 4.2.6b DDT total mg / l 0,025 4.2.7 Trichlorethylene (TRI) mg / l 10 4.2.8 Tetrachlorethylene (PER) mg / l 10 *) On the basis of the 2011. ‐ position: C, F, B2, JWW and 2012. ‐ position: E, H, SWR; **) on the basis of the 2011. ‐ position: C, H, F, B2, JWW.
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
4.1.4.3. Measles JCWP from Párnica to the mouth.
Measles state JCWP from Párnica to the mouth in 2012. Skwalifikowany was as bad [72]. His assessment was conducted by the Regional Inspectorate of Environment Protection (WIOŚ) in Szczecin, according to the Regulation of the Minister of the Environment of 9 November 2011. On the classification of surface water bodies and environmental quality standards for priority substances on the basis of the results of research conducted on three measuring stations (Fig. 12):
Measles Zachodnia‐ base UMS (Szczecin) ‐ hereinafter referred to as OP1, Western Odra ‐ Long Bridge (Szczecin) ‐ hereinafter referred to as OP2 Oder ‐ estuary to Glen Oder (Police) ‐ hereinafter referred to as OP3.
In accordance with the above. Regulation ‐ as with the current Regulation of the Minister of Environment of 22 October 2014. ‐ in the case of surface water bodies, such as JCWP Odra from Párnica to the mouth (ie. the river designated as heavily modified) indicators of water quality serving the classification of ecological potential are :
in terms of biological elements: phytoplankton (index fitoplanktonowy ifpla) macrophytes (makrofitowy index river) benthic macroinvertebrates (only element taken into account in the assessment under the Regulation of the Minister of Environment of 22 October 2014. ‐ indicator wielometryczny MMI_PL) fish fauna (only element taken into account in the assessment under the Regulation of the Minister of Environment of 22 October 2014. ‐ indicator IBI);
on the elements hydromorphological: with respect to the hydrologic regime: the number and growth of water flow connection to the groundwater. with regard to the continuity: the number and type of barriers, to ensure a transition to aquatic organisms, in relation to the morphological conditions: river depth and width variation, the structure and the channel substrate, the structure of the coastal zone, the rate of power;
in terms of physicochemical elements: as indices characterizing the physical state of the water temperature, total suspension. as indices characterizing the oxygen and organic contaminants: dissolved oxygen, five‐
day biochemical oxygen demand BOD5, Chemical oxygen demand COD‐Mn, total organic carbon, the chemical oxygen demand COD Cr‐
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as indices characterizing salinity conductivity at 20 ° C, sulfates, chlorides, calcium, magnesium, total hardness, as indices characterizing the acidity: pH, total alkalinity, as indicators characterizing the nutrients: nitrogen, ammonium, Kjeldahl nitrogen, nitrate nitrogen, total nitrogen, phosphate, total phosphorus, as especially harmful to the aquatic environment (specific impurities synthetic and non-synthetic) formaldehyde, arsenic, barium, boron, chromium, hexavalent chromium general, zinc, copper, phenols, volatile (phenol index), hydrocarbons of petroleum (index mineral oil), aluminum , free cyanides, cyanide-related, molybdenum, selenium, silver, thallium, titanium, vanadium, antimony, fluoride, beryllium, cobalt, tin.
Made in 2012. Phytoplankton and macrozoobenthos studies have shown that the biological elements are respectively II and class IV water quality. While other biological elements, ie. Macrophytes and fish species were not tested. On this basis, the potential ecological JCWP Odra from Párnica to the mouth in the field of biological elements was regarded as weak.
In accordance with the principle that a body of water, not assigned on the basis of reviewing the terms hydromorphological as artificial or modified is suitable in the range of hydromorphological elements class I, whereas the body of water designated as artificial or modified class II ecological potential JCWP Measles from Párnica to the mouth of hydromorphological elements range was assessed as good.
Ecological potential JCWP Odra from Párnica to the mouth in terms of physico‐chemical elements has been assessed as good. Such an evaluation water potential decided the results of the chemical oxygen demand COD‐Mn, Kjeldahl nitrogen and alkalinity.
Based on the above. findings ecological potential JCWP Odra from Párnica to the mouth was assessed as weak [71, 79].
JCWP chemical status was regarded as less than good. It decided to exceed the environmental quality standards established for tributyltin compounds.
The latest available results of water JCWP Odra from Párnica to the mouth relate to 2013. And comes from the position of Western Odra ‐ Base SUM (PO1). They do not change the previous assessment that JCWP.
Test results of water quality of the Oder in the years 2012 and 2013 are presented in tab.15, specifying limits for individual indicators in accordance with the Regulation of the Minister of the Environment of 22 October 2014. On the classification of surface water bodies and environmental quality standards for substances priority.
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Table 15. Measles JCWP test results from Párnica to the mouth in 2013. And 2012. (Source: [71], [79]).
average concentration for concentration limits No. name quality index unit OP1 OP2 OP3 class I class II class III class IV class V ecological potential Phytoplankton ‐ pointer 1.1 0.82 0.74 * 0.75 * ≥0,8 ≥0,6 ≥0,4 ≥0,2 <0.2 fitoplanktonowy
Macrophytes ‐ 1.4 ≥44,7 ≥36,5 ≥28,2 ≥20,0 <20.0 makrofitowy index River
benthic macroinvertebrates 1.5 ‐ an indicator wielometryczny 0.356 * ≥0,903 ≥0,717 ≥0,478 ≥0,239 <0.239 MMI_PL 1.6 Ichthyofauna ‐ pointer IBI ≥0,883 ≥0,750 ≥0,600 ≥0,400 <0.400 3.1.1 Temperature ° C 14.5 11.7 * 11.8 * ≤22 ≤24 3.1.5 total suspension mg / l 9.02 * ≤25 ≤50
3.2.1 Dissolved oxygen above the mg / l O2 9.2 8.2 * 9.6 * ≥7 ≥5 bottom The five‐day biochemical 3.2.2 mg / l O2 2.6 2.3 * 2.3 * ≤3 ≤6 oxygen demand (BOD5) Chemical oxygen demand COD‐ 3.2.3 Mn (index permanganic) mg / l O2 6,825 * ≤6 ≤12
The total organic carbon (TOC) 3.2.4 mg / l C 9.1 9.4 * 8.9 * ≤10 ≤15
Chemical oxygen demand COD‐ 3.2.6 mg / l O ≤25 ≤30 Cr 2 3.3.2 Conductivity at 20°C S / cm 662 727 * 729 * ≤1000 ≤1500 70
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
average concentration for concentration limits No. name quality index unit OP1 OP2 OP3 class I class II class III class IV class V
3.3.4 Sulfur mg / l SO4 74.6 * ≤150 ≤250 3.3.5 chloride mg / l Cl 107.4 * ≤200 ≤300 3.3.6 Calcium mg / l Ca ≤100 ≤200 3.3.7 Magnesium mg / l Mg ≤50 ≤100 3.3.8 total hardness mg / l 226 220 * 223 * ≤300 ≤500 3.4.1 PH pH 7.7‐8.2 7,2‐8,6 * 7,4‐8,6 * 6‐8.5 6‐9 3.4.2 total alkalinity mg 153.8 * ≤150 ≤250 3.5.1 ammonium mg / l N‐ 0.15 0.22 * 0.16 * ≤0,78 ≤1,56 3.5.2 Kjeldahl nitrogen (Norg + N‐ mg / l N 1.19 1.46 * 1.29 * ≤1 ≤2 3.5.3 nitrate nitrogen mg / l N‐ 1.77 1.35 * 1.32 * ≤2,2 ≤5 3.5.5 total nitrogen mg / l N 2.97 2.84 * 2.63 * ≤5 ≤10
3.5.6 phosphates mg / l P‐PO4 0.133 0.18 * 0.19 * ≤0,2 ≤0,31 3.5.7 total phosphorus mg / l P 0.178 0.16 * 0.15 * <0.2 <0.4 3.6.1 formaldehyde mg / l ≤0,05 3.6.2 Arsenic mg / l As ≤0,05 3.6.3 Bar mg / l Ba ≤0,5 3.6.4 Boron mg / l Ba ≤2 3.6.5 chrome 6 mg / l Cr ≤0,02 3.6.6 Chrome overall Reg. mg / l Cr ≤0,05 3.6.7 Zinc mg / l Zn 0.003 ≤1 3.6.8 Copper mg / l Cu 0.003 ≤0,05 3.6.9 phenol index mg / l 0.0007 * ≤0,01 3.6.10 index oil mg / l ≤0,2 3.6.11 Aluminum mg / l Al 0,002 * ≤0,4 3.6.12 cyanide free mg / l CN ≤0,05 80
The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
average concentration for concentration limits No. name quality index unit OP1 OP2 OP3 class I class II class III class IV class V mg / l 3.6.13 cyanide‐related ≤0,05 Me 3.6.14 molybdenum mg / l Mo ≤0,04 03/06 Selenium mg / l Se ≤0,02 3.6.16 Silver mg / l Ag ≤0,005 03/06 Thallium mg / l T ≤0,002 3.6.18 Titanium mg / l Ti ≤0,05 06/03 Vanadium mg / l V ≤0,05 06/03 Antimony mg / l Sb ≤0,002 06/03 Fluoride mg / l F ≤1,5 03/06 Beryllium mg / l Be ≤0,0008 03/06 Cobalt mg / l Co ≤0,05 chemical status concentration concentration limits No. name quality index unit year average max average max allowed 4.1.1 alachlor mg / l 2012 <0.005 <0.005 0.3 0.7 4.1.2 Anthracene mg / l 2012 0.0005 0.00063 0.1 0.4 4.1.3 atrazine mg / l 2012 <0.055 <0.055 0.6 2 4.1.4 Benzene mg / l 2012 <0.5 <0.5 10 50 4.1.5 brominated diphenyl mg / l 2012 0.00048 0.0005 depending on the depending on the 4.1.6 Cadmium and its mg / l 2013 0.0225 0.0258 hardness of hardness of compounds ** 4.1.7 C10 ‐ 13 ‐chloroalkany mg / l 2012 <0.05 <0.05 0.4 1.4 4.1.8 Chlorofenwifos mg / l 2012 <0.005 <0.005 0.1 0.3 4.1.9 chlorpyrifos mg / l 2012 <0.005 <0.005 0.03 0.1
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concentration concentration limits No. name quality index unit year average max average max allowed 4.1.10 1,2‐dichloroethane (EDC) mg / l 2012 0,625 10 4.1.11 dichloromethane mg / l 2012 0,625 20 Phthalate, di (2‐ 4.1.12 mg / l 2012 <0.15 1.3 ethylhexyl) 4.1.13 diuron mg / l 2012 <0.02 <0.02 0.2 1.8 4.1.14 endosulfan mg / l 2012 0 0 0.005 0.01 4.1.15 fluoranthene mg / l 2012 0.0047 0.0085 0.1 1 4.1.16 Hexachlorobenzene (HCB) mg / l 2012 <0.0005 <0.0005 0.01 0.05 4.1.17 Hexachlorobutadiene (HCBD) mg / l 2012 <0.015 <0.015 0.1 0.6 4.1.18 Hexachlorocyclohexane (HCH) mg / l 2012 0 0 0.02 0.04 4.1.19 isoproturon mg / l 2012 <0.015 <0.015 0.3 1.0 4.1.20 Lead and lead compounds mg / l 2013 <0.5 7.2 4.1.21 Mercury and its mg / l 2013 0,009 0,018 0.05 0.07 4.1.22 Naphthalene mg / l 2012 <0.0435 2.4 4.1.23 Nickel and its compounds mg / l 2013 2.0 20 4.1.24 nonylphenols mg / l 2012 <0.0005 <0.0005 0.3 2 4.1.25 octylphenol mg / l 2012 0.0020 0.1 4.1.26 pentachlorobenzene mg / l 2012 <0.0001 0,007 4.1.27 Pentachlorophenol (PCP) mg / l 2012 <0.025 <0.025 0.4 1 4.1.28 Benzo (a) pyrene mg / l 2012 0.0015 0.0030 0.05 0.1 4.1.28b Benzo (b) fluoranthene mg / l 4.1.28c Benzo (k) fluoranthene mg / l Sum 2012 0.0017 0.03
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concentration concentration limits No. name quality index unit year average max average max allowed 4.1.28d Benzo (g, h, i) perylene mg / l 4.1.28 Indeno (1,2,3‐cd) pyrene mg / l Sum 2012 0.0014 0,002 01/04/2 simazine mg / l 2012 <0.015 <0.015 1 4 4.1.30 tributyltin compounds mg / l 2012 0.0013 0.00458 0.0002 0.0015 4.1.31 Trichlorobenzene (TCB) mg / l 2012 0 0.4 4.1.32 trichloromethane mg / l 2012 0.34 2.5 04/01/3 trifluralin mg / l 2012 <0.0005 0.03 4.2.1 tetrachloromethane mg / l 2012 0.28 12 4.2.2 Aldrin mg / l 4.2.3 dieldrin mg / l 4.2.4 Endrin mg / l 4.2.5 isodrin mg / l Sum 2012 0 0,010 4.2.6 DDT ‐ para‐isomer para mg / l 2012 <0.0005 0.01 4.2.6b DDT total mg / l 2012 0 0,025 4.2.7 Trichlorethylene (TRI) mg / l 2012 <0.15 10 4.2.8 Tetrachlorethylene (PER) mg / l 2012 <0.11 10 *) On the basis of the 2012.
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4.2. STAGE II.
4.2.1. Identification of the factors of the Project on water quality elements.
As agents of the Project and related projects that may affect the elements of the water quality of surface water bodies Świna estuary, Szczecin Lagoon, Odra from Párnica to the mouth should be noted:
widening and deepening of the fairway and associated turntables and passing places; Conducting dredging work in order to achieve the required parameters associated with the issuance of the water column: mineral fine particle fraction (silt and clay), and vegetable detritus resulting from the dredging work technologies. nutrients, inorganic and organic micro‐pollutants accumulated in the surface layer of the bottom sediment. with a consequent decrease in the transparency of water, and a possible increase in the concentration of the above‐mentioned water. substances and micropollutants. Some of these micro‐substances is considered to be particularly harmful to the aquatic environment ‐ are taken into account in the assessment of the state / potential ecological JCWP part ‐ priority substances, which are for assessing status. During dredging works following the destruction of habitats and aquatic organisms in the bottom zone, as well as on certain sections of offshore.
construction of wharfs and revetments or bottom; Construction of embankments and revetments and bottom connected with the violation of the periodic structure of the bottom and banks and their caps and excitation of bottom sediments. It relates primarily to aquatic organisms, including groups of organisms that are the objects of research the biological quality elements for the assessment of state / ecological potential. It causes a periodic silting and water column habitat disturbance and destruction of these organisms at the time the investment species living in the coastal zone and the bottom.
storage / deposition of dredging spoil; Construction of the island is a local change of shape and structure of the seabed and its coverage. It relates primarily to aquatic organisms, including groups of organisms that are the objects of research the biological quality elements for the assessment of state / ecological potential. It causes a destruction of the habitat of these organisms, periodic silting and destruction of the water column during the investment species living in the area of the bottom. Backfilling of the dredged material
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deepening existing local trims Channel Mielińskim Piast and involve a periodic decrease in the number of macrozoobenthos in these places.
Project implementation and related projects will result in the emergence of the fairway ships of larger size, and in the long term, more ships than at present. This factor must therefore also be taken into account in the analyzes of the impact of the Program on water quality indicators representing the state of ecological and chemical JCWP identified.
Analysis of the scope of the Project and related projects did not identify factors that could affect the quantitative status and the chemical status of groundwater bodies.
4.2.2. Determining the list of indicators of water quality being potentially influenced by factors identified impacts of the Project.
Listed in Sec. 3.2.1 Project impact factors related projects may have an impact on the following indicators of the quality of surface water:
in terms of biological elements: macroalgae and angiosperms (macrophytes) benthic macroinvertebrates, fish fauna.
Remaining indicator of water quality in this area, ie. The phytoplankton was not subject to further assessment. Identified factors of the Program do not change the parameters for abiotic to which the indicator is associated (temperature and salinity) or cause only temporary changes in these parameters (nutrient content).
on the elements hydromorphological: For listed in the Regulation of the Minister of the Environment of 22 October 2014. on the classification of surface water bodies and environmental quality standards for priority substances indicators of water quality in terms of hydromorphological elements not specified still existing methodologies of determining them. In the case of transitional Regulation contains only records that in the limit of the first class of water quality is assumed "freshwater flow system" and "Depth variation, substrate conditions and the terms and condition of the intertidal zones correspond totally undisturbed conditions or close to these conditions," and for other classes limits not determined.
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While for heavily modified river water it formulated the following requirements for the class limit and ecological potential: the size and dynamics of movement and the resulting connection of underground water corresponding only to interactions that determined the recognition JCWP for heavily modified, continuity JCWP corresponding only to those interactions, which decided to declare it heavily modified, after taking all protective measures, to ensure "the best approximation to ecological continuum, in particular with respect to migration of fauna and appropriate spawning and breeding grounds" forms a trough, the depth and width variation, the flow rate conditions and the conditions of the substrate and the structure corresponding only to the coastal zones of the interactions that have determined the recognition JCWP for heavily modified. Limits for other classes has not been established.
With this in mind, it was decided that later in this report will be carried out analysis and impact assessment identified factors impact of the project in relation to all the indicators mentioned in the regulation.
in terms of physicochemical elements: transparency, nutrients, substances that are particularly harmful to the aquatic environment.
in relation to the chemical status: priority substances and other pollutants listed in Annex 9 to the Regulation of the Minister of the Environment of 9 November 2011. on the classification of surface water bodies and environmental quality standards for priority substances.
4.2.3. Evaluation of the impact of the Project on selected indicators of water quality.
4.2.3.1. Biological elements.
Macroalgae and angiosperms (macrophytes) Thallophyta macroalgae and angiosperms Angiospermae ‐ called macrophytes ‐ are benthic flora waters both inland and coastal and transitional. Macrophytes development depends on the physical and chemical conditions in the water (temperature, salinity, transparency, concentration of nutrients) and bottom sediments (soil type, pH, redox conditions, nutrient content).
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Macrophytes respond to the following types of pressures: changing the nutrient supply loads and concentration suspensions, and changing the structure of the edge of the bottom and the physicochemical conditions of bottom sediments.
JCWP Estuary Świna. Under JCWP Świna Estuary is planned to deepen the existing fairway to a depth of 14.5 meters. Currently, the depth of the technical section of the track is 14.3 m. The dredging work ‐ carried out in the framework of the statutory tasks of the Maritime Office in Szczecin ‐ will not go beyond the scope of the track and thus they do not endanger the optionally present in the vicinity of macrophytes.
JCWP Szczecin Lagoon. Vegetation Szczecin Lagoon is concentrated in the coastal zone (littoral) and in the shallows. The project does not interfere in these areas. Dredging work will only affect the existing fairway. However, in areas where the planned location of artificial islands ‐ constructed in dredge spoil originating from the deepening seaway ‐ there was no occurrence of any plant species [26]. The factors that prevent the development of macrophytes in these areas are most likely too large reservoir depth, limited availability of light, strong heave, poor water transparency). The resulting island will help over time to improve the ecological potential JCWP Szczecin Lagoon, among others, macrophytes in the field ‐ they will be colonized by vegetation, rushes, and in the coastal zone will start to grow vegetation and sea.
Bodied ‐ within the accompanying investments ‐ new quays fragment Świny the edge of only approx. 0.16% of the length of the coastline JCWP Szczecin Bay, and is highly urbanized areas.
This entitles you to determine that the project will have no negative impact on the ecological potential JCWP Szczecin Lagoon in the range of macrophytes, and in the longer term, may even contribute to its improvement in this regard.
Measles JCWP from Párnica to the mouth. According to the information in zawartyni [26] species diversity of macrophytes waters covered by the project is small. The plants are concentrated only in the coastal zone. In the trough, due to the presence of the fairway, macrophytes are absent. The most common species is listed common reed, forming larger or smaller patches. Relatively frequently observed species is also yellow water lily, growing in the accumulation of organic matter and sheltered ‐ where slightly indented coastline forms small bays. Other macrophytes are single, without creating their own communities. Pleustofity prevail ‐ free‐floating in the water or on the surface ‐ the ryzofitami, water plants which are rooted in the base [26].
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In [26] presents the state of macrophytes in the areas of interference Project peripheral zone JCWP Measles from Párnica to the mouth and the possible effects of this interference as a loss positions. In the absence of the State Environmental Monitoring Research, responsible for the assessment of water status, it is difficult to estimate to what extent these losses can have a negative impact on the ecological potential JCWP as a whole in terms of macrophytes. Whereas, however, contained in [26] statement that the said loss or patches of vegetation positions should not reduce biodiversity area adjacent to the project sites interference in the peripheral zone and taking into account that the above. space ‐ understood to be strengthened or built over the edges of quays fragments ‐ are only approx.
Benthic macroinvertebrates. Benthic macroinvertebrates (Macrozoobenthos) are the fraction of organisms inhabiting the surface of bottom sediments (epifauna) or inside (infauna), which remains after washing on a sieve with a mesh opening of 1.0 mm.
Most species macrozoobenthos prefer doped organic material which is a food base necessary for their development. Too high a content of organic matter in the sludge ‐ caused by excessive eutrophication ‐ is, however, degradation of these organisms.
In the conditions of the waters undisturbed współdominuje usually several or even a dozen species of macrozoobenthos. As the water pollution, the number of dominant species decreases, the proportion of the susceptible species ‐ a narrow tolerance range of organic ‐ is reduced and the tolerance of species increases. In extreme cases, the only species are the most resistant ‐ opportunistic [30].
Macrozoobenthos an important food base for fish, in particular from the group bentofagów. It may also be complementary to food base for diving birds, such as ducks or necked as well as other species such as gulls and terns.
JCWP Estuary Świna. Included in [39] Mouth description macrozoobenthos JCWP Świny in the project area has been prepared include on the basis of the results of studies of bottom sediments of the three selected reference points (SW2, SW3, SW4) Long‐Term Program for Maintenance of marine waterways in the area of the mouth of the Oder River in the years 2014 ÷ 2026 (hereinafter referred to as a program offshore maintenance of roads). The location of these points is shown in Fig. 13, and set points for the mean density of macrozoobenthos taxa identified and its average biomass is summarized respectively in tab.16a and 16b. Analysis of these tables shows that most often the highest density
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The impact assessment of the project entitled. "Modernization of Swinoujscie‐Szczecin to a depth of 12.5 m" on water resources
Project achieved in the area of worms, mainly due to the occurrence of Pygospio elegans and Marenzelleria neglecta. And the highest biomass formed shellfish, in particular Mya arenaria.
This is also confirmed research done in 2012. By the Regional Inspectorate for Environmental Protection in Szczecin on two positions: SW IV (figure 13). Test results macrozoobenthos in samples of sediment collected in these positions, presented in tab.15 and 16. Analysis of these tables show that the state of the macrozoobenthos JCWP can be considered weak.
Under JCWP Świna Estuary is planned to deepen the existing fairway to a depth of 14.5 meters. Currently, the depth of the technical section of the track is 14.3 m. Dredging works ‐ which will be made in the framework of the statutory tasks of the Maritime Office in Szczecin ‐ due to their scope should be regarded as podczyszczeniowe maintenance work. They will not have a material impact on the ecological potential JCWP Mouth Świna in terms of macrozoobenthos.
Table 16a. The average number of reference points in macrozoobenthos maintenance program sea roads located in Oder Bay (from [39]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans 1395 18,750 Marenzelleria viridis 1278 17.180 Hediste diversicolor 781 10,500 Bivalvia Mya arenaria 1159 15,580 Cerastoderma glaucum 302 4,060 Mytilus edulis 286 3.840 Macoma balthica 178 2.390 Gastropod Hydrobia sp. 270 3,630 crustacea Balanus improvisus 1132 15.210 Corophium volutator 585 7.860 Gammarus sp. 38 0.510 Cyanthura carinata 14 0.190 Crangon crangon 2 0.030 Oligochaeta 20 0.270 SUM: 7440 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 69.02 Intermediate 23.00
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Fig. 13. The test points macrozoobenthos in the Szczecin Lagoon and the Pomeranian Bay (Development based on: [21]). 90
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Table 16b. The average biomass macrozoobenthos reference points in the maintenance program sea roads located in Oder Bay (from [39]).
taxon biomass [g / m2] % POLYCHAETA Pyrogospio elegans 0.7 0.62 Marenzelleria viridis 0.2 0.18 Hediste diversicolor 0.2 0.18 Bivalvia Mya arenaria 70.0 62.39 Cerastoderma glaucum 18.7 16.66 Mytilus edulis 12.6 11.23 Macoma balthica 6.1 5.44 Gastropod Hydrobia sp. 0.1 0.09 crustacea Balanus improvisus 2.6 2.32 Corophium volutator 0.7 0.62 Gammarus sp. 0.1 0.09 Cyanthura carinata 0.1 0.09 Crangon crangon 0.1 0.09 Oligochaeta 0.00 SUM: 112.2 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 71.22 Intermediate 17.37
Table 15. The size and position on the assessment of macrozoobenthos in 2012 SW. (Based on [71])
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor 386 4.71 Oligochaeta 84 1.02 INSECTA Chironomidae 8 0.10 crustacea Heterotanais oerstedi Cyanthura carinata 18 0.22 Gammarus
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taxon number [individuals / m2] % Corophium volutator 3774 46.02 Gastropod valvata piscinalis Potamopyrgus antipodarum Hydrobidae 1732 21.12 Bivalvia Dreissena polymorpha Macoma balthica 1658 20.22 Mya arenaria 540 6.59 SUM: 8200 100.00 B index (Cl) 2.38 (Class IV) 1 ‐ tolerant 2 ‐ 3 ‐ sensitive 78.66 Intermediate 0.22
Table 16. The size and position on the assessment of macrozoobenthos in 2012 SW. (Based on [71])
taxon number [individuals / m2]] % POLYCHAETA Pyrogospio elegans 70 1.10 Hediste diversicolor 394 6.22 Oligochaeta 88 1.39 INSECTA Chironomidae 2 0.03 crustacea Heterotanais oerstedi Cyanthura carinata 12 0.19 Gammarus 2 0.03 Corophium volutator 3744 59.09 Gastropod valvata piscinalis Potamopyrgus antipodarum Hydrobidae 64 1.01 Bivalvia Dreissena polymorpha Macoma balthica 86 1.36 Mya arenaria 1874 29.58 SUM: 6336 100.00 B index (Cl) 2.01 (Class IV) 1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 97.67 1.04 1.29
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JCWP Szczecin Lagoon Included in [39] Description of macrozoobenthos JCWP Szczecin Lagoon in the project area has been prepared include on the basis of the test results of bottom sediments of the four selected reference points (BT3, ME‐W, ST2, TW2) maintenance program sea roads. The location of these points is shown in figure 13, and set points for the mean density of macrozoobenthos taxa identified and its average biomass is summarized in Table respectively. 17a, and 17b. Analysis of these tables shows that the most common taxon in the area of the Project are the larvae of Chironomidae, while the main building the biomass is taxon Dreissena polymorpha.
Table 17a. The average number of reference points in macrozoobenthos maintenance program sea roads located in Szczecin Lagoon (from [39]).
taxon number [individuals / m2] % Oligochaeta Tubificidae 2094 52.53 Hirudinea 5 0.13 INSECTA Chironomidae 1395 35.00 Bivalvia Dreissena polymorpha 472 11.84 crustacea Gammarus 20 0.50 SUM: 3986 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 87.66 Intermediate 0.00
Table 17b. The average biomass macrozoobenthos reference points in the maintenance program sea roads located in Szczecin Lagoon (from [39]).
taxon biomass [g / m2] % Oligochaeta Tubificidae 7 8.33 Hirudinea 0.0005 0.00 INSECTA Chironomidae 14 16.67 Bivalvia Dreissena polymorpha 63 75.00 93
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taxon biomass [g / m2] % crustacea Gammarus 0.004 0.00 SUM: 84 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 25.00 Intermediate 0.00
As part of the natural inventory carried out for the report on the impact of the project on the environment [26] were made research macrozoobenthos in places where it is planned execution of the islands of ore coming from dredging the fairway ‐ position: W22, W27 and W28 (Fig. 13). Attempts bottom sediments collected by the catcher Van Veen in the period from 18 to 21 October 2014.
In the tests, the presence of species characteristic of the muddy bottom of the Szczecin Lagoon and the dominant skąposzczetów and larvae Chironomidae (Tab. 18 to 20). Only the station W27 experienced individuals Dreissena polymorpha, with mean density osobn./m2 90 and the biomass 10.8 g / m2 (Tab. 19a and Tab. 19b.). In the areas intended islands was not detected sensitive or valuable species of invertebrates. The sampling areas bottom is muddy, prevailing poor oxygen conditions, which can be inferred from the nature of the solid and the odor originating from the decomposition of organic material [26].
Table 18a. The number of macrozoobenthos the position of W22 (from [26]).
taxon number [individuals / m2] % Oligochaeta Tubificidae 5670 71.59 INSECTA Chironomidae 2250 28.41 Bivalvia Dreissena polymorpha 0 0.00 SUM: 7920 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 100.00 Intermediate 0.00
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Table 18b. Biomass macrozoobenthos the position of W22 (from [26]).
taxon biomass [g / % Oligochaeta Tubificidae 18.49 53.70 INSECTA Chironomidae 15.94 46.30 Bivalvia Dreissena polymorpha 0 0.00 SUM: 34.43 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 100.00 Intermediate 0.00
Table 19a. The number of macrozoobenthos the position of W27 (from [26]).
taxon number [individuals / m2] % Oligochaeta Tubificidae 7416 48.53 INSECTA Chironomidae 7776 50.88 Bivalvia Dreissena polymorpha 90 0.59 SUM: 15282 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 99.41 Intermediate 0.00
Table 19b. Biomass macrozoobenthos the position of W27 (from [26]).
taxon biomass [g / % Oligochaeta Tubificidae 36.94 30.33 INSECTA Chironomidae 74.05 60.80 Bivalvia Dreissena polymorpha 10.8 8.87 SUM: 121.79 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 91.13 Intermediate 0.00
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Table 20a. The number of macrozoobenthos the position of W28 (from [26]).
taxon number [individuals / m2] % Oligochaeta Tubificidae 2286 68.28 INSECTA Chironomidae 1062 31.72 Bivalvia Dreissena polymorpha 0 0.00 SUM: 3348 100.00
1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 100.00 0.00 0.00
Table 20b. Biomass macrozoobenthos the position of W27 (from [26]).
taxon biomass [g / % Oligochaeta Tubificidae 6.81 53.12 INSECTA Chironomidae 6.01 46.88 Bivalvia Dreissena polymorpha 0 0.00 SUM: 12.82 100.00
1 ‐ tolerant 2 ‐ 3 ‐ sensitive 100.00 Intermediate 0.00
Ww. perceptions about poor taxonomically bottom makrofaunybezkręgowej Szczecin Lagoon is also confirmed by studies done in 2011 and 2012 by the Regional Inspectorate for Environmental Protection in Szczecin. Test results macrozoobenthos in samples of sediment collected at different positions WIOŚ were summarized in Table. 21 ÷ 27. Analysis of these results indicates that only the position E located in the vicinity of the island Chelminek macrozoobenthos state can be considered moderate, while in all other positions he is weak at best.
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Table 21. Assessment of macrozoobenthos abundance and the position C in 2011. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor Oligochaeta 12 42.86 INSECTA Chironomidae 16 57.14 crustacea Heterotanais oerstedi Cyanthura carinata Gammarus Corophium volutator Gastropod valvata piscinalis Potamopyrgus antipodarum Hydrobidae Bivalvia Dreissena polymorpha Macoma balthica Mya arenaria SUM: 28 100.00 B index (Cl) 1.17 (class V) 1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 100.00 0.00 0.00
Table 22. Assessment of macrozoobenthos abundance and the position E in 2012. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor Oligochaeta 562 2.78 INSECTA Chironomidae 242 1.20 crustacea Cyanthura carinata Gammarus 2674 13.23 Corophium volutator 11132 55.06 97
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taxon number [individuals / m2] % Gastropod valvata piscinalis 6 0.03 Potamopyrgus antipodarum 4 0.02 Hydrobidae 258 1.27 Bivalvia Dreissena polymorpha 5340 26.41 Macoma balthica Mya arenaria SUM: 20218 100.00 B index (Cl) 2.82 (Class III) 1 ‐ tolerant 2 ‐ 3 ‐ sensitive 59.04 Intermediate 0.03
Table 23. The size and position on the assessment of macrozoobenthos F in 2011. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor Oligochaeta 118 55.66 INSECTA Chironomidae 86 40.57 crustacea Heterotanais oerstedi Cyanthura carinata Gammarus Corophium volutator Gastropod valvata piscinalis 6 2.83 Potamopyrgus antipodarum Hydrobidae Bivalvia Dreissena polymorpha 2 0.94 Macoma balthica Mya arenaria SUM: 212 100.00 B index (Cl) 2.12 (Class IV) 1 ‐ tolerant 2 ‐ 3 ‐ sensitive 96.23 Intermediate 2.83
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Table 24. The size and position on the assessment of macrozoobenthos H in 2012. (Based on [71]).
taxon number [individuals / m2] % Oligochaeta 34 28.81 INSECTA Chironomidae 76 64.41 crustacea Gammarus 4 3.390 Gastropod Potamopyrgus antipodarum 2 1,695 Hydrobidae 2 1,695 SUM: 118 100.00 B index (Cl) 1.90 (class V) 1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 93.22 6.78 0.00
Table 25. The size and position on the assessment of macrozoobenthos SWR in 2012. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans 6 0.28 Hediste diversicolor 8 0.38 Oligochaeta 106 4.98 INSECTA Chironomidae 296 13.90 crustacea Cyanthura carinata 2 0.09 Gammarus 38 1.78 Corophium volutator 852 40.00 Gastropod Potamopyrgus antipodarum 0 0.00 Hydrobidae 2 0.09 Bivalvia Macoma balthica 816 38.31 Mya arenaria 4 0.19 SUM: 2130 100.00 B index (Cl) 2.00 (Class IV) 1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 97.76 1.87 0.37
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Table 26. Assessment of macrozoobenthos abundance and the position B2 in 2012. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor Oligochaeta 562 2.78 INSECTA Chironomidae 242 1.20 crustacea Heterotanais oerstedi 2 0.01 Cyanthura carinata Gammarus 2674 13.22 Corophium volutator 11132 55.05 Gastropod valvata piscinalis 6 0.03 Potamopyrgus antipodarum 4 0.02 Hydrobidae 258 1.28 Bivalvia Dreissena polymorpha 5340 26.41 Macoma balthica Mya arenaria SUM: 20220 100.00 B index (Cl) 1.74 (class V) 1 ‐ tolerant 2 ‐ Intermediate 3 ‐ sensitive 59.03 40.93 0.04
Table 27. The size and position on the assessment of macrozoobenthos JWW in 2011. (Based on [71]).
taxon number [individuals / m2] % POLYCHAETA Pyrogospio elegans Hediste diversicolor Oligochaeta 92 24.87 INSECTA Chironomidae 236 63.78 crustacea Heterotanais oerstedi Cyanthura carinata
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taxon number [individuals / m2] % Gammarus Corophium volutator Gastropod valvata piscinalis 40 10.81 Potamopyrgus antipodarum Hydrobidae 2 0.54 Bivalvia Dreissena polymorpha Macoma balthica Mya arenaria SUM: 370 100.00 B index (Cl) 2.59 (Class IV) 1 ‐ tolerant 2 ‐ 3 ‐ sensitive 88.65 Intermediate 10.81
Deepening or widening and deepening of the fairway cause physical removal of the layers of bottom sediments, with vs those found in the organisms, and then transferring it to a designated dumping site or other parts of the track in order to compensate for existing trims. This means that in places of work of dredging and spoil deposition macrozoobenthos periodically cease to exist. This impact will affect approx. 4.77 km2 JCWP Szczecin Bay surface [27, 39] which is 1.2% of its total area.
After completion of dredging work space deepened and widened fairway will gradually re‐ populated makrobezkręgowcami benthic by migration from areas adjacent (e.g. see .: Corophium, Gammarus, Oligochaeta, Gastropoda) or by deposition on the bottom of planktonic larvae (this Bivalvia and polychaetes) . Reappearance at these sites common in sediments Szczecin Bay larvae Chironomidae apparent from the course of the reproductive cycle of these organisms ‐ submitted by it on the water surface eggs drift, and then sink and sink to the bottom, where the hatch of larvae.
It should be emphasized that the process of the playback unit macrozoobenthos important is also the length of the life cycles different taxa. Organisms living several years (eg. The clams) are not able to reproduce rapidly in population structure that existed previously. This may result in a rapid increase in the number of these organisms in the area of in‐depth, but their slow playback biomass. In contrast, areas that are often exacerbated never be able to recreate the full structure of macrozoobenthos, characteristic for the area. In this case, the bottom is occupied by the benthos depleted structure organisms with short life cycle and high dispersion. Macrozoobenthos biomass in these areas will always be low. This is confirmed by the study,
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Odra in the years 2014‐2026 [10]. A good example in this regard is the reference point SW1, located in the estuary stretch Świna (Fig. 13), in the area where he regularly works are carried out dredging associated with the maintenance of the fairway ‐ these works were performed in 2012, 2013 and 2014. This station is characterized by the extremely low density makrozobentosu (315 os./m2) and its very low biomass (1.5 g / m2).
Dredging works related to the widening and deepening of existing tracks and should not cause a decrease in the number of species of macrozoobenthos species and changes in the share sensitive and resistant to stress caused by eutrophication. This is confirmed by, among others, the results of monitoring pre‐investment, investment and pro‐investment led to the task of construction of breakwater for the external port in Swinoujscie. [73] Positions covered by this monitoring, a year after the impact of the works that could have a significant impact on the structure of benthic disturbing, is still visible. For example, in one of these positions (position ZP 2, located near the above. Positions SW2 and SW3) were only approx. 50% of the biomass and abundance of mussels listed before the investment. In relation to the total biomass of macrozoobenthos qualitative similarity of dominant and subdominantów was 75%, and in terms of the size of only 28%. However, the rate of biodiversity Shannon‐Wiener determined for this position for a period of pre‐ and poinwestycjnego was almost identical to [39].
Storage of dredging spoil fairway as the corresponding island or islands filling means at certain places Szczecin Bay bottom sediments with living therein makrobezkręgowcami benthic, leading to their destruction. This interaction will apply to approx. 3.8 km2, which is less than 1.0% of the JCWP Szczecin Lagoon.
Establishment of the islands will mean the emergence of new littoral zones, which will be occupied by other species than was found in those places previously in the bottom mud. It is anticipated that it can produce a rush, submerged vegetation occur, as it did in the case of island Chelminek. Through the increase of various kinds of vegetation and habitat generate a mosaic to be harboring taxa macrozoobenthos more than a muddy bottom, therefore, increase the biodiversity of the assembly. It is difficult to predict whether we will have to deal with the increase in the density or biomass [39]. It is worth mentioning that the above‐cited studies in Szczecin WIOŚ clearly show
One of the effects of the creation of the islands will be the formation of new shoals Dreissena polymorpha. Mussel has a beneficial impact on the water as by filtration contributes to the reduction of blooms and turbidity of water, and by depositing agglutinates (filtered algae) and calcium carbonate gives good habitat for other invertebrates [39]. Dreissena polymorpha be colonized coastal islands with the greatest intensity from 0 to a depth of about 5 meters.
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Dredging work on the fairway and the discharge of excavated material will cause turbidity, most felt in the immediate vicinity of works. The range of the spread of this will depend on the turbidity existing at the time of the currents and wind power. Excess slurry may cause clogging of the filtration apparatus odfiltrowujących animal feed water. However, this problem affects mainly planktonic organisms that can not stop filtering, because it is associated with respiratory movements of legs, for example. Cladocerans. Most benthic filtratorów reacts to sudden changes in the environment closure shell, burying the houses like. They can thus safely survive transient turbidity or other deterioration [26]. It should also be emphasized, that in the Lagoon Szczecin, because of the shallowness and the undulation at the bottom of the water is usually heavily loaded suspension. Present in the basin organisms are therefore adapted to such conditions.
As a result of violations of bottom sediments may appear local changes in water chemistry, relating primarily to decrease the amount of oxygen, reduce the redox potential, or the release of toxic substances deposited in the sediment. These factors may lead to the elimination of some, particularly sensitive taxa of macrozoobenthos. However ‐ as shown by the test results presented above ‐ in the areas where work will be conducted dredging and discharge dredged materials dominate taxa more resistant to these factors (Tubificidae and Chironomidae larvae). They should not, therefore, suffer greatly in this respect.
Destruction of macrozoobenthos can also take place in the coastal zone in places of work or the bottom edges umocnieniowych and construction or reconstruction of quays. For JCWP Szczecin Bay such work will be performed on the bank a total length of approx. 2 km, and at the bottom of a total area of approx. 0.08 km2, which constitutes a small proportion of the peripheral surface of the or JCWP (0.6% and 0.02%).
Identified factors of the Project and related projects ‐ work dredging associated with the widening and deepening of the fairway, the deposition of excavated during these works excavated works umocnieniowe and expansion or construction of embankments ‐ can thus interfere with the existing structure of macrozoobenthos and slow down ‐ or even prevent ‐ its reconstruction to good potential. In order to assess whether and to what extent their impact is significant indicator of the impact are used WskWp used in [31] for the initial designation heavily modified transitional water (see rozdz.4.1.3.2). It was assumed that the growth depicted above. impact indicator JCWP morphological changes caused by the investment will result in the same ‐ calculated as% ‐ reduction in the multimeric index B,
Bearing in mind the judgment of the Court of Justice of the European Union on 1 July 2015 in Case C‐461/13 [61], it was assumed that:
in a situation where the reduction in value of a multimeric B index results in a change of classification status / potential macrozoobenthos, even if it does not translate into a change in the assessment of the overall
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JCWP state, is considered analyzed the investment has a significant negative impact on the state of macrozoobenthos and can cause deterioration JCWP;
in a situation when the state / potential macrozoobenthos monitoring positions located within the project impact is in the fifth grade classroom, any reduction of the multimeric B index is considered a significant impact on the state of macrozoobenthos investment is likely to cause deterioration of the JCWP.
It should be emphasized that according to Polish law for JCWP Szczecin Lagoon ‐ despite believing it to be heavily modified ‐ for macrozoobenthos apply the same limits as for the quality classes transitional waters not treated as significant morphological pressures.
In the case under consideration Project and accompanying investments it is estimated that the impact of the change indicator for JCWP Szczecin Lagoon will amount to 2.63% (see chap. 4.2.3.2). When determining the initial state ‐ corresponding to the measured in the years 2011 and 2012 the index values multimeric B ‐ were taken WskWp = 19.28, ie. The pre‐implementation phase II upgrade the fairway. According to previous assumptions, this means reduction of the multimeric index B for the respective positions of the monitoring also 2.63% (See Tab. 28).
Table 28. Estimated change in terms of water quality macrozoobenthos at different positions within the JCWP Szczecin Lagoon.
index value B position estimated after location position current the Project C 1.17 1.14 within investment E 2.82 2.75 within investment F 2.12 2.06 within investment H 1.90 1.85 within investment B2 1.74 1.69 within investment SWR 2.00 1.95 within investment beyond the reach of JWW 2.59 2.52 investments (Lake. average 2.05 2.00
With tab. 28 shows that the above. lowering the multimeric B index positions located within the monitoring of the Project and related projects will not result in the reclassification of water quality in terms of macrozoobenthos to the lower class.
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However, due to the fact that three of these positions macrozoobenthos is in the fifth grade classroom, it should be considered, the project has a significant negative impact on the ecological potential JCWP Szczecin Lagoon in the range of benthic macroinvertebrates.
Measles JCWP from Párnica to the mouth.
As part of the natural inventory carried out for the report on the impact of the project on the environment [26] were made studies of macrozoobenthos in the littoral zone of islands along the fairway between Szczecin‐Police (Mieleński Ostrow Mieleński, Ostrow Grabowski, Mieleńska Meadow, United Kepa, Radolin, Debina , Crane, Fish Ostrow, Kopin, Raduń, Long Ostrow, Karwa Great). 2 inspections were carried out: in the spring (16.05.2015 r.) And in summer (22 and 27.07. 2015.). According to [26], found as a result of the control taxa macrozoobenthos taxa were commonplace typical test section of a river. They occurred mosaic, depending on the ground of the site.
Inventory in the spring showed virtually no representatives macrozoobenthos [26]. The occurrence of individual animals merely shellfish succession amphipods (Amphipoda) belonging to the suborder kiełżowatych (gammaridea) representative bugs heteroptera (Hetroptera) species Nepa cinerea (NEPA cinerea) mszywioła cristatella mucedo. Mszywioł this occurred at the entrance to the Eagle Isthmus, in a sheltered by lodges and most likely came from the lake Dabie. The area covered by the drift zone inventory identified the presence of mussel (Bivalvia) from the family skójkowatych (Unionidae) of the species duck mussel (Anodonta anatina) painter's mussel (Unio pictorum) swollen river mussel (Unio tumidus). There was no presence of rare species or protected.
Inventory in the summer period demonstrated an increase in the number of macrozoobenthos and more taxa identified [26]. The smallest number of taxa characterized by medium sand, gravel and small stones ‐ were found in such places only single specimens and sharpened skójki painting, duck mussel, zebra mussel (Dreissena polymorpha) and single Gammaridae. In the case of hides in the form of cavities in the rim or the roots were found cancer zebrafish (Orconectes limosus). The presence of the plant to increase the number of affected Gammaridae, appeared crustaceans belonging to the genus Mysidacea. Most rich fauna characterized by the shores of islands Ostrow Mieleński and Property, where the vegetation was the richest littoral dominance with yellow water lily, osoki aloesowatej, pondweed crested. In the littoral of these islands found numerous: gammaridea, Mysidacea, Orconectes limosus., Anatina Anodonta, Unio pictorum, Unio tumidus, Dreissena polymorpha, viviparus viviparus, planorbarius corneus, Chironomidae larvae, Gerris sp. And a number of littoral cladocerans. There was no presence of rare species or protected. In July also found the presence of common species imagines dragonfly on the edges of the Oder: Ischnura elegans and Orthetrum cancellatum.
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When performing the inventory was seen very strong impact on the coastal zone of the islands of waves generated by a passing unit. Even the movement of waves coming close small units of about 2 meters deep into the beach and caused leaching of land. In turn, on the coast covered with common reed (Phragmites australis), the plants are strongly bent and performed very strong current of water, introducing strong disturbance in the environment. In May, in the littoral islands, there was no other outside reed submerged vegetation. However, in July in some places it appeared submerged vegetation represented mainly by stuckenia pectinata. With the advent of this type of vegetation has increased the size and number of taxa of macrozoobenthos ascertained.
There are no studies on macrozoobenthos Odra estuary. The nearest examined in this respect sections of the rivers Oder Eastern and Western Odra, which is located between Park Lower Oder Valley Landscape. Despite the proximity and abundance of macrozoobenthos in these sections is significantly different from that found for the section of the Oder River estuary. [26] This is due to the different nature of habitats occurring in these areas. Underlining requires that, after the Oder East and West are movable unit of multiple times the tonnage of less than immersion and seaway Swinoujscie‐Szczecin. Ripple caused by these units does not result in such large havoc in the coastal zone, as is the case for individuals with high tonnage moving the aforementioned. track in the Odra estuary. Nevertheless, even in the case of the Oder River in Eastern and Western bentofauna littoral it is poorer than that found at the bottom of the river bed [60].
Ww. This observation confirms the macrozoobenthos study done in 2012. by the Regional Inspectorate for Environmental Protection in Szczecin Senior Western Odra ‐ Base SUM (Stettin) (fig. 13). The results of these tests are presented in Table. 29.
Table 29. The size of the position macrozoobenthos WIOŚ (from [71]).
number taxon % [subjects / m2] NEMATOMORPHA Gordiidae 24 5.86 Bivalvia Dreissenidae 171 41.71 Sphaeriidae 4 0.98 Unionidae 1 0.24 Gastropod Valvatidae 1 0.24 POLYCHAETA Polychaeta 6 1.46
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number taxon % [subjects / m2] Amphipoda Gammaridae 100 24.39 Trichoptera Ecnomidae 2 0.49 Diptera Chironomidae 100 24.39 Ceratopogonidae 1 0.24 SUM: 410 100.00 ASPT 5.13 Log10 (Sel_EPTD + 1) 0 1‐GOLD 0.75 S 10 EPT 1 H ' 1.40 MMI_PL 0.356 quality class IV
In Poland, for the evaluation of water quality based on the status indicator macrozoobenthos used wielometryczny MMI_PL. It is a weighted average of the normalized values of the six metriksów used in biomonitoring hydrobiologicznym, ie .:
Averaged Water Quality Indicator (ASPT) ‐ quotient of BMWP‐E (ie, the sum of points assigned to the families of benthic invertebrates) and the number of bulleted families;
Log10 (Sel_EPTD 1) ‐ logarithm of the sum of the individuals in families with four rows: collar beams (Ephemeroptera), stoneflies (Plecoptera), Trichoptera (Trichoptera) and flies (Diptera), plus one; GOLD 1 ‐ 1 and the difference frequency gastropods (Gastropoda) skąposzczetów (Oligochaeta) and flies (Diptera); number of identified families; EPT number of families ‐ the number of families with three rows: mayflies (Ephemeroptera), stoneflies (Plecoptera) and Trichoptera (Trichoptera); Biodiversity index Shannon‐Wiener (H ').
Ww. macrozoobenthos evaluate metrics for:
structural changes in the taxonomy (number of identified families the number of families EPT index of diversity and Log 10 (Sel_EPTD 1); diversity bands (number of identified families diversity index);
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presence taxa sensitive pollution with organic compounds and biogenami (ASPT) and the hydro‐morphological changes (number of families EPT); uniformity of the occurrence of important functional groups (1‐GOLD).
WIOŚ test results indicate that the state of the macrozoobenthos JCWP Odra from Párnica to the mouth should be assessed as weak.
The enlargement (from 90 to 100 m) and deepening the existing fairway may delay or slow down the ‐ and even prevent ‐ the reconstruction of macrozoobenthos JCWP Odra from Párnica to the mouth of the potential good. Analyzes [26] it shows that the presence of this track ‐ in JCWP is a track section from km 44.000 to km 62,100 ‐ and its operation may be a major factor in determining the current weak ecological potential (class IV water quality) in terms of macrozoobenthos. It should be emphasized that according to Polish law for JCWP Odra from Párnica to the mouth ‐ despite believing it to be heavily modified ‐ for macrozoobenthos apply the same limit as second class quality for the river is not subjected to such a significant morphological pressures.
The factors that disrupt the existing structure makrozobentosu are also working umocnieniowe bottom and banks and building embankments. In the case of Measles JCWP from Párnica to the mouth, umocnieniowe work will be carried out only within the framework of the project ‐ the strengthening of embankments along the bottom of HUK, Nautical and BON on a total length of 0.26 km and an area of only 0.01 km2. However, in the framework of the investment associated with one of the existing wharves in the JCWP (Cereal on the peninsula Eve) has been extended by 35 meters. Other, mentioned in the table. 1, strengthen or bottom edges and the construction of wharves ‐ planned on the fairway from km 62.100 to km 67.424, Grabowski Canal and Port of Szczecin will be implemented outside the JCWP Odra from Párnica to the mouth. The planned investment in the Port Police concerns JCWP RSS Police. The above leads to the conclusion,
In order to estimate the extent of modernization influence on the state of the fairway macrozoobenthos can be important measure was used similar to that used in [31] for the initial designation heavily modified coastal waters transitional impact indicator WskWp (see chap. 4.1.3.1 and 4.1.3.2) .
It has been assumed that the effect of morphological changes caused JCWP upgrade path for Macrozoobenthos can be quantified using the impact indicator WskWT described by the following formula:
n LT WskWT (WskZn d) m (1) and LJCW
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where: n ‐ the number of kinds of morphological changes caused by the modernization of the fairway within JCWP evaluated. WskZn ‐ relevance indicator morphological changes d ‐ morphological changes expressed by the relative increase in the track surface AND AND m ) Or relative increase in the length L L (as m ) LT sections (as AT at which these changes occur,
LTm ‐ length of the track after modernization, is located within evaluated JCWP (In the case of Measles JCWP from Párnica to the mouth equal to 18.1 km) LJCW‐ the total length of watercourses important JCWP the evaluated (in the case of Measles JCWP from Párnica to the mouth equals 29.047 kilometers [32, 78]).
It was assumed that depicted above. indicator morphological changes due to the modernization JCWP fairway will result in the same ‐ calculated as% ‐ reduction in the rate wielometrycznego MMI_PL characterized condition / ecological potential in the range of JCWP macrozoobenthos. In the case where the reduction at the same time it means a reclassification to a lower class, it is considered that the planned modernization of the fairway has a significant impact on the current state of the macrozoobenthos. It was assumed that:
in a situation where the reduction in value of the index wielometrycznego MMI_PL results in a change of classification status / potential macrozoobenthos, even if it does not translate into a change in the assessment of the overall state of JCWP, is considered analyzed the investment has a significant negative impact on the state of macrozoobenthos and can cause deterioration JCWP;
in a situation when the state / potential for macrozoobenthos monitoring stations located within the project impact is in the fifth grade classroom, any reduction of the rate wielometrycznego MMI_PL recognized the important impact of the investment on the condition of macrozoobenthos likely to cause deterioration of the JCWP.
Inventoried in this volume morphological changes in the JCWP Odra from Párnica to the mouth are summarized in Table. 30. This table also corresponding to each change signification indices and the calculated impact indicators ‐ partial and total.
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Table 30. Morphological changes within the JCWP Measles from Párnica to the mouth resulting from the modernization of the fairway with the assessment of their impact on Macrozoobenthos.
relevance the impact of kind of change d changes changes in WskZn makrozobentos WskWT [%] Increasing the area aggravated fairway (extension of the existing track execution mijanki Police and 1 0.363 1.0 22.62 the approach portion to the Port Police)
Increasing the area exposed to the bottom 2 0.142 1.0 sediments violation (turntables)
3 New clips boundary (strengthening) 0.50 The calculation result of a change of resistance 22.62 bh[%]
With tab. 30 shows that in the case of the present project, the estimated JCWP Measles from Párnica to the mouth of the index value will be the effect WskWT 22.62%. According to this prior assumption will reduce the mean values of the position wielometrycznego MMI_PL water quality monitoring Measles ‐ Base SUM (Szczecin) also about 22.62%, ie. From 0.356 (IV quality class) to 0.275. This reduction will not result in the reclassification of water quality in terms of macrozoobenthos to the lower class. Thus it can be concluded that the project had no significant impact on the ecological potential JCWP Odra from Párnica to the mouth.
Fish fauna.
JCWP Estuary Świna. As part of the natural inventory carried out for the report on the impact of the project on the environment [26] in the spring and autumn of 2014. In the area JCWP Mouth Świna were made half of research along the transepts with a length of 1,500 meters set out on three positions: SW2, SW3, SW4 ( figure 14). Half of these were carried out using towed gear (bottom trawl).
The results of the study summarized in Table fish fauna. 31. The halves of the spring season recorded 14 species of fish, the autumn season ‐ 13, in both the total of 17 (Tab. 32). It has been found that the farther from the edge of the diversity of fish species is higher. In the spring it grew from 1.2 bit on the subject, przyujściowym Świna transect, the value of almost 2 bits per individual, in the northernmost transect SW4. In the autumn season rate of biodiversity in the Shannon‐Wiener transect SW4 far exceeded the value of 2.
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Table 31. The test results ichtyofauna Pomeranian Bay using bottom trawl catches (from [39]).
catching results SW2 SW3 SW4 number of identified species of spring season 5 7 6 autumn season 7 4 7 catch biomass [g] spring season 2570 2715 1570 autumn season 7070 145 2215 biodiversity index Shannon‐Wiener [bit / separately.] spring season 1.35 1.50 1.95 autumn season 1.65 1.95 2.30
Table 32. Fish species found in the Pomeranian Bay (based on [39]).
lp government family type 1 sprat* clupeiformes clupeid 2 Herring 3 osmeriformes smelts sparling 4 roach cypriniformes carp 5 white bream 6 łososiokształtne salmonids whitefish * 7 gadiformes WHITEFISH cod* 8 gobies goby 9 perch 10 percidae zander 11 perciformes jazgacz 12 tobiasz sandeel 13 tapping * 14 eelpout eelpout ** 15 flounder 16 Flatfish płastugowate plaice 17 turbot** *) Only in the spring season **) only in the autumn season
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Given that the modernization work on the fairway will be conducted only on the stretch from shore to approx. 800 m toward the open waters of the Gulf, and their scope is comparable will work utrzymaniowymi, it must be considered that the project will have no significant impact on the ecological potential JCWP Świna estuary fish fauna in the area.
JCWP Szczecin Lagoon. As part of the natural inventory carried out for the report on the impact of the project on the environment [26] in the spring and autumn 2014. JCWP in the area of Szczecin Lagoon catches were made on five research positions (Fig. 14), ie .:
ST2, BT3, ME‐W ‐ the positions of these, located in the southern Great part of the Lagoon, catches equipment position control performed with the use of the network sector set out along the transects a length of 1500 m;
TW2, M1 ‐ these positions, located in the northern part of the Lagoon of Holy, yields were carried out using the towed equipment (trawl) transepts along a length of 1500 m.
Results of testing carried fish fauna are presented in Table. 33a, and 33b. On the above. positions have been reported a total of 16 fish (Table 34). It was found that the species of fish fauna becomes poorer as the distance from the shoreline Lagoon, while increasing the concentration of the dominant species. The level of biodiversity of fish fauna near the port Stepnica (position ST2) was almost twice as high as the transects in the central part of the basin (position 3 and BT‐ME‐ W). The presented results (table. 33b) attention is almost 6‐fold higher rate of biodiversity Shannon‐Wiener transect the position TW2 (located in the vicinity of the New Warpno) relative to transect the position M1 (located adjacent the peninsula trench in the eastern part of the Lagoon .) despite the conclusion of the same number of species in trałach performed on these transects. This difference explains a more equal share of species in the structure of the transept trapping TW2. Although the predominant part was here perch next to this species were found including three subdominacyjne presence of other species, ie. Roach, bream and ballerus ballerus [39].
Dominant in terms of numbers, when fishing with nets were percidae sector, in particular jazgacz whose density depending on the position ranged from 58.5 to 87.8%. The test results also showed that the share of older individuals of this species grows in the direction of the central part of the Lagoon.
Dominant in terms of numbers when fishing with trawl were carp, whereby the position of the M1 animals of the family were up 93.3%, and the position of TW2 only 51.4%. The position TW2 46.4% of catch numbers were percidae, mainly perch, whose density was 45.5%.
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Fig. 13. Fishing Research fish fauna in the Szczecin Lagoon and the Pomeranian Bay (own study on the basis of: [21]).
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It should be emphasized that according to the information given in [26, 39] is carried fisheries, there were no protected species listed in Annex II of the habitats. As the most valuable species indicated CERT ‐ noted in the yield from the position ST2 ‐ which is due to serve their migration be considered an indicator of patency Lagoon for anadromous migratory fish species.
Table 33a. The test results ichtyofauna Szczecin Bay via the network sector of the catches (from [39]).
catching results ST2 BT3 ME‐In
catch species structure number of identified species 8/3 5/4 6/6 season spring / autumn season jazgacz (58.47%) jazgacz (72.31%) jazgacz (87.80%) the dominant species in perch (15.25%) perch (13.85%) perch (10.98%) numbers roach (9.32%) the dominant species in perch (33.7%) terms of biomass catch size structure [%] 9 mm 72.02 56.92 46,00 15 mm 18.52 33.85 41,00 25 mm 5.35 6.15 6.00 30 mm 2.88 0.00 6.00 40 mm 1.23 3.08 0.5 55 mm 0.00 0.00 0.5 catch biomass [g] season spring / autumn season 3852.6 / 603.8 981.7 / 887.9 1973.2 / 332.6 biodiversity index Shannon‐Wiener [bit / separately.] season spring / autumn season 1.9 / 1.05 1.15 / 1.10 1.2 / 1.45
Table 33b. The test results ichtyofauna Szczecin Bay using bottom trawl catches (from [39]).
catching results TW2 M1 catch species structure number of identified species of 9/9 9 the spring season / winter
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catching results TW2 M1 perch (45.53%) ballerus ballerus the dominant species in bream (17.43%) roach (7.77%) numbers ballerus ballerus roach (16.56%) catch size structure [%] less than 8 cm 1.96 1.55 8‐12 cm 58,39 7.77 12‐21 cm 22,00 86.53 21‐25 cm 8.71 2.85 than 25 cm 8.93 1.30 catch biomass [g] season spring / autumn season 49759.7 / 10,811.3 biodiversity index Shannon‐Wiener [bit / separately.] season spring / autumn season 2.05 / 1.25 0.35
Table 34. Fish species found in Szczecin Lagoon (from [39]).
lp government family type 1 sprat clupeiformes clupeid 2 Herring 3 osmeriformes smelts sparling 4 roach 5 bream 6 white bream 7 cypriniformes carp ballerus 8 bleak 9 certa 10 dace 11 gasterosteiformes stickleback stickleback 12 gobies goby 13 perch perciformes 14 percidae zander 15 jazgacz 16 Flatfish płastugowate flounder
As part of the natural inventory investment made for Modernization of the fairway Świnoujście ‐ Szczecin (Channel Piastowski and Mieliński) ‐ stage II, east side and west [11] 115
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in water Channel Piastowskie and Channel Mielinski were found nine species (sturgeon, paprosz, alosa, shrew blow Bitterling, loach, goat, loach), and two species of kręgoustych (lamprey and lamprey), mentioned in Annex II of the habitats .
Water Channel Channel Mielinski Piastowskie and recognizes [11] as an important passage used for both the migration cyclic, and the yearly seasonal migrations. Artificial shaped trough and reinforced edges of said channels, the use thereof for shipping and present there a significant change (variation) at the time of the flow characteristics of water and its physicochemical characteristics (direction and velocity of flow, flow rate, level of the water, sediment transport, salinity et al.) make in this area is the lack of well‐educated and occupying respective surfaces conducive to sustainable habitats, breeding and stayed on.
In light of the above, the results of research inventory ichtyofauna justified it seems to assume that the main corridor migration for migratory fish from the sea ‐ through the straits Swina, strange and foam ‐ for the Szczecin and further up the fugitive him the rivers and in the opposite direction is the fairway and area attached thereto. Breeding places, however, are the coastal areas of the Lagoon.
Fairway established a path of water in the environment for more than 100 years. The scope of modernization will not change the critical environmental conditions on the use of the basin as a migration route for fish. This work will not pose a threat to migratory organisms ‐ if they are carried out outside the period of migration of fish from the sea to the lagoon and in the opposite direction. Referring to raised in [39] issues not fully recognized the impact of noise caused by the movement of vessels on the fairway, it is worth noting that the modernization of the fairway is to make it accessible to larger vessels which in practice does not necessarily mean increasing the level of noise at the same frequency movement. There is therefore no evidence to believe that the modernization and further exploitation of these channels could adversely affect fish migrations.
Under JCWP Szczecin Lagoon Project work will not be done umocnieniowe existing banks. However, in the framework of the investment associated with building and strengthening the edge of the bottom it is planned only in the area of port Swinoujscie, on the right bank Świna waist and bottom adjacent to it. The project and accompanying investments, therefore, do not pose a threat to the breeding sites of fish in this JCWP.
From the analysis of the tests carried out it shows that due to the conditions of life of fish fauna in Szczecin Lagoon dumping site dredging fairway should be located at the greatest possible distance from the existing shoreline Szczecin Lagoon. Indicated in [39] places the location of these landfills ‐ in the form of one or three islands ‐ meet this requirement. It should also be stressed that the planned dumping site
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will be located in areas of the muddy bottom of the low diversity of species present therein, characterized by high resistance to environmental stress [39].
Deposition of excavated material may cause damage to part of the population of fish fauna inhabit the island region formed ‐ this is particularly small and slow flying species. Created during klapowania excavated barriers suspension or chemical can modify the route of movement of fish. The decrease of transparency of water during the construction of the island may decrease the production of biological and disrupt the availability of food for the fish living in the neighborhood. Ww. Negative impacts will be local in nature, however, and the short‐ term.
By contrast, will result from the deposition of spoil islands should be considered a positive impact in relation dwelling fish fauna in the area. Increasing the length of the edge area and in particular littoral available to the fish fauna, the formation of microhabitat for fish of different age groups, the formation of islands will increase the heterogeneity of the habitat available to the fish fauna ‐ establishment of the seat different from where the uniform bottom muddy, dominant Szczecin Lagoon as also places the planned islands.
Poor food base, which is formed zoocenozy bottom area of the planned spoil not create good living conditions and environment for the fish fauna. Preparation in the immediate vicinity of new islands, a different team as benthos, contrary to the current, which can attract more than ever occurring species of fish there, increasing local diversity.
Caused the creation of the islands change fields bottom currents will concern small in relation to the entire Lagoon, areas ‐ the area of the islands will constitute less than 1% of the area of the Great Lagoon. So it should not significantly change the migration routes of fish. At the same time the change of the currents in the area of the islands, resulting in a reduction in the deposition of organic matter may lead to the emergence of the species in this area with higher environmental requirements or colonization while shallow areas formed by the water plants to generate formation of microhabitat, or finally spawning.
With this in mind, it should be considered that the project will have no significant impact on the ecological potential JCWP Szczecin Lagoon fish fauna in the area.
Measles JCWP from Párnica to the mouth.
As part of the natural inventory carried out for the report on the impact of the project on the environment [26] have been made research catches the fish fauna in the coastal zone between the Odra river and the Police, Szczecin, Channel Grabowski and Piercing Mieleński. 12 has been established inventory segments, which were determined from 3 to 5 points trapping spaced apart by 100 ÷ 300 m (total of 47 points). research
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They concentrated in regions that were expected to disrupting the existing shoreline and changes in the structure and configuration of the edge. Efforts to investigate the most diverse types of habitat. When selecting the points taken into account, in particular: the direct location in relation to areas in the vicinity of the investment bank of a different character, a kind of bottom, the nature of the vegetation and the associated probability of presence of fish in various stages of age. Catches were carried out at the turn of May and June 2015. Using an approved kit elektropołowów.
Results of testing carried fish fauna are presented in Table. 35a ÷ tab. 35c. In sections of inventory it has been reported a total of 12 fish (Table. 36), including two protected (caprine and asp).
Table 35a. The test results of the Oder fish fauna from Párnica to the mouth of the positions 1 ÷ 4 (from [39]).
catching results 1 2 3 4 number 237 89 thirty 0 catch species structure
number of identified species 10 7 5 0 of roach (34.6%) roach (43.8%) perch the dominant species in rudd bream (27.0%) perch (22.5%) numbers (33.3%) perch (16.5%) bream protected species goat asp
Table 35b. The test results of the Oder fish fauna from Párnica to the mouth of the positions 5 ÷ 8 (from [39]).
catching results 5 6 7 8 number 109 0 29 0 catch species structure
number of identified 6 0 4 0 species of roach roach the dominant species in perch perch numbers
protected species
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Table 35c. The test results of the Oder fish fauna from Párnica to the mouth of the positions 9 to 12 [(based on [39]).
catching results 9 10 11 12 number 91 13 61 37 catch species structure
number of identified species 5 2 5 2 of roach roach (92.3%) roach roach the dominant species in perch perch perch numbers (10.98%) (39 6%) (18 0%)
protected species goat
Table 36. Fish species found in the Oder from Párnica to the mouth (from [39]).
lp government family type 1 bream 2 asp 3 white bream 4 I with carp cypriniformes 5 roach 6 rudd 7 tench 8 Longhorn goat 9 esociformes szczupakowate pike 10 gadiformes miętusowate burbot 11 percidae perch perciformes 12 gobies goby
The area covered by tests stated locations of special interest for fish that can be used as spawning [26]. The entire stretch of the Oder River estuary in the area of Swinoujscie‐Szczecin is in fact long been subject to strong human pressure (the waterfront and the heavy traffic and vessels). In contrast, the edge sections unchanged or slightly changed by human are covered by trees ‐ some of which are due to wash the infected by the water has been roll‐over ‐ or wide belts compact and rushes. Relatively few places shallowed occupied by submerged vegetation, which usually is a substrate for laying eggs and, just as importantly ‐ sheltered from direct traffic surge caused
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by vessels. This configuration
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coastal zone is not conducive to spawning. Favors while bytowaniu fish. This applies to both actively floating fry and adult forms. This is confirmed by the results of the research. The most varied species were episodes inventory 1, 2 and 5 (respectively 10, 7 and 6 species) contained in reservoirs with small depths, the edges rich fallen or growing on the edge of the water trees, vegetation submerged and floating leaves, and a low density rushes. In the course of the Project should therefore take into account the changes in the existing structure of fish fauna due to displacement of parts of individuals in places not threatened. After its completion, however, you can expect a fairly rapid return to the status quo.
With this in mind, it should be considered that the project will have no significant impact on the ecological potential JCWP Odra from Párnica to the mouth of the fish fauna in the area.
4.2.3.2. Hydromorphological elements.
JCWP Estuary Świna. Under JCWP Estuary Świna is only a 800‐meter stretch of the Swinoujscie‐Szczecin. As part of the so‐called. accompanying investment is intended to be deepening to 14.5 m. depth technical Currently, this section of track is 14.3 m. Dredging works ‐ which will be made in the framework of the statutory tasks of the Maritime Office in Szczecin ‐ due to their scope should be considered as maintenance work podczyszczeniowe . They will have virtually no significant effect on the ecological potential JCWP Mouth Świny in the range hydromorphological elements.
The outflow of water from the lagoon to the Pomeranian Bay and the inflow of marine waters Lagoon depends on the difference in water levels of the reservoirs. Increasing the cross‐sectional area at the mouth of the fairway Świny approx. 1 ~ 1.3% did not cause detectable changes in hydrological regime or current distribution. Will not affect the meteorological conditions of the area and will not change the retention time of water.
Increasing the depth of the existing fairway only approx. 1.4% will have practically no influence on the estuary JCWP Świny both in plan, as in terms of the depth (bathymetry). The bottom of the fairway, due to the presence of water currents with variable directions and speeds, naturally subject to local variations. Deepening the track of 20 cm will not, therefore, a significant change in its structure and quantity of the substrate (the particle size, the content of organic compounds). It does not involve a change in the organic compounds in bottom sediments.
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The Ordinance of the Minister of Environment of 22 October 2014. On the classification of surface water bodies and environmental quality standards for priority substances when evaluating the morphological transitional waters was specified index structure of the band tides ‐ described by covering the plant and the composition of the vegetation belt shore subject to tides . Tides in the Bay Area are just a few centimeters, which makes her area would be hard to extract even subject to the tides belt shore. Deepening the fairway to disturb the natural rhythm and size tide the present JCWP.
As a result of the planned dredging work there will be no change in the index impact WskWp JCWP considered (see chap. 4.1.3.1).
JCWP Szczecin Lagoon. The planned deepening and widening of Swinoujscie‐Szczecin may cause changes in the hydrological regime JCWP Szczecin Lagoon, ie. A change in the section of water outflow from the Szczecin Lagoon to the Pomeranian Bay for three straits (foam, pigs and Dziwna) and changes in the inflow of salty sea waters of the Bay .
To estimate the effect of upgrading Swinoujscie ‐ Szczecin river water outflow section between pigs and Dziwna The foam was used in the relation given by Mielczarskiego in [23]:
100 111 P x X X X X x S D D
in which Xx It is the ratio of damming the flow for individual connections with Lagoon side, respectively: S ‐ Świna D ‐ Strange, P ‐ Foam, which is derived as:
n and X x 2 2 R AND c and hi i x where:
i = 1, n ‐ separate sections decrease in the water level along the x‐th combination Lagoon side, l ‐ the length of the trough in a separate section, AND ‐ surface area equivalent cross‐section of the trough in a separate section,
Rh ‐ hydraulic radius cross‐section of the trough in a separate section,
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c ‐ coefficient of Chézy bed in a separate section.
As equivalent to a cross section taken trapezoidal cross‐section with a width B at the bottom of the slope slopes and 1: 3.
The calculations take into account the condition that the difference in water levels between the nodes of the system Świna arms, determined along the right shoulder must be equal, respectively.
For the conditions of the pre‐planned modernization fairway assumed values for damming the flow Świna strange and foam defined in [23] to 1970. These values are shown in Table. 37. In this table, with respect to Świna, summarizes the values of the parameters used to determine the coefficients stacking flows on separate sections of both her arms. The values of these parameters were estimated by the author of this volume based on literature data.
In the calculation of the conditions after the planned modernization (Tab. 38) assumes values for odd stacking of flow and foam as in [23] and the coefficient for damming the flow Świny determined taking parameters for each of the arms shown in Tab. 37.
Table 37. Coefficients damming the flow in combination with the sea Szczecin Bay set for 1970. (From [20, 23]).
x connection L C B h AND Rh X Xand The [M] [m2.1 s‐1] [M] [M] [m2] [M] [10‐7 m‐5 s‐2] [10‐7 m‐5 s‐2] and lagoon S Swina 0.76 Cumulat 1 4200 52.17 250 14 4088 14.7 0.063 0.063 ive channel 3400 49.96 110 10.5 1486 11.3 0544 2 Mieliński 0.195 side Swina 3900 45.10 250 6 1608 6.1 1,208 3 South 900 47.34 300 8 2592 8.2 0.073 0.073 Swina Piastowski 4 6400 49.96 110 10.5 1486 11.3 1,024 canal 0.426 old Swina 10110 42.05 500 4 2048 4.0 3.381 D Odd 45.97 1 Odd 45.97 P Foam 21.62 1 Foam 21.62
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Table 38. Coefficients damming the flow connections Szczecin Lagoon from the sea after a planned modernization fairway (from [20, 23]).
x connection L C B h AND Rh X Xand The [M] [m2.1 s‐1] [M] [M] [m2] [M] [10‐7 m‐5 s‐2] [10‐7 m‐5 s‐2] and lagoon S Swina 0.44 Cumulat 1 4200 52.49 250 14.5 4256 15.3 0.055 0.055 ive channel 3400 51.49 120 12.5 1969 13.6 0.244 2 Mieliński 0.116 side Swina 3900 45.10 250 6 1608 6.1 1,208 3 South 900 49.59 300 10.5 3481 10.8 0.028 0.028 Swina Piastowski 4 6400 51.49 120 12.5 1969 13.6 0459 canal 0.245 old Swina 10110 42.05 500 4 2048 4.0 3.381 D Odd 45.97 1 Odd 45.97 P Foam 21.62 1 Foam 21.62
Obtained as a result of the above. calculation of the estimated outflow section of river water between pigs Dziwna and foam and between individual arms Świny before and after the planned upgrading fairway are shown in Table. 39 and Tab. 40. It should be emphasized that the values given in the tables share respective connections in the outflow to be regarded as a guide. The aim of the calculations was primarily to estimate the scale of changes in these shares in case of realization of the planned modernization of the fairway. Obtaining a more accurate value of the relevant calculations would require using three‐dimensional model hydrodynamic implemented for all of the analyzed bodies, under conditions of current bathymetry and after all the changes resulting from the modernization of the fairway.
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Table 39. Estimated distribution of river water outflow from the Szczecin Lagoon before and after the planned modernization of the fairway to a depth of 12.5 m.
Lagoon connection % Of the total outflow of river waters sea before the modernization after Swina 76.0 80.5 Odd 9.8 8.0 Foam 14.2 11.5
Table 40. Estimated outflow section of river water and the pigs against the planned upgrading fairway to 12.5 m.
arm system % Of river runoff by Swina Świna before the modernization after Piastowski canal 64.5 73.1 old Swina 35.5 26.9 channel Mieliński 59.8 69.0 side Swina 40.2 31.0 arm system % Of river runoff by Swina Świna before the modernization after Piastowski canal 49.0 58.9 old Swina 27.0 21.7 channel Mieliński 45.5 55.6 side Swina 30.5 25.0
Nevertheless, the results section of river water outflow Świna, strange and Foam are consistent with data reported by other authors. According to [76] to Swina accounts for 78% foam 14%, and a strange 8% of the total volume flow of the river. As many as 47% of the total volume flow of the river is directed Piastowskim Canal, while 31% Old Fever (which is respectively 60.3% and 39.7% for the outflow of swine). Ww. flow ratios were determined on the basis of measurements carried out in the 60s of the last century. According to [12] 65.3% by river water runoff channel is directed Swina Piastowskim and 34.7% Old pigs. Then 58.5% of the outflow channel is carried Mielińskim and 41.5% ‐ side pigs.
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On a similar scale reshuffle the outflow of river water Świna, strange and Foam showed the results of motion simulation set made using three‐dimensional numerical model of the estuary of the Oder ESTURO, developed by the Institute of Hydraulic Engineering (IBW), the PAN in 1998 ÷ 1999 the work on specific guidelines to design target solution hydrotechnical Swinoujscie‐ Szczecin [14]. This model is an implementation package trisula (delft3D‐flow), developed by Delft Hydraulics, for the area of the Szczecin Lagoon, together with the straits ‐ Świna, strange and Foam ‐ and the Bay of Greifswald and part of Pomeranian Bay (limited from the north by a line extending from the island of Rügen in the area Sassnitz to Polish shore in the area of Mrzezyno).
ESTURO model is a hydrodynamic model includes information regarding the transport equation, which allows to determine the transfer and mixing of the reactive substance, and thereby determine movement of saline.
In this model, above. reservoirs are illustrated by a curved grid, the axis of which coincides with the path of the Swinoujscie ‐ Szczecin. In the nodes of the grid, vertical layers 8 has been established with the following distribution depth: 1 (selvedge has) ‐ 5% 2 ‐ 10% 3 ‐ 15%, 4 ‐ 20% 5 ‐ 20% 6 ‐ 15% 7 ‐ 10%, 8 (near the bottom) ‐ 5%. Depth nodes were adopted: for the area of the Pomeranian Bay and Szczecin Lagoon ‐ based on nautical charts, cross‐strait Świna on the fairway and by the Szczecin Lagoon according to the surveys made by the Maritime Office in Szczecin.
ESTURO model has three open borders, where questions are boundary conditions. And so: in the western part of the Bodden and the Pomeranian Bay asked are: the level of the water table and its salinity and temperature, while the south side: the flow of the Odra and the salinity and temperature of water flowing Oder. The initial conditions are the water level, flow rate, and temperature and salinity of the water in the nodes of the net. In the calculations it was taken as the initial conditions of the same water level and a zero flow rate. The initial temperature and salinity of the waters of the basin modeled differentiated by dividing it into seven sub‐areas. Calculations were performed with the time step equal to 1 minute.
In the framework [14], using a model ESTURO was designated section of river water outflow pigs strange and foam under a steady flow of the Oder of 1000 m3 / sec, a constant level of the sea and no wind. The calculations do not taken into account differences in the density of water to eliminate the change in the proportion of cash flows due to two‐way. The results of these calculations ‐ for bathymetry fairway 1968. Bathymetry and the fairway of 1998. ‐ summarized in the Table. 41 and Tab. 42.
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Table 41. Chapter outflow of water from the river Szczecin Lagoon determined by the model ESTURO (Source: [14]).
connection % Of the total outflow of river waters The lagoon bathymetry track of bathymetry track of 1968 1998 Swina 79.9 80.9 Odd 8.1 8.0 Foam 12.0 11.1
Table 42. River water outflow section Swina determined by using a model ESTURO (Source: [14]).
arm system % Of river runoff by Swina Świna bathymetry track of 1968. bathymetry track of Piastowski canal 72.0 74.2 old Swina 28.0 25.8 channel Mieliński 65.4 70.9 side Swina 34.6 29.1 arm system % Of the total outflow of river waters Świna bathymetry track of bathymetry track of 1998. Piastowski canal 57.5 60.0 old Swina 22.4 20.9 channel Mieliński 52.3 57.4 side Swina 27.6 23.5
Comparative analysis of the results presented above estimation section mean annual runoff Oder in Szczecin Lagoon strait connecting with the sea it indicates that a planned upgrading fairway approx. 3 ÷ 5% greater than the volume of the outflow is directed pigs. Consequently, the volume of effluent waters of the Oder straits: strange and ‐ through the Little Lagoon ‐ Foam will be reduced by about. 1 ÷ 2 ÷ 2% and 3%. But this should not significantly change the functioning of aquatic ecosystems, water bodies separated on these areas: JCWP Lagoon Kamieński JCWP and Kleines Haff. Underline requires that JCWP Kleines Haff has been recognized by Germany for the coastal waters and therefore within the meaning of the Water Framework Directive as not being substantially influenced by freshwater.
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In [23] Apart from the above. damming the flow coefficients for each connection Szczecin Lagoon for specific dates expansion of shipping lanes of the basin, also determined resultant damming the flow rate for the whole system of connections and average values likely bleed water level between the Baltic Sea and the Lagoon. An estimated average bleed dates for all the characteristic expansion of the sailing routes taken flow value equal to the average annual 620 m3 / s. For older dates, the value of this ‐ mainly due to the greater forest cover of the Odra river basin and reduced water consumption by the economy ‐ should be considered underestimated. Despite this, presented in [23] The calculation results show that the scale of the former hydrological changes were much larger than today's changes.
Designated in [23], values of coefficients and damming the flow of water between the average bleed Lagoon and the Baltic summarized in Tab. 43. In the last line of the table determined in this study of these parameters determined for the state after the planned upgrading fairway to 12.5 m ..
Table 43. Changes in Szczecin Bay hydrological conditions caused anthropopressure (from [23]).
the resultant flow rate the average slope between time (anthropopressure) damming the water surface and the sea 1720. (Start action to open Świna 11.81 0.49 for shipping)
1776. 9.38 0.40 1817. (1817 ÷ 1829 the orientation as in 1776. construction of breakwaters 1840. 5.39 0.23 1880. 1.30 0.05 (Opening of the Piastowski Canal) 1900. 0.98 0.04 1970. 0.44 0.02 after the planned upgrading 0.29 0.01 fairway
The abovementioned results of calculations and analyzes indicate that lasted from 1720. Transforming shipping lanes within the Szczecin Lagoon caused a decline in the average level of
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water in the Szczecin Lagoon to the elevation almost equal to the average water level in the Pomeranian Bay. The consequence of this is:
intensive exchange of water between the Pomeranian Bay and Lagoon called spiętrzeniami storm in Pomeranian Bay, raising the average salinity of the Szczecin Lagoon - conversion of the former in a fresh water tank brackish water. Extreme rise of water level in the Szczecin Lagoon and lower the Oder, constant self-Channel deepening Mielinski and Piast.
The planned modernization of the fairway Swinoujscie‐Szczecin to a depth of 12.5 m is the continuation of this process. The question therefore arises whether the change shown above hydrological regime, due to this upgrade will not:
a major enhancement to extreme water levels in the Szczecin Lagoon and the lower Odra, resulting in an increase of flood risk in this area, significant changes in salinity waters of the Szczecin Lagoon, which is a threat to ecosystems a significant change in water velocity strait Świny, and in particular the speed of bottom.
In 1999. Under the [15], by means of the above. model ESTURO ‐ previously calibrated and verified ‐ simulated variations of modernization strait Świny (eg. partition Lateral Świna elongation Channel Piastowskie, reducing the depth of the channels and Mielinski Piastowskie, execution of the orifices in the channels) and their builds. These calculations were done for the bathymetry of the track 1998. In all embodiments, it was assumed increase of the channel width of the marine bottom 90 m to 110 m. Simulated hydrodynamic two situations: the average storm (which occurred during the period 10 to 10.20.1985 r.) And extreme storm (which occurred during the period of 31.10 ÷ 7.11.1995 r.). In order to evaluate alternatives comparisons were performed, among others, changes maximum water levels in the lagoon selected points (ie. the outlet of the channel Piastowskie to flooding in the area of thinning in the south‐east and north‐west of the Lagoon).
In view of this volume, the most interesting variant is the shortness Channel Mielinski and Piastowskie to 10.5 m, referred to as a variant of 10.5 m. This option as it allows to estimate the scale that may be changes in the level of water and its salinity in Szczecin Lagoon a change the depth of the shipping channel. Presented in [15], the simulation results indicate that the flattening of the channel bottom and Mielinski Piastowskie to a depth of 10.5 m in relation to the bathymetry 1998. Resulted in only a 2‐3 cm change in the highest levels of water under ordinary storm.
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According to [13, 16], using the model ESTURO, we were also performed testing the effect of deepening a fairway strait Świny from 10.5 m to 12.5 m 14.5 m. (12.5 mi variant embodiment of 14.5 meters) levels and flow in Szczecin Lagoon and its salinity. It was found that increases the water level in Szczecin Lagoon caused by changes in the depth of the water path is small. Variant of 12.5 m in the inflow simulated storm average, the increase of water level was approx. 3 cm variant of 14.5 m ‐ another approx. 3 cm [15]. Small increases in the water level in the Vistula result from relatively short periods of influx of marine waters (1‐2 days) and a large area of the basin.
Changes in salinity in the Szczecin Lagoon, resulting from the different variants of modernization of the strait Świna assessed on the basis of the average salinity of the lagoon, which is determined from the value of the salinity in the individual layers twenty points located throughout the basin, obtained by simulating the average storm. In [15] are set to values determined in this way the average salinity flooding in terms of the average storm prior to infusion of saline (11.10.1985 r. H. 0.00) and after the storm (10.21.1985 r.). They show that the shortness of the bottom of the Piast Canal Mielinski and to a depth of 10.5 m (10.5 m variant), in relation to the 1998 bathymetry., Resulted in a slight decrease in the salinity of the waters of the Szczecin Lagoon. The average salinity of the storm was 0.881 in this embodiment dog (from 0.702 to dog the storm)
According to [13, 16] obtained in the comparison result of the simulation options: 10.5 m, 12.5 m and 14.5 m field distribution salinity and flow in surface layers and in the layers of bottom Szczecin Lagoon not indicated a significant effect of deepening the waterway in a strait Świny the range of propagation in the Lagoon seawater flowing thereto. It should be emphasized, however, that the above. Simulations were performed with a depth leaving the fairway for Lagoon Oder and at ‐10.5 m. Deepening the track at these parts to 12.5 m will mean a greater range of salt water wedge wezbraniach after heavy seas.
In [15, 16] also included resulting from simulations using a model ESTURO applications in assessing the impact of the proposed variants of modernization seaway Świny strait on the hydrodynamic conditions prevailing in the strait. It was found that with increasing depth of the waterway increasing flow Channel Piastowskim. Thus, assuming the flow in the embodiment of 10.5 m for 100%, the estimated desired track deepening to 12.5 m will increase the flow rate of approx. 20% and deepening to 14.5 can be more than ten percent. Speed at the bottom of this channel while rated as similar in all variants. At the same time stressed that the strait Świna since the construction of the Piast Canal and Mielinski is steadily deepening, whose rate in the period 1950 ÷ 1999 rated for 2 to 4 cm / year.
As part of the ongoing work on the IBW PAN specific guidelines for the design of the target solution hydrotechnical Swinoujscie‐Szczecin, using package trisula (delft3D‐flow) has been developed
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Also Strait Świny model [17]. This model ‐ based on the bathymetry of 1998. ‐ served, among others, to study the hydrodynamic conditions in the Strait of Świna The side with the Old and pigs in a situation of deepening the fairway to 12.5 m. in 2009. This model has been upgraded in the field of bathymetry. Also the modified grid in order to more accurately track the position of the mapping aqueous [43, 44]. Made using this model simulations indicated that:
the current conditions of the bathymetry of the Strait of bottom Świny speed greater than a predetermined threshold speed (the speed of blurring) of 0.45 m / s are low heads of water between Świnoujście and AND gate of rail or between channels A and gate Swinoujscie larger and equal to 0.2 m (the probability of bleed water on the values of approx. 10%),
as a result of the proposed changes in the seaway Strait Świny change the slope of the water table, particularly in the channels and Piastowskie Mielińskim, which will result in changes in water velocity. Under the inflow of water into the Lagoon will be a slight increase in near-bottom water velocity in the region Cumulative Świna. Whereas, under the water outflow from the lagoon, in the case of an abrupt increase in water level in the basin, there will be a significant increase in speed in the region of bottom Piastowski Canal.
Bearing in mind that the planned modernization of the fairway will not stop the progressive deepening of the Strait Świna Project provides for filling existing channels Mielińskim trims and Piast dredged material originating from dredging work on the fairway. This will improve the safety of embankments on the track and at the same time eliminate the possibility of higher than estimated above reshuffle flows between pigs and Dziwna foam.
The retention time of the body of water is expressed as the ratio between the volume of a river, the annual supply. Volume JCWP Szczecin Bay, based on [76] can be estimated approx. 15,57 thousand. km3. Planned deepening and widening of the waterway extending through the JCWP an increase of the volume of approx. Approx. 0.08 km3 and will not cause virtually no change in the retention time of the water reservoir.
Project implementation in no way affect the meteorological conditions in the area of the Szczecin Lagoon.
Modification of the depth of the waterway at approx. 11.4 km (which consists of deepening to the ordinate 12.5 m or filling up the trims to the local elevation of 12.5 m), increase the width and depth of the fairway for approx. 27.5 km , mijanki embodiment and the construction of new or extension of existing storage facilities dredging spoils will cause changes in the configuration of the bottom surface 9 ÷ 10 km2, approx. 2.5% of the entire lagoon JCWP Szczecin. The project does not provide for changes in the course of the existing coastline JCWP and related changes associated developments are insignificant in scale this JCWP. However, due to the construction of new deposition dredging spoils will extend the
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the total length of shoreline located within the basin islands. Depending on the variant adopted storage of excavated material and design solutions adopted, it may be several kilometers (approx. 5% of the length of the current shoreline analyzed JCWP). The project will therefore affect the shape of the Szczecin Lagoon JCWP both in the plan, such as in terms of the depth (bathymetry).
Planned Project work affecting the bottom, ie. Deepening and widening of the existing fairway with the staggered arrangement and the motor unit and the construction of islands / island of refulatu or extending existing landfill refulatu not cause significant in scale JCWP Szczecin Bay, changes in the structure of a quantitative and a substrate base ( The particle size, the content of organic compounds). They do not involve a change in the organic compounds in bottom sediments. The work carried out for the gutter are in the existing deep fairway. The proposal provides no new fortifications or bottom edges in the area JCWP Szczecin Lagoon, in the framework of the planned investments associated with the strengthening of the bottom relate to only 0.02% of the JCWP.
The Szczecin Lagoon phenomenon tide does not occur [3, 36], thus indicated in the Regulation of the Minister of the Environment of 22 October 2014. On the classification of surface water bodies and environmental quality standards for priority substances for the evaluation of morphological conditions index structure of the band tides ‐ described by plant cover and composition shore vegetation belt subject to tides ‐ is not for this body of water use.
To assess the impact of the Project and related projects on ecological potential JCWP Szczecin Lagoon in terms of morphological elements may be used indicator of the impact WskWp, used for the initial determination of heavily modified water intermediates (see chap. 4.1.3.2). Demonstrate that the morphological changes resulting from the planned investment result in a significant change in the indicator WskWp impact, would give the basis for the assertion that the implementation of this investment may result in a reduction of the ecological potential in terms of morphological elements and, consequently, change the overall assessment of the JCWP. A significant change in the morphological elements may also affect the selection of the biological elements of that body and thus lead to the deterioration of her general condition. The approach used in [7], wherein the assessment of the effect of the second stage of the modernization of the fairway for environmental purposes. Made according to [7. 31] quantify the morphological changes within the body of water JCWP upon completion of the step shown that the proposed project will result in only approx. 1 the percentage change in impact indicator (WskWp = 20:27). This made it possible to recognize that it will not significantly affect the ecological potential JCWP Szczecin Lagoon in terms of morphological elements.
In the case of the Project and related projects, changes affecting the value of the indicator is the impact of changes in the scope of:
surface of the aggravated fairway (approx. 4.7 km2)
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surface exposed to violation of sludge (approx. 1.25 km2 in connection with the embodiment of the passing place at the Lagoon) spoil storage area (with a preferred embodiment of the three islands approx. 3.8 km2) quays length (about 642.2 m).
Made according to [7, 31] quantification of the lesions in the JCWP Szczecin Lagoon the project and the accompanying investments are shown in Tab. 44. These changes result in an increase in the value of the indicator for the impact of WskWp 21.91. Stacked ‐ ie. Resulting from the modernization of the whole Swinoujscie ‐ Szczecin and the associated track operatively investment ‐ increase this ratio would be 2.63%, which in comparison with the projected increase in the depth of the track 2 m ‐ according to the author of this volume ‐ no longer allows argue that the project does not affect the ecological potential JCWP Szczecin Lagoon in the range of morphological elements. In contrast, the potential impact of the above. morphological changes in the ecological potential of the JCWP in terms of macrozoobenthos presented in Chap. 4.2.3.1.
It should be emphasized that in the current legal status of a heavily modified body of water in the field of transitional hydromorphological elements is broadcast a'priori Class II. In the case where the classification of the biological elements JCWP indicating their poor environmental potential, irrespective of the classification results hydromorphological elements (as well as physical and chemical) of the JCWP suitable class V ecological potential.
Table 44. Morphological changes within the JCWP Szczecin Lagoon on the implementation of the Project and related projects and their evaluation.
relevance ecosystem kind of change d changes WskWp degree WskZn of change [%]
1 The total area of fairway dredged 49.10 0.67 8.08 The total area exposed to changes in bottom 2 sediments violation (trawling, anchoring and 37.33 0.20 1.83 turntables)
The total area of the stored ore bagrowanego 3 6.10 0.50 0.75
The total length of the edge Building spurs 4 0.25 0.00 piers 5 The total length of the breakwaters 2.54 0.40 0.32 The total length of the fairway for deep lagoons 6 43.75 0.40 5.44
7 The total length of the transverse structure 0.50 0.00
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8 Total length of quays 67.37 0.50 1.15 9 The total length of the edge bands (reinforcements) 24.36 0.20 1.51 10 The total length of the supplied bank of 0.08 0.00 11 The total length of dikes 70.03 0.13 2.83 The calculation result of changes in ecosystem resilience [%] 21.91
Measles JCWP from Párnica to the mouth. Project and associated developments in no way interfere with the continuity of morphological JCWP Measles from Párnica to the mouth.
Interference in the form of a trough and its variation width and depth of this section refers only to JCWP, on which the fairway. Width at the bottom of this track is now 90 m, while the width of the river is much greater. It is a water mirror 180 ÷ 200 meters and more, and downstream of the Inoujście ‐ called Domiaza ‐ even 300 to 400 m. [22]. The maximum depth JCWP Measles from Párnica to the mouth below the connection Przekop Mielenski correspond to the current depth technical or fairway is its greater. This applies in particular Domiąży, which rises to a depth of 12 m, and locally up to 14 m.
Extending fairway to 100 m and the bottom of the deepening to 12.5 m will increase the cross sectional area of the trough. For example, in track section of km 53.000 to km 54.700 increase in cross sectional area of the trough in relation to the cross‐sectional area of the fairway of current technical parameters can be estimated at approx. 7 ÷ 13%, for the section from 55,400 to km 59,100 to approx. 12 ÷ 14%, and the section from km 60.500 to km 62.900 approx. 8 ÷ 16% [27]. It can therefore be assumed that the modernization fairway within JCWP Measles from Párnica to the mouth will not greater than 16% strength increase of cross‐sectional area of its channel.
Measles JCWP from Párnica to the mouth of the river network is part of the lower Oder. United and flows (and velocity) in the individual sections of the network that network dependent feature the level of the sea and the river flows from the top (see rozdz.4.1.2.3). Determination of the value ‐ and in the case and the flow velocity on the direction of ‐ for given boundary conditions bathymetric and requires a calculation using suitable hydrodynamic models. Bathymetry change at one of the sections of the river network may result in changes in flow speed on both this and the other sections of that network. In Tab. 45, as an example, shows the values of the average velocity in one of the sections Domiąży and obtained by means of developed at the Maritime Institute of Gdansk, Branch Office in the hydrodynamic model of the lower Oder to flow characteristic Oder multi‐year 1949 ÷ 1989 and the average water level in Trzebież [29 ]. This table also contains the estimated change in the water velocity after the modernization of the fairway. Due to the fact that Domiaza is a section of the river network, which is headed up the flow of the river, it was possible
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concluded that the change of flow rate in this section only result from changes in the surface of its cross‐section. The values should be treated as indicative, including no less indicate they modernization of the fairway will not cause a significant change in the average speed occurring on this section JCWP in different situations hydrodynamic determinowanych sea level and flow from the top of the Oder. No comprehensive research model on potential changes in stocks and flows in the lower Odra river network caused by the modernization of the fairway does not allow, however, to assess whether the impact of this investment in relation to other sections of the Oder JCWP from Párnica to the mouth will be as insignificant. According to the author of this volume, should therefore be considered
Project and associated developments do not affect the groundwater.
Table 45. Estimated change in the average speed of the water JCWP Measles from Párnica to the mouth section Domiąży (from [29]).
Gozdowicach the average water velocity [m / s] is a sectional flow [m3/ S] Domiąży the water level Trzebiez 0.05 m. before modernization the modernization of the WWQ = 1981 0.54 0.45 SWQ 1247 = 0.34 0.29 SSQ = 547 0.14 0.12 SNQ = 261 0.07 0.06 NNQ = 156 0.04 0.03
Planned Project work and investments associated with the work of violating the bottom will not cause a substantial change in the scale JCWP structure and substrate bottom JCWP Odra from Párnica to the mouth. Dredging will trough existing fairway remaining in the maintenance. Provided for strengthening the bottom will be performed on the surface approx. 0.016 km2 and a length of approx. 0.26 km as the length of courses relevant to JCWP of 24.047 and the average width of approx. 200 m is negligible share.
Measles JCWP from Párnica to the mouth was considered heavily modified body of water due to the longitudinal development (the waterfront and sea defenses arising from the function of port and shipping). Broadening and deepening running within the JCWP fairway does not involve the creation of new buildings and existing only with security. However, in the context of accompanying investment in this JCWP no plans to create new berths (except elongation of 35 m waterfront Harvesters Peninsula Eve). It should therefore be considered
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that the terms and structure of coastal zones JCWP Odra from Párnica to the mouth of the reply will still only impacts resulting from its characteristics that determined the designation as a heavily modified.
4.2.3.3. physicochemical elements
Transparency During the implementation phase of projects part of the program will be a temporary decrease the transparency of water due to dredging work carried out within their borders.
When carrying out dredging work, by means of dredging buckets to the surface in contact with the surrounding water, which leads to a dilution of the top layer of the precipitate collected. Freed in this way, part of the organic detritus (muds) and the fraction of mineral clay, silt or fine sand ‐ under the influence of surface currents and subsurface wave and ‐ no sediments around dredgers, but is kept as a suspension by increasing the turbidity of the water.
According to [10], the predominant fraction of sediment covering the bottom Szczecin Lagoon fairway and its surroundings are fine sands or mules very coarse and coarse. the share of organic matter in the sediments depending on the period and position ranges from less than 1% to over 20%.
In order to estimate the expected range of influence of the spread of the ore during dredging Szczecin Lagoon calculation resultant angle φ characterizing the movement of the grains sludge during sedimentation (angle characteristic falling grains), which depends current speed v and the speed of sedimentation of grains precipitate in water ie .: