Article : The application of geomorphological analysis of the Vistula River, Poland in the evaluation of the safety of regulation structures
Authors : Wilmsen, M.Institut fur Palaontologie der Bayerischen Julius-Maximilians-Universitat, Pleicherwall 1, D-97070 Wurzburg, Germany, firstname.lastname@example.org, Chwieduk, E.Institute of Geology, Adam Mickiewicz University, Makow Polnych Str. 16, PL-61-606 Poznan, Poland, email@example.com, Jurewicz, E.Faculty of Geology, University of Warsaw, Al. Żwirki i Wigury 93, PL-02-089 Warsaw, Poland, firstname.lastname@example.org, Niedźwiedzki, G.Department of Paleobiology and Evolution, Faculty of Biology, Warsaw University, S. Banacha Str. 2, PL-02-097 Warszawa, Poland, email@example.com, Anistratenko, O.Institute of Geological Sciences of National Academy of Sciences of the Ukraine, O. Gontchara Str., 55-b, UA-01601, Kiev, Ukraine, firstname.lastname@example.org, Falkowski, T.Geologia, kształtowanie środowiska.,
Abstract : Investigations within the channel zone of the Middle Vistula River have shown the presence of protrusions of the alluvial basement composed of deposits resistant to erosion. On their surface, and in the basal part of the present-day channel facies, occur residual lags composed of gravels and pebbles. These lags indicate exposure of the surface of the alluvial basement in the channel bottom during high-water stages. Protrusions of the resistant alluvial basement often show a complex morphology which influences the course of the thalweg, particularly during floods. The constant trend to concentrate the high-water stream may be the reason for the damage to regulation and flood control system structures. The concentration of the high-water flow causes the formation of specific erosional and depositional forms on the terrace surface. Such forms can thus serve as indicators of the zones of alluvial basement protrusions. The paper presents examples of three reaches of the Middle Vistula River Valley (The Mid-Polish Lowlands).
Publishing house : Faculty of Geology of the University of Warsaw
Publication date : 2007
Number : Vol. 57, no. 3
Page : 377 – 390
Bibliography : DUBICKI, A. 1997. Characteristics of the formation and course of floods and hydrogeological shield in the Odra drainage basin; Flood in 1997, IMGW Warszawa, 59-90. In Polish
DURY, G.H. 1969. Relation of morphometry to run-off frequency. In: R.J. CHORLEY (Ed.), Water, Earth and Man, pp. 419-430. Methuen; London.
FALKOWSKI, E. 1982. Some regularities of the valley floor evolution of the Middle Vistula river valley. In: L. STARKEL, Evolution of the Vistula river valley during the last 15 000 years. Geographical Studies, Special Issue 1, IGiPZ PAN, 9-20.
FALKOWSKI, E. 1990. Morphogenetic classification of river valleys developing in formerly glaciated areas for needs of mathematical and physical modeling in hydro-technical projects. Geographia Polonica, 58, 55-67.
FALKOWSKI, E. (head of a team) 1978. Morpho- and lithogenetic map of the Middle Vistula River valley. Archive of Institute of Hydrogeology and Engineering Geology, Faculty of Geology, Warsaw University. In Polish
FALKOWSKI, T. 2006. Factors of natural stability of the Middle Vistula River channel zones, pp 1-128. Wydawnictwo SGGW; Warszawa. In Polish
FALKOWSKI, T. & ZŁOTOSZEWSKA-NIEDZIAŁEK, H. 2003. Influence of the alluvial basement on the morphology of the Vistula channel in the vicinity of Góra Kalwaria. Przegląd Naukowy Inżynieria i Kształtowanie Środowiska, 12, 2(27), 75-81. In Polish
FRIEDKIN, J.F. 1945. A laboratory Study of the Meandering of Alluvial Rivers; War Department, Corps of Engineers, U.S. Army, Mississippi River Commission, 13, 237-281.
GĘBICA, P. & SOKOŁOWSKI, T. 2001. Sedimentological interpretation of crevasse splays formed during the extreme 1997 flood in the upper Vistula River Valley (south Poland). Annales Societatis Geologorum Poloniae, 71, 53-62.
GILVEAR, D.J. 1999. Fluvial geomorphology and river engineering: future roles utilizing a fluvial hydrosystems framework. Geomorphology, 31, 229-245.
GRZEŚ, M. 1985. The problem of ice-jams and ice-jam floods in the lower Vistula River. Przegląd Geograficzny, 57 (4), 499-525. In Polish
KARABON, J. 1980. Morphogenetic effects of flood flows connected with ice jams in the Middle Vistula River valley. Przegląd Geologiczny, 9, 512-515. In Polish
KERN, K. 1992. Restoration of lowland rivers: the German Experiences. In: P.A. CARLOW., PETTS G.E. (Eds), Lowland Floodplain Rivers. Geomorphological perspectives, pp. 279-297. J. Wiley & Sons Ltd.; Chichester.
KOZARSKI, S. 1983. River channel adjustment to climatic change in west central Poland. In: K. GREGORY (Ed.), Backgound to Palaeohydrology, pp. 355-374. J. Wiley & Sons Ltd.; Chichester.
LARSEN, P. 1994. Restoration of River Corridors: German Experiences. In: P. CARLOW G.E. PETTS (Eds), The River Handbook, pp. 419-440. Blackwell Scientific Publications; Oxford.
OZGA-ZIELIŃSKA, M. 1997. The need of determining the maximal reliable high-water levels caused by the maximal reliable rainfall for Polish rivers. Flood in 1997, IMGW Warszawa, pp. 1-10. In Polish
PRZEDWOJSKI, B., BŁAŻEJEWSKI, R. & PILARCZYK, K.W. 1995. River training techniques, fundamentals, design and applications, pp 1-625. A.A. Balkema.
SARNACKA, Z. 1980. Explanations to the Detailed Geological Map of Poland, scale 1:50 000, Magnuszew sheet; Instytut Geologiczny, Warszawa. In Polish
SARNACKA, Z. & KRYSOWSKA-IWASZKIEWICZ, M., 1974. Eopleistocene deposits in the vicinity of Magnuszew in southern Mazowsze. Z badań czwartorzędu w Polsce, T. 14. Biuletyn Instytutu Geologicznego, 268, 165-187. In Polish
SKIBIŃSKI, J. 1994. An investigation of the relationship between bed load and suspended load in selected Polish rivers. Proceedings of the International Symposium “State-of-the art in river engineering – methods and design philosophies”, Petersburg.
STACHY, J. & BOGDANOWICZ, E. 1997. Causes and course of the flood in July 1997; Flood in 1997, IMGW Warszawa, 195-208. In Polish
STARKEL, L. 1983. The reflection of hydrologic changes in fluvial environment of the temperate zone during the last 15 000 years. In: J. GREGORY (Ed.), Background to Palaeohydrology, pp. 213-234. J. Wiley & Sons Ltd.; Chichester.
STARKEL, L. 1994. Frequency of floods during the Holocene in the Upper Vistula Basin. Studia Geomorphologica Carpatho-Balcanica, 27-28, 3-13.
STARKEL, L. 1995. Reconstruction of hydrological changes between 7000 and 3000 BP in the Upper and Middle Vistula River Basin, Poland. The Holocene, 5 (1), 34-42.
THORNE, C.R. 2002. Geomorphic analysis of large alluvial rivers. Geomorphology, 44, 203-219.
VANDERBERGHE, J. 1995. Timescales, climate and River development. Quaternary Science Reviews, 14, 631-638.
VANDERBERGHE, J. 2002. The relation between climate and river processes, landforms and deposits during the Quaternary; Quaternary International 91, Pergamon, 17-23.
WILIAMS, G.P. & MACKAY, D.K. 1973. The characteristics of ice jams. In: Seminar on Ice Jams in Canada, Technical Memorandum, National Research of Canada, 107, 17-35. Ottawa.
ŻELAZO, J. & POPEK, Z. 2002. Principles of river renaturisation, pp. 1-319. Wydawnictwa SGGW; Warszawa. In Polish
ZIELIŃSKI, T. 2000. Sedimentological results of 1997 and 1998 floods in the Upper Nysa Kłodzka drainage basin. In: S. OSTAFICZUK (Ed.), Dynamic evaluation and forecast of the geological hazards caused by flood, on the example of Nysa Kłodzka, Upper Soła and Upper San-Solinka. Wydawnictwo Instytutu Gospodarki Surowcami mineralnymi i Energią PAN, Kraków, pp. 105-136. In Polish
Qute : Wilmsen, M. ,Chwieduk, E. ,Jurewicz, E. ,Niedźwiedzki, G. ,Anistratenko, O. ,Falkowski, T. ,Falkowski, T. , The application of geomorphological analysis of the Vistula River, Poland in the evaluation of the safety of regulation structures. Acta Geologica Polonica Vol. 57, no. 3/2007