Dynamics of the Kopa?ki Rit (Croatia) wetland floodplain water regime

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• 作者：Lidija Tadi? (1)
  Ognjen Bonacci (2)
  Tamara Dadi? (1)
  
• 关键词：Wetland ; Floodplain ; Water level ; Water regime ; Kopa?ki Rit
• 刊名：Environmental Earth Sciences
• 出版年：2014
• 出版时间：April 2014
• 年：2014
• 卷：71
• 期：8
• 页码：3559-3570
• 全文大小：10,433 KB
• 参考文献：1. Altdorff D, Epting J, Kruk J, Dietrich P, Huggenberger P (2013) Delineation of fluvial sediment architecture of subalpine riverine systems using noninvasive hydrogeophysical methods. Environ Earth Sci 69(2):633-44. doi:10.1007/s12665-013-2304-4 CrossRef
  2. Amoros C, Bornette G (2002) Connectivity and biocomplexity in waterbodies of riverine floodplains. Freshw Biol 47:517-39 CrossRef
  3. Azevedo TM, Goncalves MA (2009) Geochemistry of core sediments from the Middle Tagus alluvial plain (Portugal) since the last glacial: using background determination methods to outline environmental changes. Environ Earth Sci 59(1):191-04. doi:10.1007/s12665-009-0016-6 CrossRef
  4. Bari?i?-Lasovi? A (2012) Impact of agricultural drainage system on water quality on Kopa?ki Rit. Master Thesis, University of Osijek
  5. Bonacci O (2010) Analiza nizova srednjih godi?njih temperatura zraka u Hrvatskoj [Analyses of mean annual air temperature series in Croatia]. Gra?evinar 62(9):781-91 (Croatian)
  6. Bonacci O, Trnini? D, Roje-Bonacci O (2008) Analyses of the water temperature regime of the Danube ant its tributaries in Croatia. Hydrol Process 22(7):1014-021 CrossRef
  7. Bridge JS (2003) Rivers and Floodplains—Forms, processes, and sedimentary record. Blackwell Pbl, Malden
  8. Brookes A (1994) River channel change. In: Calow P, Petts GE (eds) The rivers handbook, vol 2. Blackwell Sci Pbl, Oxford, pp 55-5 CrossRef
  9. Castaldelli G, Colombani N, Vincenzi F (2013) Linking dissolved organic carbon, acetate and denitrification in agricultural soils. Environ Earth Sci 68(4):939-45. doi:10.1007/s12665-012-1796-7 CrossRef
  10. ?erba D, Bogut I, Vidakovi? J, Palijan G (2009) Invertebrates in Myriophyllum spicatum L. stands in Lake Sakada?, Croatia. Ekologia—Ecology 28:94-05
  11. ?urokovi? Z, Brni?-Levada D (1999) Utjecaj izvedenih hidrotehni?kih radova na vodne resurse u Kopa?kom ritu [Influence of hydrotechnical works on Kopa?ki Rit water resources]. In: Proceedings of 2nd Croatian conference on water, Dubrovnik, pp 661-66 (Croatian)
  12. Elwaseif M, Ismail A, Abdalla M, Abdel-Rahman M, Hafez MA (2012) Geophysical and hydrological investigations at the west bank of Nile River (Luxor, Egypt). Environ Earth Sci 67(3):911-21. doi:10.1007/s12665-012-1525-2 CrossRef
  13. Franz C, Makeschin F, Roig H et al (2012) Sediment characteristics and sedimentations rates of a small river in Western Central Brazil. Environ Earth Sci 65(5):1601-611. doi:10.1007/s12665-011-1498-6 CrossRef
  14. Garbrecht J, Fernandez GP (1994) Visualization of trends and fluctuations in climatic records. Water Resour Bull 30(2):297-06 CrossRef
  15. Hein T, Baranyi C, Herndl G, Wanek W, Schiemer F (2003) Allochthonous and autochthonous particulate organic matter in floodplains of the River Danube: the importance of hydrological connectivity. Freshw Biol 48:220-32 CrossRef
  16. Horvati? J, Per?i? V, Mihaljevi? M (2006) Bioassay method in evaluation of trophic conditions and nutrient limitation in the Danube wetland waters (1388-426 rkm). Hydrobiologia 563:453-63 CrossRef
  17. Kent DM (2001) Applied Wetlands Science and Technology, 2nd edn. CRC Press, Boca Ratom
  18. Lang M, McCarty G, Oesterling R, Yeo L-Y (2012) Topographic metrics for improved mapping of forestry wetlands. Wetlands. doi:10.1007/s13157-012-0359-8
  19. Magner J, Hansen B, Sundby T, Kramer G, Wilson B, Nieber J (2012) Channel evolution of Des Moines Lobe till drainage ditches in southern Minnesota (USA). Environ Earth Sci 67(8):2359-369. doi:10.1007/s12665-012-1682-3 CrossRef
  20. Mari?i? S (2005) Analyses of one of the rare natural retention in the Middle Danube. In: Proceedings of the Ninth international symposium on water management and hydraulic engineering. Ottenstein, Austria, pp 383-95
  21. Merz C, Winkler A, Pekdeger A (2009) Trace elements in streambed sediments of floodplains: consequences for water management measures. Environ Earth Sci 59(1):25-8. doi:10.1007/s12665-009-0001-0 CrossRef
  22. Mihaljevi? M et al (1999) Kopa?ki Rit—overview of investigations and bibliography. Croatian academy of science and art, Osijek
  23. Mihaljevi? M, Stevi? F, Horvati? J, Hackenberger Kutuzovi? B (2009) Dual impact of the flood pulses on the phytoplankton assemblages in a Danubian floodplain lake (Kopa?ki Rit Nature Park. Croatia). Hydrobiologia 618:77-8 CrossRef
  24. Palijan G, Fuks D (2006) Alteration of factors affecting bacterioplankton abundance in the Danube River floodplain (Kopa?ki Rit. Croatia). Hydrobiologia 560:405-15 CrossRef
  25. Per?i? V, Horvati? J (2011) Spatial distribution of nutrient limitation in the Danube River floodplain in relation to hydrological connectivity. Wetlands 31(5):933-44. doi:10.1007/s13157-011-0208-1 CrossRef
  26. Per?i? V, Horvati? J, Mihaljevi? M (2005) Bioassay method in the trophic evaluation of a wetland area-case study in the Danubian region (1426-388 rkm). Period Biol 107:293-98
  27. Per?i? V, Horvati? J, Has-Sch?n E, Bogut I (2009) Changes in N and P limitation induced by water level fluctuations in Nature Park Kopa?ki Rit (Croatia): nutrient enrichment bioassay. Aquat Ecol 43:27-6 CrossRef
  28. Rodrigues ASL, Malafia G, Costa AT, Nalini HA (2013) Evaluation of the mineral exploration influence on sediment composition in the Gualaxo do Norte River Basin (MG-Brazil) based on geochemical and stratigraphic data. Environ Earth Sci 68(4):965-72. doi:10.1007/s12665-012-1799-4 CrossRef
  29. Schwarz U (2006) Genesis and typology of riparian and fluvial landforms of the Kopa?ki Rit within the Danube floodplain corridor in Croatia and Serbia. In: Proceedings 36th international conference of IAD. Austrian Committee Danube Research, Vienna. ISBN 13: 978-3-9500723-2-7, pp 318-21
  30. Singh CK, Satyanarayan S, Singh A, Mukherjee S (2011) Quantitative modeling of groundwater in Satluj River basin of Rupnagar district of Punjab using remote sensing and geographic information system. Environ Earth Sci 62(4):871-81. doi:10.1007/s12665-010-0574-7 CrossRef
  31. Slowik M, Sobczynski T, Mlynarczyk Z (2010) Types of sedimentary environment in alluvial sediments distinguished on the basis of its chemical constitution: the example of the lower course of the Obra river (Western Poland). Environ Earth Sci 59(5):957-66. doi:10.1007/s12665-009-0089-2 CrossRef
  32. Tadi? Z, Bonacci O, Radeljak I, Tadi? L (2003) Vodni re?im Parka prirode Kopa?ki rit [Water regime of Kopa?ki Rit Nature Park]. In: Proceedings of 3rd Croatian conference on water. Osijek, pp 941-50 (Croatian)
  33. Tadi? L, Dadi? T, Bara? B (2013) Flood frequency modelling of Kopa?ki Rit Nature Park. Tehni?ki vjesnik-Technical Gazzete 20(1):51-7
  34. Thoms MC, Southwell M, McGinness HM (2005) Floodplain-river ecosystems: fragmentation and water resources development. Geomorphology 71:126-38 CrossRef
  35. Vandeberg GS, Martin CW, Pierzynski GM (2011) Spatial distribution of trace elements in floodplain alluvium of the upper Blackfoot River, Montana. Environ Earth Sci 62(7):1521-534. doi:10.1007/s12665-010-0637-9 CrossRef
  36. Walling DE, Webb BW (1992) 3: Water quality I. Physical characteristics. In: Calow P, Petts GE (eds) The River Handbook. Blackwell Sci, Oxford, pp 48-2
  37. Zglobicki W, Lata L, Plak A, Reszka M (2011) Geochemical and statistical approach to evaluate background concentrations of Cd, Cu, Pb and Zn (case study: Eastern Poland). Environ Earth Sci 62(2):347-55. doi:10.1007/s12665-010-0529-z CrossRef
  
• 作者单位：Lidija Tadi? (1)
  Ognjen Bonacci (2)
  Tamara Dadi? (1)
  
  1. Faculty of Civil Engineering, University of Osijek, Crkvena 21, 31000, Osijek, Croatia
  2. Faculty of Civil Engineering, Architecture and Geodesy, University of Split, Matice hrvatske 15, 21000, Split, Croatia
  
• ISSN：1866-6299

文摘

Kopa?ki Rit Nature Park is part of the Danube River natural floodplain and one of the last oases of wild life in the Danube River Basin. Due to its extraordinary value, it was inscribed on the list of Wetlands of International Importance in 1993. More than 2,000 species have been registered in this area, which consists of lakes, canals, grassland, marshland and forests. Even the number of investigations which have been performed on its biological and ecological features, hydrological and water resources characteristics, as a prerequisite for ecohydrological analyses, are still rather unknown in the scientific community. Mainly the Danube River and partly the River Drava cause flooding of Kopa?ki Rit and inundations enter the area from both the northern and southern parts. Results of hydrological and meteorological analysis show a decreasing trend of both mean and minimum, annual water levels in the Rivers Drava and Danube (respectively 1.8 and 1.38?cm/year). These reductions in water level can reduce the replenishment periods of Kopa?ki Rit Nature Park. In addition, a significant rise of mean annual air temperature and consequently water temperature (data 1988-011) may be causing increasing evapotranspiration and loss of water within Kopa?ki Rit. But an encouraging counteracting finding is that, the results of frequency analysis show, even a discharge of 5-years-return period on the River Danube inundates 70?% of the Danube floodplain and Kopa?ki Rit Nature Park.