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Sedimentation from suspension and sediment accumulation rate in the River Vistula prodelta, Gulf of Gdańsk (Baltic Sea)

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The River Vistula is one of the largest suppliers of fresh water and terrigenous matter to the Baltic Sea. The impact of this river on the Baltic coastal system and the fate of the sediment delivered to the Gulf of Gdańsk are not well understood. Spatial transport patterns, as well as the settling, deposition and accumulation of the sediments were studied at the Vistula prodelta in different seasons from January 2012 to January 2013. The concentration of suspended matter in the water column was measured with optical methods, the sedimentation rate was determined with sediment traps, and the sediment accumulation rate was estimated using 210Pb dating. Our data shows that the annual supply of sediment to the sediment-water interface exceeds the annual rate of sediment accumulation in the outer Vistula prodelta by a factor of three. Sediment trapping during rough weather showed that significant sediment redeposition was taking place, even at depths of 55 m. The dynamic sedimentary processes occurring in the Vistula prodelta mean that that more than two-thirds of the sediment mass can be remobilized and then redeposited in deeper parts of the Gdańsk Basin.
Czasopismo
Rocznik
Strony
937--950
Opis fizyczny
Bibliogr. 17 poz., rys., wykr.
Twórcy
autor
  • Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30–063 Kraków, Poland
autor
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland
  • Institute of Oceanology, Polish Academy of Sciences, Powstańców Warszawy 55, 81-712 Sopot, Poland
Bibliografia
  • 1. Budillon F., Violante C., Conforti A., Esposito E., Insinga D., Iorio M., Porfido S., 2005, Event beds in the recent prodelta stratigraphic record of the small flood-prone Bonea Stream (Amalfi Coast, Southern Italy), Mar. Geol., 222-223, 419-441, http://dx.doi.org/10.1016/j.margeo.2005.06.013
  • 2. CSO - Central Statistical Office, 2011, Statistical yearbook of the Republic of Poland 2011, CSO, Warsaw, p. 84.
  • 3. Emeis K., Christiansen C., Edelvang K., Jähmlich S., Kozuch J., Laima M., Leipe T., Löffler A., Lund-Hansen L.C., Miltner A., Pazdro K., Pempkowiak J., Pollehne F., Shimmield T., Voss M., Witt G., 2002, Material transport from the near shore to the basinal environment in the southern Baltic Sea. II: Synthesis of data on origin and properties of material, J. Marine Syst., 35,(3-4), 151-168, http://dx.doi.org/10.1016/S0924-7963(02)00127-6
  • 4. Flynn W.W., 1968, The determination of polonium-210 in environmental materials, Anal. Chim. Acta, 43, 221-227, http://dx.doi.org/10.1016/S0003-2670(00)89210-7
  • 5. Keen T.R., Bentley S.J., Chad Vaughan W., Blain C.A., 2004, The generation and preservation of multiple hurricane beds in the northern Gulf of Mexico, Mar. Geol., 210(1-4), 79-105, http://dx.doi.org/10.1016/j.margeo.2004.05.022
  • 6. Koszka-Maroń D., 2009, Facies model of the contemporary delta lobe of the Vistula River, Oceanol. Hydrobiol. St., 38(Suppl. 1), 57-68.
  • 7. Kunzendorf H., Emeis K.-C., Christiansen C., 1998, Sedimentation in the central Baltic Sea as viewed by non-destructive Pb-210-dating, Geogr. Tidsskr., 98, 1-9.
  • 8. Łajczak A., Plit J., Soja R., Starkel L., Warowna J., 2007, Changes of the Vistula river channel and floodplain in the last 200 years, Geogr. Pol., 72(2), 65-87.
  • 9. Pruszak Z., van Ninh P., Szmytkiewicz M., Manh Hung N., Ostrowski R., 2005, Hydrology and morphology of two river mouth regions (temperate Vistula Delta and subtropical Red River Delta), Oceanologia, 47(3), 365-385.
  • 10. Suplińska M.M., Pietrzak-Flis Z., 2008, Sedimentation rates and dating of bottom sediments in the Southern Baltic Sea region, Nukleonika, 53(Suppl. 2), 105-111.
  • 11. Syvitski J.P.M., Kettner A., Correggiari A., Nelson B.W., 2005, Distributary channels and their impact on sediment dispersal, Mar. Geol., 222-223, 75-94, http://dx.doi.org/10.1016/j.margeo.2005.06.030
  • 12. Szczepańska A., Zaborska A., Maciejewska A., Kuliński K., Pempkowiak J., 2012, Distribution and origin of organic matter in the Baltic sea sediments dated with 210Pb and 137Cs, Geochronometria, 39(1), 1-9, http://dx.doi.org/10.2478/s13386-011-0058-x
  • 13. Voss M., Liskow I., Pastuszak M., Rüß D., Schulte U., Dippner J.W., 2005, Riverine discharge into a coastal bay: a stable isotope study in the Gulf of Gdańsk, Baltic Sea, J. Marine Syst., 57(1-2), 127-145, http://dx.doi.org/10.1016/j.jmarsys.2005.04.002
  • 14. Zaborska A., Carrol J., Papucci C., Pempkowiak J., 2007, Intercomparison of alpha and gamma spectrometry techniques used in 210Pb geochronology, J. Environ. Radioactiv., 93(1), 38-50, http://dx.doi.org/10.1016/j.jenvrad.2006.11.007
  • 15. Zajączkowski M., 2002, On the use of sediment traps in sedimentation measurements in glaciated fjords, Pol. Polar Res., 23(2), 161-174.
  • 16. Zajączkowski M., Włodarska-Kowalczuk M., 2007, Dynamic sedimentary environments of an Arctic glacier-fed river estuary (Adventfjorden, Svalbard). I. Flux, deposition, and sediment dynamics, Estuar. Coast. Shelf Sci., 74(1-2), 285-296, http://dx.doi.org/10.1016/j.ecss.2007.04.015
  • 17. Zajączkowski M., Darecki M., Szczuciński W., 2010, Report on the development of the Vistula River plume in the coastal waters of the Gulf of Gdańsk during the May 2010 flood, Oceanologia, 52(2), 311-317, http://dx.doi.org/10.5697/oc.52-2.311
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-cfe469e7-ac87-4b7f-a761-6f766da672fe
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