Long-Term Trends in Water Quality Indices in the Lower Danube and Tributaries in Romania (1996–2017)
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Review of EFAS Progress During 2008
Review of EFAS progress during 2008 Jutta Thielen und FLOODS team EFAS Run and monitored pre-operationally ~ 360 days • some flooding in Sweden in April 2008 • major flooding in Eastern Europe in July 2008 • localised floods in french rivers, Po, Ebro, Romanian rivers, … EFAS FLOOD ALERTS in Mar 2008 From January 2008 onwards EFAS warnings are accessed directly by the partners through the EFAS-IS interface. This interface is password protected and only accessible to EFAS partners. In addition EFAS issues brief alert emails. Activated EFAS Alert issued on – for - confirmed - none Informal EFAS Alert issued on – for - confirmed Flooding Mar Rivers Countries Confirmed 3 Tisza RO,HU not known Active alert email send to MoU partners Informal alert email send because catchment area too small, not part of MoU agreement (but partner has signed an MoU for another river) EFAS FLOOD ALERTS in April 2008 From January 2008 onwards EFAS warnings are accessed directly by the partners through the EFAS-IS interface. This interface is password protected and only accessible to EFAS partners. In addition EFAS issues brief alert emails. Activated EFAS Alert issued on – for - confirmed Flooding April Rivers Cou ntries Confirmed 07 Ebro ES no info RO, HU, 07 Tisza, Prut, Siret MD no info 18 Tisza, Somes RO, HU yes 28 Kalixaelven SE yes Informal EFAS Alert issued on – for - confirmed Flooding April Rivers Cou ntries Confirmed 24 Ljusan SE yes 28 Osterdalalven SE yes 30 Cinca (Ebro) ES yes Active alert email send to MoU partners Informal alert email send because catchment area too small, not part of MoU agreement (but partner has signed an MoU for another river) EFAS FLOOD ALERTS in May 2008 From January 2008 onwards EFAS warnings are accessed directly by the partners through the EFAS-IS interface. -
Study of Heavy Metals Existing in the Danube Wa- Ters in Turnu Severin – Bechet Section
South Western Journal of Vol.2, No.1, 2011 Horticulture, Biology and Environment pp.47-55 P-Issn: 2067- 9874, E-Issn: 2068-7958 STUDY OF HEAVY METALS EXISTING IN THE DANUBE WA- TERS IN TURNU SEVERIN – BECHET SECTION Elena GAVRILESCU University of Craiova, Horticulture Faculty, A.I.Cuza Street, no. 13, Craiova, Romania E-mail: [email protected] Abstract. The Danube River Protection Convention and the Environment Programme of the Danube River Basin aim to the complex assessment of water quality at the national level and of its development trends in order to substantiate the measures and policies to reduce pollution, plus other pri- ority objectives as the quantification of the heavy metals content (Lack 1997). The monitored sections in the study, respectively Turnu Severin - Calafat - Bechet were part of the TNMN network for tracking the Danube water quality (Harmancioglu et al. 1997).The heavy metals are from both the upstream of Turnu Severin and from the Jiu River. After the study conducted in 2007-2009 there were found in some metals significant amounts of nickel, copper, chromium, arsenic and lead in particular. Key words: monitoring, heavy metals, aquatic ecosystem, water pollution, the Danube INTRODUCTION Danube represents the biggest water resource for Romania being more than double (85x109 cm/year) in comparison with the inland water (river and lakes), which represents about 40x109 cm/year, but the possibilities of their use in natural regime are limited because of different technical reasons (Botterweg & Rodda 1999). Even so the importance of the Danube health is of major concern for Romania as well as for other countries. -
Bitterling Populations in the Sighişoara-Târnava Mare Natura 2000 Site
Management of Sustainable Development Sibiu, Romania, Volume 8, No.1, June 2016 10.1515/msd-2016-0001 BITTERLING POPULATIONS IN THE SIGHI ŞOARA-TÂRNAVA MARE NATURA 2000 SITE ‒ A SUPPORT SYSTEM FOR MANAGEMENT DECISIONS Angela, CURTEAN-BĂNĂDUC 1, Ioana-Cristina, CISMA Ș2 and Doru, BĂNĂDUC 3 1"Lucian Blaga" University of Sibiu, Sibiu, Romania, [email protected] 2"Lucian Blaga" University of Sibiu, Sibiu, Romania, [email protected] 3"Lucian Blaga" University of Sibiu, Sibiu, Romania, [email protected] ABSTRACT : The predominant threats to the Bitterling populations in the Sighi şoara-Târnava Mare Natura 2000 site are the hydro technical modifications of the river channels, organic contamination and illegal fishing. ADONIS:CE is applied commonly for business processes modelling, however, in this study case was applied in an ecology/biology sphere of interest. The authors acquired a Bitterling model which contained all of the identified habitat species’ necessities, the specific indicators that give good preservation status and the present pressures and threats. The keeping of the riverbed morphodynamics is especially necessary – the meanders existence is significant for the aquatic mollusc species which are existing in the inner U shape sectors of the lotic systems. The sectors, where the sand and mud are relatively fixed, give appropriate habitats for molluscs which is valuable for the reproduction of Bitterling. The preserving of the present water oxygenation and regime of liquid flows, and the prevention of the sediments deposition rate in the aquatic habitats are needed too for the molluscs’ existence. The sediments exploitation in these lotic systems should be realised in relation with the natural rate of renewal and at sites at a distance over five km between them. -
Settlement History and Sustainability in the Carpathians in the Eighteenth and Nineteenth Centuries
Munich Personal RePEc Archive Settlement history and sustainability in the Carpathians in the eighteenth and nineteenth centuries Turnock, David Geography Department, The University, Leicester 21 June 2005 Online at https://mpra.ub.uni-muenchen.de/26955/ MPRA Paper No. 26955, posted 24 Nov 2010 20:24 UTC Review of Historical Geography and Toponomastics, vol. I, no.1, 2006, pp 31-60 SETTLEMENT HISTORY AND SUSTAINABILITY IN THE CARPATHIANS IN THE EIGHTEENTH AND NINETEENTH CENTURIES David TURNOCK* ∗ Geography Department, The University Leicester LE1 7RH, U.K. Abstract: As part of a historical study of the Carpathian ecoregion, to identify salient features of the changing human geography, this paper deals with the 18th and 19th centuries when there was a large measure political unity arising from the expansion of the Habsburg Empire. In addition to a growth of population, economic expansion - particularly in the railway age - greatly increased pressure on resources: evident through peasant colonisation of high mountain surfaces (as in the Apuseni Mountains) as well as industrial growth most evident in a number of metallurgical centres and the logging activity following the railway alignments through spruce-fir forests. Spa tourism is examined and particular reference is made to the pastoral economy of the Sibiu area nourished by long-wave transhumance until more stringent frontier controls gave rise to a measure of diversification and resettlement. It is evident that ecological risk increased, with some awareness of the need for conservation, although substantial innovations did not occur until after the First World War Rezumat: Ca parte componentă a unui studiu asupra ecoregiunii carpatice, pentru a identifica unele caracteristici privitoare la transformările din domeniul geografiei umane, acest articol se referă la secolele XVIII şi XIX când au existat măsuri politice unitare ale unui Imperiu Habsburgic aflat în expansiune. -
Introduceţi Titlul Lucrării
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Annals of the University of Craiova - Agriculture, Montanology, Cadastre Series Analele Universităţii din Craiova, seria Agricultură – Montanologie – Cadastru (Annals of the University of Craiova - Agriculture, Montanology, Cadastre Series) Vol. XLIII 2013 RESEARCH ON THE IDENTIFICATION AND PROMOTION OF AGROTURISTIC POTENTIAL OF TERRITORY BETWEEN JIU AND OLT RIVER CĂLINA AUREL, CĂLINA JENICA, CROITORU CONSTANTIN ALIN University of Craiova, Faculty of Agriculture and Horticulture Keywords: agrotourism, agrotourism potential, agrotouristic services, rural area. ABSTRACT The idea of undertaking this research emerged in 1993, when was taking in study for doctoral thesis region between Jiu and Olt River. Starting this year, for over 20 years, I studied very thoroughly this area and concluded that it has a rich and diverse natural and anthropic tourism potential that is not exploited to its true value. Also scientific researches have shown that the area benefits of an environment with particular beauty and purity, of an ethnographic and folklore thesaurus of great originality and attractiveness represented by: specific architecture, traditional crafts, folk techniques, ancestral habits, religion, holidays, filled with historical and art monuments, archeological sites, museums etc.. All these natural and human tourism resources constitute a very favorable and stimulating factor in the implementation and sustained development of agritourism and rural tourism activities in the great and the unique land between Jiu and Olt River. INTRODUCTION Agritourism and rural tourism as economic and socio-cultural activities are part of protection rules for built and natural environment, namely tourism based on ecological principles, became parts of ecotourism, which as definition and content goes beyond protected areas (Grolleau H., 1988 and Annick Deshons, 2006). -
Exceptional Floods in the Prut Basin, Romania, in the Context of Heavy
1 Exceptional floods in the Prut basin, Romania, in the context of 2 heavy rains in the summer of 2010 3 4 Gheorghe Romanescu1, Cristian Constantin Stoleriu 5 Alexandru Ioan Cuza, University of Iasi, Faculty of Geography and Geology, Department of 6 Geography, Bd. Carol I, 20 A, 700505 Iasi, Romania 7 8 Abstract. The year 2010 was characterized by devastating flooding in Central and Eastern 9 Europe, including Romania, the Czech Republic, Slovakia, and Bosnia-Herzegovina. This 10 study focuses on floods that occurred during the summer of 2010 in the Prut River basin, 11 which has a high percentage of hydrotechnical infrastructure. Strong floods occurred in 12 eastern Romania on the Prut River, which borders the Republic of Moldova and Ukraine, and 13 the Siret River. Atmospheric instability from 21 June-1 July 2010 caused significant amounts 14 of rain, with rates of 51.2 mm/50 min and 42.0 mm/30 min. In the middle Prut basin, there are 15 numerous ponds that help mitigate floods as well as provide water for animals, irrigation, and 16 so forth. The peak discharge of the Prut River during the summer of 2010 was 2,310 m3/s at 17 the Radauti Prut gauging station. High discharges were also recorded on downstream 18 tributaries, including the Baseu, Jijia, and Miletin. High discharges downstream occurred 19 because of water from the middle basin and the backwater from the Danube (a historic 20 discharge of 16,300 m3/s). The floods that occurred in the Prut basin in the summer of 2010 21 could not be controlled completely because the discharges far exceeded foreseen values. -
The Danube River Basin District
/ / / / a n ï a r k U / /// ija ven Slo /// o / sk n e v o l S / / / / a r o G a n r C i a j i b r S / / / / a i n â m o R / / / / a v o d l o M / / / / g á z s r ro ya ag M The /// a / blik repu Danube River Ceská / Hrvatska //// osna i Hercegovina //// Ba˘lgarija /// / B /// Basin District h ic e River basin characteristics, impact of human activities and economic analysis required under Article 5, Annex II randr Annex III, and inventory of protected areas required under Article 6, Annex IV of the EU Water Framework Directivee (2000/60/EC) t s Part A – Basin-wide overviewÖ / / Short: “Danube Basin Analysis (WFD Roof Report 2004)” / / d n a l h c s t u e D / / / / The complete report consists of Part A: Basin-wide overview, and Part B: Detailed analysis of the Danube river basin countries 18 March 2005, Reporting deadline: 22 March 2005 Prepared by International Commission for the Protection of the Danube River (ICPDR) in cooperation with the countries of the Danube River Basin District. The Contracting Parties to the Danube River Protection Convention endorsed this report at the 7th Ordinary Meeting of the ICPDR on December 13-14, 2004. The final version of the report was approved 18 March 2005. Overall coordination and editing by Dr. Ursula Schmedtje, Technical Expert for River Basin Management at the ICPDR Secretariat, under the guidance of the River Basin Management Expert Group. ICPDR Document IC/084, 18 March 2005 International Commission for the Protection of the Danube River Vienna International Centre D0412 P.O. -
S E R B I a Knin ˆ Bor
CENTRAL BALKAN REGION 16 18 20 22 Nagykanizsa Tisza Hódmezövásárhely Dravaˆ Kaposvár Szekszárd SLOVENIA P Celje Varazdin A Szeged N H U N G A R Y N Arad O N Pécs 46 I 46 A Danube Subotica Mures N Bjelovar B A Zagreb S Kikinda Deva I Tisa N Sombor Timisoara¸ Hunedoara T N A Karlovac B A R O M A N I A Sisak C R O A T I A Osijek Vojvodina Petroseni Sava Vukovar Zrenjanin S Resita¸ ¸ LP Novi Sad A ˆ N IA Slavonski Brod Federation of Bosnia Vrsac N and Herzegovina Danube A Tirgu-Jiu V Prijedor Ruma L ˆ ˆ ˆ Y S Bihac Republika Srpska Brcko Pancevo N A D Banja Luka Doboj Sava R Drobeta-Turnu Bijeljina Sabac Belgrade Danube T Severin Udbina I Smederevo Kljuc Tuzla N B O S N I A A A N D Valjevo Danube Zenica Drina R S e r b i a Knin ˆ Bor 44 H E R Z E G O V I N A Srebrenica Kragujevac 44 Glamoc I ˆ Vidin Calafat C Sarajevo Uzice Paracin´ Šibenik Pale Kraljevo Federation of Bosnia ˆ Morava D and Herzegovina Gorazde Split A ˆ L A M Foca Montana A T L Nis´ B I Republika A Mostar L A Priboj K P Srpska A ˆ Ta ra Novi Pazar N M Ploce S Bijelo TS. Piva Polje Neum Kosovska Mitrovica Berane Montenegro BULG. Nikšic´ Pec´ Priština Dubrovnik Kosovo Vranje Pernik CROATIA Podgorica Dakovica Gnjilane NORTH (Djakovica) Uroševac Kotor ALBANIAN Kyustendil ALPS Prizren A Lake I N Kumanovo Scutari N Kukës A 42 Shkodër L Tetovo Skopje 42 Bar P R A S Gostivar Štip Shëngjin Titov Veles A d r i a t i c Peshkopi THE FORMER YUGOSLAV REPUBLIC OF MACEDONIA Vardar Strumica Barletta S e a Tirana Prilep Lake Durrës Ohrid I T A L Y Bari Elbasan Ohrid Bitola Republic boundary -
Ukraine Facts Figures
Danube Facts and Figures: Ukraine Danube Facts and Figures Ukraine (September 2015) General Overview Three sub-basins of the Danube are partly located in Ukraine - the Tisza, Prut and Siret basins, as well as part of the Danube Delta. Furthermore, 2.7 million people live in the Ukrainian part of the Danube Basin, which is 3.3% of the total Danube Basin District. Ukraine has been a Signatory State to the Danube River Protection Convention since 1994. The Convention was ratified by the Ukrainian Parliament in 2002 and is now a law. Topography The largest part of the Tisza Basin is located in the Ukrainian Carpathian Mountains, which are middle-height mountains of 1,000 to 1,200 metres above sea level - the highest peaks reach 2,000 metres. The main mountain ranges are located longitudinally from north-west to south-east and divided by transverse river valleys. One third of the Tisza Basin is located in the Zakarpattya Lowland, which forms part of the Great Hungarian Plain and the Pannonian Plain, with dominating heights of 120-180 metres above sea-level. Like the Tisza Basin, the Prut and Siret Basins are located mainly in the Ukrainian Carpathians, but in the eastern hills. The source of the Prut is in the Chernogora Mountains at around 1,600 metres above sea-level. The total area of the sub- basins is 30,520km 2, which makes up only 3.8% of the total Danube Basin area and 5.4% of the Ukrainian territory. The Danube itself comes through the lower part of Ukraine; its length in the mouth is 174km. -
The Excesively Rainy Summer of 2018 in South-Western Romania in the Context of Climate Changes
RISCURI ŞI CATASTROFE, NR. XVIII, VOL. 24, NR. 1/2019 THE EXCESIVELY RAINY SUMMER OF 2018 IN SOUTH-WESTERN ROMANIA IN THE CONTEXT OF CLIMATE CHANGES I. MARINICĂ5, ANDREEA MARINICĂ6 Abstract. The summer of 2018 was warm and extremely rainy. The rainy summer feature is due to the first two months of summer in which the monthly average rainfall (calculated for the whole region) was very high. In June the monthly average monthly rainfall was 162.8 l / m2, and its percentage deviation from normal was 93.4% (almost twice the normal) and in July the average monthly quantities for the whole region was 138.0 l / m2 and its percentage deviation from normal 112.4% (more than twice the normal). The average air temperature average was 21.9°C and its deviation from normal 1.2°C, which shows that the summer was warm. The dry and warm weather, usually in summer in Oltenia, started on 2 June, 1818 and extended throughout autumn, seriously affecting the beginning of the 2018-2019 agricultural year by delaying the establishment of autumn crops. Throughout the summer there were 7 overly rainy intervals, which amounted to over 15 days of rain. Due to synoptic situations, usually unusual summer, which caused torrential rains, the summer of 2018 changed the way to achieve seasonal climatic forecasts at three-month intervals at 4-week intervals. This is still a confirmation of the ongoing climate change across the planet, and summer 2018 will remain in the history of the climate as the one that has changed the seasonal weather forecast reference range. -
Study for Evaluating the Water Quality of the Jiu River in Gorj County
Annals of the „Constantin Brancusi” University of Targu Jiu, Engineering Series , No. 4/2020 STUDY FOR EVALUATING THE WATER QUALITY OF THE JIU RIVER IN GORJ COUNTY DELIA NICA-BADEA*, Constantin Brancusi University Targu – Jiu, Romania ANIELA BALACESCU, Constantin Brancusi University Targu – Jiu, Romania * Corresponding author: [email protected] Abstract: This paper presents a study conducted in the autumn season 2018, whose main objective was to assess the water quality of the Jiu River in the administrative territory of Gorj County. Based on the physico-chemical parameters determined in three sampling points on the direction of river flow, we analyzed the data and established the water quality class from an ecological point of view by reference to elements and physico-chemical quality standards according to O 161/2006. From the perspective of ecological status, most parameters fall into quality class I for all three water segments, except: P-PO4 class IV. The WQI values calculated for each parameters vary depending on the analyzed segment and fall into different quality classes: Excellent (DO, BOD, Nitrate, Phosphates, pH); Good (TDS; BOD –SJ3); Bad (Temperature); Very Bad (Turbidity). The general WQI varies very little, respectively: 79, 78, 77, falling within the Good quality range, decreasing towards the southern segment of the Jiu River. The assessment of the quality of water bodies described in this study, reveals that the Jiu River is a clean body of water, a fact which has also been confirmed by national and European authorities in the periodic in recent reports. Keywords: Jiu River, Water quality parameters, Ecological status, Water Quality Index 1. -
Thermo-Mineral Waters from the Cerna Valley Basin (Romania)
Studia Universitatis Babeş-Bolyai, Geologia, 2008, 53 (2), 41 – 54 Thermo-mineral waters from the Cerna Valley Basin (Romania) Ioan POVARĂ1*, Georgel SIMION2† & Constantin MARIN1 1„Emil Racoviţă” Institute of Speleology, Frumoasă 31, 78114, Bucharest, Romania 2 S.C. Prospecţiuni SA, Caransebeş 1, 12271, Bucharest, Romania († deceased) Received: May 2008, accepted November 2008 Available online November 2008 ABSTRACT. In the Cerna Valley basin, located southwest of the Southern Carpathians and upstream from the confluence of Cerna with Belareca, an aquifer complex has developed. The basin is strongly influenced by hydrogeothermal phenomena, acting within two major geological structures, the Cerna Syncline and the Cerna Graben. The complex consists mainly of Jurassic and Cretaceous carbonate rocks, as well as the upper part of the Cerna Granite that is highly fractured, tectonically sunken into the graben. The geothermal investigations have shown the existence of some areas with values of the geothermal gradient falling into the 110-200ºC/km interval, and temperatures of 13.8-16ºC at the depth of 30 m. The zone with the maximal flux intensity is situated between the Băile Herculane railway station and the Crucea Ghizelei Well, an area where 24 sources (10 wells and 14 springs) are known. The geothermal anomaly is also extended to the south (Topleţ), north (Mehadia) and NE (Piatra Puşcată), a fact, which is stressed by the existence of hypothermal springs with low mineralization. The physical-chemical parameters of the sources show a strong N-S variability. At the entire thermo-mineral reservoir scale, the temperature of the water sources, the total mineralization, and the H2S quantity are increasing from the north to the south, and the pH and natural radioactivity are following the same trend.