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Sedimentation of suspensions in the Vistula River mouth

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The aim of this study was to analyze the variability of the suspension concentration in the area where the Vistula River discharges into the Gulf of Gdańsk. While analyzing the relationship between suspension concentration and the distance from the river mouth and the spatial location in the water column, a number of other important factors were considered, i.e. salinity, temperature, the composition of suspension and in situ hydrodynamic conditions. The samples of surficial sediment were analyzed with regard to the content of organic matter and <0.063 mm size fraction.
Rocznik
Strony
195--201
Opis fizyczny
Bibliogr. 25 poz., wykr.
Twórcy
autor
autor
  • Institute of Oceanography, University of Gdańsk Department of Marine Geology Al. Marszałka Piłsudskiego 46, 81-378 Gdynia, Poland, e.szymczak@ug.edu.pl
Bibliografia
  • 1.Bradtke K. (1997). Simulation of suspended particulate matter transport in the Gulf of Gdańsk during 1996. Oceanological Studies XXVI(4), 123-132.
  • 2.Bradtke K., Latała A. & Czabański P. (1997). Temporal and spatial variations In particle concentrations and size distributions in the Gulf of Gdańsk. Oceanological Studies XXVI(2-3), 39-59.
  • 3.Brański J. (1972). The suspended sediment budget along the Vistula River. Prace PIHM 3. (in Polish).
  • 4.Brański J. (1975). Evaluation of the Vistula river basin denudation based on the results of measurements of suspended sediment. Prace PIHM 6, 1-57. (in Polish)
  • 5.Burska D. Graca B. (2011). Carbon and biogenic substances in suspended matter. In Sz. Uścinowicz (Eds.), Geochemistry of Baltic Sea surface sediments (pp. 326-334), Warsaw: Polish Geological Institute.
  • 6.Cyberska B. & Krzymiński W. (1988). Extension of the Vistula River water in the Gulf of Gdańsk. 16th Conference of Baltic Oceanographers, September 1988 (pp. 290-304). Kiel, Institute of Marine Research, Kiel University.
  • 7.Cyberski J. (1982). Hydrological characteristics. In B. Augustowski (Eds.), The lower Vistula River valley (pp. 103-153). Gdańsk GTN: Ossolineum. (in Polish)
  • 8.Cyberski J., Krężel A. (1993). Influence of the Vistula river on suspended matter content in the Gulf of Gdańsk waters. Studia i Materiały Oceanologiczne 64, Marine Pollution 3, 27-39.
  • 9.Droppo I. G., Jeffries D., Jaskot C. & Backus S. (1998). The prevalence of freshwater flocculation in cold regions: a study from Mackenzie River Delta, Northwest Territories, Canada, Arctic 51(2), 155-164.
  • 10.Eisma D. (1991). Particle size of suspended matter in estuaries. Geo-Marine Letters 11, 147-153.
  • 11.Emeis K., Christiansen C., Edelvang K., Jähmilch 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 the data on origin and properties of material. Journal of Marine System 35, 151-168.
  • 12.Grelowski A. & Wojewódzki T. (1996). The impact of the Vistula River on the hydrological conditions In the Gulf of Gdańsk in 1994. Bulletin of the Sea Fisheries Institute 137, 23-33.
  • 13.Jonasz M. (1983). Particle size distribution in the Baltic. Tellus 35B,5, 346-348.
  • 14.Kranck K. (1979). Dynamics and distribution of suspended particulate matter in the St. Lawrence Estuary. Naturaliste Canada 106, 163-173.
  • 15.Kranck K. (1984). The role of flocculation in the filtering of particulate matter in estuaries. In V. S. Kennedy (Eds.), The estuary as a filter, (pp. 159-175). Orlando, Academic Press.
  • 16.Leeder M. R. (1982). Sedimentology process and products. London, George Allen & Unwin.
  • 17.Łajczak A. (1999). Recent transport and sedimentation of suspended material in the Vistula River and major tributaries. Monografia Komitetu Gospodarki Wodnej PAN 15, Warszawa, Warszawska Drukarnia Naukowa Polskiej Akademii Nauk. (in Polish).
  • 18.Łajczak A. (2005). The role of the Vistula and Odra River in the delivery of suspended sediment to the Baltic Sea. In J.P. Girjatowicz & Cz. Koźmiński (Eds.), Hydrographic and meteorological aspects of research on the Baltic coast and in selected areas of Poland (pp. 61-65), Szczecin, Uniwersytet Szczeciński, Instytut Nauk o Morzu, Polskie Towarzystwo Geograficzne - Oddział Szczeciński. (in Polish).
  • 19.Magnuszewski A. & Soczyńska U. (2001). International dictionary of hydrology. Warsaw, Wyd. Nauk. PWN. (in Polish).
  • 20.Majewski A. (1975). Hydrological characteristics of Polish estuary waters. Prace PIHM 105, 3-35. (in Polish).
  • 21.Nowacki J. & Matciak M. (1996). Hydrological conditions in the area of the Vistula River water front. Przegląd Geofizyczny 41(4), 275-285. (in Polish).
  • 22.Passega R. (1964). Grain-size representation by CM patterns as a geological tool. Journal of Sedimentary Petrology 34, 830-847.
  • 23.Passega R. (1977). Significance of CM diagrams of sediments deposited by suspension. Sedimentology 24, 723-733.
  • 24.Passega R., Byramjee R. (1969). Grain size image of clastic deposits. Sedimentology 13, 830-847.
  • 25.Stoch L. (1974). Clay minerals. Warsaw, Wydawnictwo Geologiczne. (in Polish).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0029-0055
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