Modeling and Monitoring of Hydrodynamics and Surface Water Quality in the Sulejów Dam Reservoir, Poland
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Reservoir Sedimentation Problems in the Vistula River Basin, Poland
Erosion and Sediment Yield: Global and Regional Perspectives (Proceedings of the Exeter Symposium July 1996). IAHSPubl.no. 236, 1996. 501 Reservoir sedimentation problems in the Vistula River basin, Poland ADAM LAJCZAK Institute of Nature Conservation, Polish Academy of Sciences, Lubicz str. 46, 31-512 Cracow, Poland Abstract Existing knowledge of the geometric and hydrological characteristics of existing and planned dam reservoirs in the Vistula River basin, Poland, and of the spatial differentiation of suspended sediment and bed load transport in the area provides a basis for proposing appropriate locations for planned reservoirs in the river basin. If the location and the order of building of the planned dams conform to these proposals, this will result in slow silting of the reservoirs with advantages both for the use of the river as a waterway and for maximizing the useful life of the reservoirs. INTRODUCTION The correct planning of the development multipurpose reservoir systems in large river basins, where the rivers are characterized by different hydrological regimes and different suspended sediment loads and bed load yields, presents an important problem for fluvial sedimentology. Estimation of the useful lifetime of reservoirs of very diffe rent initial geometric and hydrological characteristics, when their functions are fulfilled, must be a prelude to the correct location of planned structures. This time period, which has been estimated for every reservoir studied according to the concept proposed, should not be shorter than the amortization time of the reservoir. The above procedure can be undertaken if the following information is available: (a) the average annual suspended sediment load and bed load as measured at successive gauging stations on the river and its tributaries over a suitable period of time; (b) the initial geometric and hydrological characteristics of existing and planned reservoirs; and (c) the initial trap efficiency for the suspended sediment load of every reservoir studied. -
Floods in Poland from 1946 to 2001 — Origin, Territorial Extent and Frequency
Polish Geological Institute Special Papers, 15 (2004): 69–76 Proceedings of the Conference “Risks caused by the geodynamic phenomena in Europe” FLOODS IN POLAND FROM 1946 TO 2001 — ORIGIN, TERRITORIAL EXTENT AND FREQUENCY Andrzej DOBROWOLSKI1, Halina CZARNECKA1, Janusz OSTROWSKI1, Monika ZANIEWSKA1 Abstract. Based on the data concerning floods on the territory of Poland during the period 1946–2001, the reasons generating floods, the number of regional floods in the rivers catchment systems, and sites of local floods occurrence, were defined. Both types of floods: caused by riverbank overflows, and land flooding by rain or snow-melt water, were considered. In the most cases, the floods were caused by rainfall. They were connected with changes in the rainfall structure within Po- land. In each season of the year floods of various origin were observed. When the flood initiating factors appeared simulta- neously, the flood grew into a catastrophic size. In present analysis, for the first time in Poland, a large group of local floods has been distinguished. A special attention has been paid to floods caused by sudden flooding of the land (flash flood), including floods in the urban areas — more and more frequent during the recent years. The results of the analyses have provided important data for the assessment of the flood hazard in Poland, and for the creation of a complex flood control strategy for the whole country and/or for selected regions. Key words: flood, classification of floods, floods territorial extent, frequency of floods occurrence, torrential and rapid rain- fall, threat of life, material losses. Abstrakt. Na podstawie zbioru danych z lat 1946–2001 okreœlono przyczyny wystêpowania powodzi w Polsce, liczbê powodzi re- gionalnych w uk³adzie zlewni rzecznych oraz miejsca wyst¹pieñ powodzi lokalnych. -
Pedigree of the Wilson Family N O P
Pedigree of the Wilson Family N O P Namur** . NOP-1 Pegonitissa . NOP-203 Namur** . NOP-6 Pelaez** . NOP-205 Nantes** . NOP-10 Pembridge . NOP-208 Naples** . NOP-13 Peninton . NOP-210 Naples*** . NOP-16 Penthievre**. NOP-212 Narbonne** . NOP-27 Peplesham . NOP-217 Navarre*** . NOP-30 Perche** . NOP-220 Navarre*** . NOP-40 Percy** . NOP-224 Neuchatel** . NOP-51 Percy** . NOP-236 Neufmarche** . NOP-55 Periton . NOP-244 Nevers**. NOP-66 Pershale . NOP-246 Nevil . NOP-68 Pettendorf* . NOP-248 Neville** . NOP-70 Peverel . NOP-251 Neville** . NOP-78 Peverel . NOP-253 Noel* . NOP-84 Peverel . NOP-255 Nordmark . NOP-89 Pichard . NOP-257 Normandy** . NOP-92 Picot . NOP-259 Northeim**. NOP-96 Picquigny . NOP-261 Northumberland/Northumbria** . NOP-100 Pierrepont . NOP-263 Norton . NOP-103 Pigot . NOP-266 Norwood** . NOP-105 Plaiz . NOP-268 Nottingham . NOP-112 Plantagenet*** . NOP-270 Noyers** . NOP-114 Plantagenet** . NOP-288 Nullenburg . NOP-117 Plessis . NOP-295 Nunwicke . NOP-119 Poland*** . NOP-297 Olafsdotter*** . NOP-121 Pole*** . NOP-356 Olofsdottir*** . NOP-142 Pollington . NOP-360 O’Neill*** . NOP-148 Polotsk** . NOP-363 Orleans*** . NOP-153 Ponthieu . NOP-366 Orreby . NOP-157 Porhoet** . NOP-368 Osborn . NOP-160 Port . NOP-372 Ostmark** . NOP-163 Port* . NOP-374 O’Toole*** . NOP-166 Portugal*** . NOP-376 Ovequiz . NOP-173 Poynings . NOP-387 Oviedo* . NOP-175 Prendergast** . NOP-390 Oxton . NOP-178 Prescott . NOP-394 Pamplona . NOP-180 Preuilly . NOP-396 Pantolph . NOP-183 Provence*** . NOP-398 Paris*** . NOP-185 Provence** . NOP-400 Paris** . NOP-187 Provence** . NOP-406 Pateshull . NOP-189 Purefoy/Purifoy . NOP-410 Paunton . NOP-191 Pusterthal . -
4.Rekonstrukcja Rozmieszczenia Młynów Łodnych Na Drwęcy I Pomorskim Odcinku Wisły W Pierwszej Połowie Xix Wieku
PRACE KOMISJI KRAJOBRAZU KULTUROWEGO ISSN 1896-1460 e-ISSN 2391-5293 DISSERTATIONS OF CULTURAL LANDSCAPE COMMISSION www.cultural-landscape.us.edu.pl No. 40 (2) 2018, 71–89 DOI 10.30450/201816 Dariusz Brykała1, Maciej Prarat2 1 Institute of Geography and Spatial Organization Polish Academy of Sciences in Toruń, Poland e-mail: [email protected] 2 Nicolaus Copernicus University in Toruń, Institute for the Study and Conservation of Cultural Monuments, Poland e-mail: [email protected] REKONSTRUKCJA ROZMIESZCZENIA MŁYNÓW ŁODNYCH NA DRWĘCY I POMORSKIM ODCINKU WISŁY W PIERWSZEJ POŁOWIE XIX W. RECONSTRUCTION OF BOAT MILLS DISTRIBUTION ON THE DRWĘCA RIVER AND THE POMERANIAN PART OF THE VISTULA RIVER IN THE EARLY NINETEENTH CENTURY Streszczenie Artykuł przedstawia wyniki kwerendy źródeł archiwalnych i materiałów kartograficznych, które pozwoliły na odtworzenie lokalizacji młynów łodnych na dolnym odcinku Wisły i Drwęcy. Zidentyfikowano w sumie położenie 9 obiektów na Wiśle oraz 3 na Drwęcy. Z opracowań dla wcześniejszych okresów wiadomo o kolejnych 6 lokali- zacjach na Wiśle, które w większości nie były już wykorzystywane w XIX w. Stwierdzono ponadto występowanie w korycie rzecznym specjalnych budowli hydrotechnicznych towarzyszących młynom pływającym oraz dość częste relokacje pływaków. Abstract This article presents the results of an inquiry into written sources and cartographic materials which allowed the recreation of the locations of boat mills on the lower Vistula and Drwęca rivers. In total, there were 9 locations on the Vistula River and 3 on the Drwęca. From the research works referring to the earlier periods, we know that there were 6 locations on the Vistula, the majority of which had already gone out of use in the 19th century. -
Low-Carbon-Funding-Report-Mazovia
INDIVIDUAL REGIONAL BASELINE REPORTS ON LOW CARBON INVESTMENTS FUNDING MAZOVIA REGION Preface Present Individual Regional Baseline Reports on Low Carbon Investments Funding is a strategic document to be delivered for seven Partner Regions under the Project entitled “PROmoting regional Sustainable Policies on Energy and Climate change mitigation Towards 2030” funded by the Interreg CENTRAL EUROPE Programme. Partner Region: Mazovia Region Programme priority: 2. Cooperating on low-carbon strategies in CENTRAL EUROPE Specific objective: 2.2 To improve territorial based low-carbon energy planning stra- tegies and policies supporting climate change mitigation Project acronym: Prospect2030 Project index number: CE1373 Lead partner: Piemonte Region Project start date: 01.04.2019 Project end date: 30.09.2021 Deliverable number: D.T1.1.2 Prepared by: PP3 MAE Date: 28.11.2019 Table of Contents 1. Background ..........................................................................................1 2. Presentation of the target region ................................................................2 2.1. General presentation of the target region ................................................2 2.2. Potentials for low-carbon sector development ...........................................3 2.2.1. Energy efficiency ........................................................................3 2.2.2. Renewables ...............................................................................3 2.3. Regional low-carbon policies, institutional framework and policy -
Demonstration of the Bzura River Restoration Using Diatom Indices
Biologia 66/3: 411—417, 2011 Section Botany DOI: 10.2478/s11756-011-0032-3 Demonstration of the Bzura River restoration using diatom indices Barbara Rakowska & Ewelina Szczepocka Algology Laboratory, Department of Algology and Mycology, University ofLód´ z, 12/16 Banacha Str. PL-20-237 Lód´ z, Poland; e-mail: [email protected] Abstract: The quality of running waters is reflected in the composition of benthic diatom assemblages. The biological assessment of changes in the composition, and thus of changes in water quality, was carried out in the lowland mid-sized Bzura River, Central Poland, over the period of 30 years. The benthic diatom material consisted of samples collected in two investigation periods, in 1972 and in 2003–2004. The methods applied were three diatom indices, IPS – Specific Pollution Sensitivity Index, GDI – Genetic Diatom Index and TDI –Trophic Diatom Index, and the OMNIDIA computer program, which are commonly used in Europe. The aim of the study was demonstrating the process of restoration that occurred in the river. The Bzura was included to the most polluted ones in Poland till 1996. Since 1998 a gradual improvement in water quality has been observed, which is caused by a number of biological-technical measures, mostly a proper organization of sewage management in most cites located on the river. In 1972 the IPS classified Bzura water into Water Quality Class IV-V, while in 2003–2004 it reached much higher values, i.e. Class III-IV. On the basis of the GDI Class III was determined in the whole river in 2003–2004, while its values indicated Class III-IV in 1972. -
INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Biuro Prognoz Hydrologicznych W Krakowie Obszar Warszawa Ul
INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY Biuro Prognoz Hydrologicznych w Krakowie Obszar Warszawa ul. Podleśna 61, 01-673 Warszawa tel.: 22-56-94-144 fax.: 22-834-48-97 e-mail: [email protected] www.pogodynka.pl www.imgw.pl INSTYTUT METEOROLOGII I GOSPODARKI WODNEJ PAŃSTWOWY INSTYTUT BADAWCZY BIURO PROGNOZ HYDROLOGICZNYCH W KRAKOWIE Obszar Warszawa podaje KOMUNIKAT OPADOWY z dnia 30.07.2019 godz. 6 UTC UTC - ang. Universal Time Coordinated - czas uniwersalny; w okresie letnim czas urzedowy w Polsce UTC+2h, a w okresie zimowym UTC+1h. Dobowa suma opadu 6 UTC Stacja meteorologiczna Rzeka [mm] A B C województwo śląskie PILICA Pilica 24.7 BONOW ICE Pilica 18.5 W ĄSOSZ Pilica 10.5 województwo świętokrzyskie STANOW ISKA Czarna (Maleniecka) 9.8 PILCZYCA Czarna (W łoszczowska) 1.4 JANUSZEW ICE Czarna (W łoszczowska) 8.4 województwo lubelskie JARCZEW W ilga 37.6 województwo podlaskie ZAMOSZE Narew 0.7 BONDARY Narew 1.1 NAREW Narew 0.1 TYKOCIN Narew 0.3 MARIANOW O II Narew 0.1 NOW OSADY Kołonna 1.8 BIAŁOW IEŻA Narewka 2.3 NAREW KA Narewka 0.9 CHRABOŁY Orlanka 0.0 NOW OSIÓŁKI Supraśl 2.0 SUPRAŚL Supraśl 0.0 FASTY Supraśl 0.0 DRAHLE Sokołda 0.0 JAŁÓW KA Sokołda 0.0 BIAŁYSTOK Biała 0.0 MOŃKI Nereśl 0.0 JABŁONOW O-W YPYCHY Ślina 0.1 ZAW ADY Ślina 0.0 DĘBOW O Biebrza 1.4 OSOW IEC Biebrza 0.0 BURZYN Biebrza 0.0 RÓŻANYSTOK Sidra 0.0 JANÓW Brzozówka 0.0 BIEBRZA Ełk 0.0 RADZIŁÓW W issa 0.2 PTAKI Pisa 0.1 A B C DOBRYLAS Pisa 0.0 TYSZKI-W ĄDOŁOW O Skroda 0.0 ZARUZIE Ruż 0.3 HAJNÓW KA Leśna 0.0 TONKIELE Bug 0.0 BRAŃSK Nurzec 0.0 -
Transformation of the Flow Regime of a Large Allochthonous River in Central Europe—An Example of the Vistula River in Poland
water Article Transformation of the Flow Regime of a Large Allochthonous River in Central Europe—An Example of the Vistula River in Poland Dariusz Wrzesi ´nski and Leszek Sobkowiak * Department of Hydrology and Water Management, Institute of Physical Geography and Environmental Planning, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Krygowskiego str. 10, 61-712 Pozna´n,Poland; [email protected] * Correspondence: [email protected] Received: 31 December 2019; Accepted: 10 February 2020; Published: 12 February 2020 Abstract: Identification of river flow regime and its possible changes caused by natural factors or human activity is one of major issues in modern hydrology. In such studies different approaches and different indicators can be used. The aim of this study is to determine changes in flow regime of the largest river in Poland—the Vistula, using new, more objectified coefficients and indices, based on data recorded in 22 gauges on the Vistula mainstream and 38 gauges on its tributaries in the multi-year period 1971–2010. The paper consists of three main parts: in the first part, in order to recognize changes in the flow regime characteristics along the Vistula, data from gauges located on the river mainstream were analyzed with the help of the theory of entropy. In the second part gauging stations on the Vistula mainstream and its tributaries were grouped; values of the newly introduced pentadic Pardé’s coefficient of flow (discharge) (PPC) were taken as the grouping criterion. In the third part of the study a novel method of determining river regime characteristics was applied: through the recognition of the temporal structure of hydrological phenomena and their changes in the annual cycle sequences of hydrological periods (characteristic phases of the hydrological cycle) on the Vistula River mainstream and its tributaries were identified and their occurrence in the yearly cycle was discussed. -
Wykaz Nazw Wód Płynących List of Names of Flowing Waters
WYKAZ NAZW WÓD PŁYNĄCYCH LIST OF NAMES OF FLOWING WATERS Rodzaj Współrzędne geograficzne Nazwa obiektu Końcówka nazwy obiektu wodnego w dopełniaczu wodnego Recypient szerokość długość Uwagi Name of water object Ending of hydronyms Kind of water Recipient Remarks Geographic coordinates in the genitive case object latitude longitude Abramów -owa potok Ciapków 49°24’42” 19°01’51” Aleksandrowska, -ej, -i struga Widawka 51°18’20” 19°09’56” Struga Aleksandrówka -i potok Brzoskwinka 50°04’13” 19°45’37” Ambrowski Potok -ego -u potok Jasiołka 49°30’18” 21°42’24” Andrzejówka -i potok Sanica 50°34’49” 20°45’37” Aniołowo, Potok Aniołowo, -u struga Elszka 54°05’17” 19°34’55” Antałowski Potok -ego -u potok Czarny Dunajec 49°17’44” 19°51’11” Arciechowski, Kanał -ego, -u kanał Kanał Bieliński 52°22’20” 20°04’54” Arkonka -i struga Odra (Jez. Goplany) 53°28’01” 14°29’58” obszar bezodpływowy Arłamówka -i potok Wyrwa 49°32’57” 22°40’16” Astrabiec -bca potok Panna 49°25’39” 21°42’58” Augustowski, Kanał -ego, -u kanał Strużnica (Gwda) 53°14’22” 16°55’45” Augustowski, Kanał -ego, -u kanał Netta 53°41’03” 22°54’34” odcinek kanału Augustowski, Kanał -ego, -u kanał Netta (jez. Necko) 53°51’49” 22°59’49” odcinek kanału Augustowski, Kanał -ego, -u kanał Czarna Hańcza 53°53’31” 23°24’57” odcinek kanału Awissa -y rzeka Narew 53°00’59” 22°52’33” Baba -y rzeka Sztoła 50°15’33” 19°28’33” Baba -y struga Warta 52°05’53” 17°19’19” Baba -y struga Klaskawska Struga 53°47’29” 18°00’56” Baba -y potok Czerwona 54°13’20” 15°48’46” 1 Rodzaj Współrzędne geograficzne Nazwa obiektu -
Variability of Chemical Weathering Indices in Modern Sediments of the Vistula and Odra Rivers (Poland) - 2453
Nadłonek ‒ Bojakowska: Variability of chemical weathering indices in modern sediments of the Vistula and Odra Rivers (Poland) - 2453 - VARIABILITY OF CHEMICAL WEATHERING INDICES IN MODERN SEDIMENTS OF THE VISTULA AND ODRA RIVERS (POLAND) NADŁONEK, W.1* – BOJAKOWSKA, I.2 1Faculty of Earth Sciences, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland 2Polish Geological Institute – National Research Institute Rakowiecka 4, 00-975 Warszawa, Poland *Corresponding author e-mail: [email protected] (Received 10th Jan 2018; accepted 19th Apr 2018) Abstract. The survey was conducted to determine chemical weathering indices in modern river sediments in Poland. Weathering Index of Parker (WIP), Chemical Index of Alteration (CIA), Vogt’s Residual Index (V), Harnois’s Chemical Index of Weathering (CIW), and Plagioclase Index of Alteration (PIA) was calculated for 178 sediment samples taken from the Vistula River and its tributaries as well as for 114 samples from the Odra River and its tributaries. The indices values were in the ranges: WIP 0.5–20; CIA 4–80; V 0.1–2.8; CIW 4–82; and PIA 3–81.7. The observed variation of values resulted from a varied sample lithology and varied climatic conditions in the Poland area. Sediments from the upper parts of the Odra and the Vistula drainage basins (southwestern part of the country), where pre-Quaternary rocks are exposed, are more resistant to chemical weathering and characteristic for lower susceptibility to leaching of elements. The highest elements losses due to leaching are characteristic for samples taken from the lower parts of the Odra and the Vistula drainage basins, dominated by Quaternary deposits. -
Regulations Governing the Impact of the Aquatic Environment On
Scientific Journal of Silesian University of Technology. Series Transport Zeszyty Naukowe Politechniki Śląskiej. Seria Transport Volume 109 2020 p-ISSN: 0209-3324 e-ISSN: 2450-1549 DOI: https://doi.org/10.20858/sjsutst.2020.109.15 Journal homepage: http://sjsutst.polsl.pl Article citation information: Rutkowski, M. Regulations governing the impact of the aquatic environment on transport in the Kingdom of Poland: removing obstacles from the rivers, creating riverside public spaces and signs and land drainage. Scientific Journal of Silesian University of Technology. Series Transport. 2020, 109, 163-176. ISSN: 0209-3324. DOI: https://doi.org/10.20858/sjsutst.2020.109.15. Marek RUTKOWSKI1 REGULATIONS GOVERNING THE IMPACT OF THE AQUATIC ENVIRONMENT ON TRANSPORT IN THE KINGDOM OF POLAND: REMOVING OBSTACLES FROM THE RIVERS, CREATING RIVERSIDE PUBLIC SPACES AND SIGNS AND LAND DRAINAGE Summary. This work focuses on several aspects of water-related transportation laws as well as drainage law introduced in the Kingdom of Poland before 1860. Thus, while focusing on a) laws concerning the removal of diverse type of obstacles from the rivers used for official navigation; b) establishing of riverside towing routes; c) construction of rivers verst signs on the river banks, this research also deals with the introduction of provisions concerning draining and receiving of waters, which had a huge impact on the road construction and maintenance process in Poland for the first half of the 19th century. Keywords: water-related transportation laws, drainage laws, Kingdom of Poland, 19th century 1. THE LAWS ON LIQUIDATION OF BUILDINGS, WATER FLOATING MILLS AND WEIRS ON RIVERS The program of regulation of rivers of the Kingdom of Poland, initiated at the end of the second decade of the nineteenth century, forced the state to solve the problems of terracing 1 Email:[email protected]. -
Growth Rate of the Chub (Squalius Cephalus) and the Nase (Chondrostoma Nasus) from Raba, Dunajec, and Poprad River Piotr Epler, Michał Nowak, and Włodzimierz Popek
AACL BIOFLUX Aquaculture, Aquarium, Conservation & Legislation International Journal of the Bioflux Society Growth rate of the chub (Squalius cephalus) and the nase (Chondrostoma nasus) from Raba, Dunajec, and Poprad River Piotr Epler, Michał Nowak, and Włodzimierz Popek Department of Ichthyobiology and Fisheries, University of Agriculture in Kraków, ul. T. Spiczakowa 6, 30-199 Kraków, Poland, EU. Corresponding author: M. Nowak, [email protected] Abstract. In presented study growth rate of the chub Squalius cephalus and nase Chondrostoma nasus from Raba, Dunajec, and Poprad River were investigated using a back-scaling method. A total number of 167 chubs and 186 nases were analysed. Age of these fishes varied from 2 to 12 years. Growth rate of fish analysed was high and similar to other results from upper Vistula River drainage. We consider that artificial fry gained from these rivers may contribute declining populations of these two species in other rivers of upper Vistula drainage. Key Words: growth rate, chub, nase, Raba, Dunajec, Poprad. Strzeszczenie. Celem badań było określenie tempa wzrostu klenia Squalius cephalus oraz świnki Chondrostoma nasus z Raby, Dunajca i Popradu metodą odczytów wstecznych. Przebadano łącznie 167 kleni i 186 świnek w wieku od 2 do 12 lat. Tempo wzrostu obu gatunków w badanych rzekach było wysokie i porównywalne z danymi uzyskanymi podczas badań na innych rzekach w rejonie Górnej Wisły. Można przypuszczać, że materiał zarybieniowy wyprodukowany na bazie klenia i świnki z Raby, Dunajca i Popradu z powodzeniem mógłby zostać użyty do wzmocnienia zagrożonych populacji tych ryb w rejonie Górnej Wisły. Słowa kluczowe: tempo wzrostu, kleń, świnka, Raba, Dunajec, Poprad.