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Flood control in the Vistula river delta (Poland)

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EN
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EN
This paper presents past and recent water management in the area called the Vistula Delta Fens (Zulawy Fens). This area (56 x 56 km) is located at the outlet of the Vistula River to the Baltic Sea, at the shore of the Gulf of Gdansk. A large part of the area (30%) is located below sea level as potentially submerged depressions. A multitude of rivers, channels, ditches and pumping stations have been constructed here during several centuries. The area is characterized by highly productive alluvial soils, surface water with a high potential for fish-farming and fishery, and attractive tourist areas at the banks of the rivers and channels. Historically, floods have occurred repeatedly as a result of: i - breaks in the dams along of big rivers, e.g. after heavy rains and high water levels (in summer); ii - dam breaks caused by accumulation of ice-cakes in winter or during spring times; iii - dam breaks after storms on the sea with increasing sea water levels at the river outlets (mainly in winter); iv - overflow of water into flat land after heavy rains followed by slow drainage of water from the fields, ditches, channels and pumping stations (in summer); v - overflow of water into depressions and swamps below sea level after interruptions of, or decreases in, the pump operations at the pumping stations. The EU directive on flood control advises that the member countries should: i - produce maps of the areas vulnerable to floods to facilitate communication and planning; ii - develop management plans for flooding events; iii - exchange experience and codes of good practice during flood; iv - facilitate a close cooperation between the scientific society and politicians in the field of flood protection; v - rise the level of knowledge, communication and awareness among local societies living in areas prone to flooding.
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1--6
Opis fizyczny
Bibliogr. 21 poz., rys.
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autor
  • Department of Sanitary Engineering, Faculty of Civil and Environmental Engineering, Gdansk University of Technology, 80-952 Gdansk, Poland, pkow@pg.gda.pl
Bibliografia
  • Bertram,H. 1907.Die Entwicklung desDeich und Enwässerungswesens. 194 p. Druck der Danziger Allgemainen Zeitung, Danzig.
  • Cebulak, K. 1977. Vistula Delta Fens as an example of polder integration in a develpmental processes of land reclamation [Komasacja polderów jako proces rozwojowy układów wodnomelioracyjnych na przykładzie Żuław Delty Wisły”]. Ph.D.Thesis, Gdansk University of Technology (in Polish).
  • Cebulak, K. 2004a. Chlodniewo - a polder and a pumping station in the Vistula Delta [Chłodniewo - polder i pompownia w delcie Wisły]. Jantarowe Szlaki XLVII, No. 2 (272): 24-27 (in Polish).
  • Cebulak, K. 2004b. Pumping station Oslonka and Marzecin depression in the Vistula Delta [Pompownia Osłonka i Depresja Marzecińska w delcie Wisły]. Jantarowe Szlaki XLVII, No. 3 (273): 5-9 (in Polish).
  • Cebulak, K. 2004c. About the struggle against storms in the Vistula Delta Fens [O walce ze sztormem w delcie Wisły na Żuławach Gdańskich]. Jantarowe Szlaki XLVII, No. 4 (274): 8-12 (In Polish).
  • Cebulak, K. 2005a. Where the Vistula River delta begins [Tam gdzie deltyWisły początek]. Jantarowe Szlaki XLVIII, No. 1 (275): 1-4 (in Polish).
  • Cebulak, K. 2005b. Here the Vistula River ends [Tu gdzie bieguWisły koniec]. Jantarowe Szlaki XLVIII, No. 2 (276): 3-7 (in Polish).
  • Cebulak, K. 2005c. On the lowermost site in Poland [O miejscu najniżej położonym w Polsce]. Jantarowe SzlakiXLVIII,No. 4 (278): 18-21 (in Polish).
  • Cebulak, K. 2006a. On polder depressions in the Vistula Delta [O depresjach polderowych w delcieWisły]. Jantarowe Szlaki XLIX, No. 1 (279): 7-11 (in Polish).
  • Cebulak, K. 2006b. On polder depressions in the Vistula Delta Fens around the Lake Druzno [O depresjach polderowych w delcie Wisły wokół jeziora Drużno]. Jantarowe Szlaki XLIX, No. 3 (281): 9-14 (in Polish).
  • De Bakker, H., B.A. Marsman. 1981. Cresty fields: fields with an elevated centre and lower margins. Boor & Spade 20: 9-38.
  • Kowalik, P. 1980. Water management in the Vistula Delta Fens [Gospodarka wodna na Żuławach Wiślanych]. In: Peribalticum, Investigations on the Baltic Sea Region [Peribalticum, Problemy Badawcze Obszaru Bałtyckiego] (ed. B. Rosa), pp. 125-130. Wydawnictwo GTN, Gdańsk (in Polish).
  • Kowalik, P. 1982. Polders of Vistula River. In: Polders of the World, Proceedings of the International Symposium, Volume I, pp. 58-66. Lelystad, the Netherlands, ILRI, Wageningen.
  • Kowalik, P. 1988.Water management and drainage design of a selected polder. Agricultural Water Management 14: 103-112.
  • Kowalik, P. 2001. Polder water management in the Vistula Delta Fens [Polderowa gospodarka wodna na ˚uławach delty Wisły]. 154 p. Monografia KGW PAN, Warszawa (in Polish).
  • Kowalik, P. 2006. Drainage and capillary rise component in water balance of alluvial soils.AgriculturalWaterManagement 86: 206-211.
  • Kowalik, P. 2007. Water and agriculture - a general overview. Tidskrift, The Royal Swedish Academy of Agriculture and Forestry, 146 (1): 7-10.
  • Majewski, A. 1980. Flood threat and water salinity in the Vistula Delta Fens [Zagrożenie powodziowe i zasolenie wód na Żuławach]. In: Wybrane problemy rolnictwa, gospodarki wodnej i zagospodarowania przestrzennego Żuław delty Wisły - gospodarka wodna, pp. 43-50. Rada Koordynacyjna PAN w Gdańsku, Gdańsk (in Polish).
  • Makowski, J. 1994. The utmost flood catastrophe in the history of Gdansk and the probability for its re-occurrence [Największa katastrofalna powódź w dziejach Gdańska i prawdopodobieństwo jej powtórzenia w obecnych warunkach]. IBW PAN w Gdańsku, Biblioteka Naukowa Hydrotechnika 18: 1-48 (in Polish).
  • Reich, A. 1905. Das Meliorationwesen. 107 p. E. Engelmann, Leipzig.
  • Szukalski, J. 1975. The Vistula Delta Fens [Żuławy Wiślane]. 152 p. Wydawnictwa Szkolne i Pedagogiczne, Warszawa (in Polish).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAR0-0062-0061
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