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This study presents the diversity of sediments forming sand bars located in the Vistula channel between 695 km and 775 km of its course. The analysed section of the Vistula channel is located in the Toruń Basin. During the fieldwork carried out on 20-21 September 2011, 45 channel bars were identified and sampled. The collected samples were analysed in a laboratory. The obtained results were presented in the form of figures and graphics. The research related to the Vistula bed load performed to date was based on various research methods. The authors applied the sampling method used by Z. Babiński (1992). It was employed also by other authors (Habel, 2013). The obtained results were referred to other studies and the findings clearly indicate that such detailed research must be conducted along the whole middle section of the Lower Vistula valley.
Czasopismo
Rocznik
Tom
Strony
97--104
Opis fizyczny
Bibliogr. 39 poz., rys., tab.
Twórcy
autor
- Kazimierz Wielki University, Faculty of Physical Education, Health and Tourism, Institute of Geography
autor
- Kazimierz Wielki University, Faculty of Physical Education, Health and Tourism, Institute of Geography
Bibliografia
- 1. Andrzejewski L., 1995. Genesis of the fluvial system of the lower Vistula river based on the selected side valleys. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part V. Geographical Studies Special Issue No. 8, 139-156.
- 2. Babiński Z., 1979. Wstępna charakterystyka utworów powierzchniowych koryta Wisły poniżej stopnia we Włocławku. Gospodarka Wodna 1, 10-12 [In Polish].
- 3. Babiński Z., 1982. The influence of the water dam in Włocławek of fluvial processes of the Vistula River. Dokumentacja Geograficzna 1-2. Instytut Geografii i Przestrzennego Zagospodarowania PAN, Warszawa [In Polish with English summary].
- 4. Babiński Z., 1984. The effects of human activity on changes in the lower Vistula channel. Geographia Polonica 50, 271–282.
- 5. Babiński Z., 1990. Charakterystyka litologiczna łach koryta dolnej Wisły. Gospodarka Wodna 12, 266-270 [In Polish].
- 6. Babiński Z., 1992. The presentday fluvial processes of the lower Vistula River. Prace Geograficzne 157. Instytut Geografii i Przestrzennego Zagospodarowania PAN, Warszawa [In Polish with English summary].
- 7. Babiński Z., 1999. Changes of clastic rock-debris transportation in the lower Vistula river as a result of water regulation works. Acta Universitatis Nicolai Copernici, Geografia XXIX, Nauki Matematyczno-Przyrodnicze, Toruń, 327-335 [In Polish with English abstract].
- 8. Banach M., 1977. The growth of landslides on the right-bank slope of the Vistula River between Dobrzyń and Włocławek. Prace Geograficzne 124, Instytut Geografii i Przestrzennego Zagospodarowania PAN, Warszawa [In Polish with English summary].
- 9. Bluck B.J., 1987. Bed forms and clast size changes in gravel-bed rivers. [In:] K. Richards (Eds.), River channels: Environment and processes. Basil Blackwell Inc., New York, 159-178.
- 10. Born A., 1958. Wleczenie materiału dennego w korytach rzek i potoków. Wiadomości Służby Hydrologicznej i Meteorologicznej PIHM 3, Warszawa, 3-29 [In Polish].
- 11. Cyberski J., Grześ M., Gutry-Korycka M., Nachlik E., Kundzewicz Z.W., 2006. History of floods on the River Vistula. Hydrological Sciences Journal 51(5), 799-817.
- 12. Falkowski T., 2007. The application of geomorphological analysis of the Vistula River Poland in the evaluating of the safety of regulation structures. Acta Geologica Polonica 57(3), 377-390.
- 13. Gierszewski P., 1991. Ice-jam deformations of the Vistula flood-plain in the Ciechocinek region. Przegląd Geograficzny 43, 1-2, 133-141 [In Polish with English Abstract].
- 14. Gierszewski P.J., Szmańda J.B., Luc M., 2015. Changes of Vistula River channels pattern caused by Włocławek Dam functioning based on the analysis of aerial photographs. Przegląd Geograficzny 87(3), 517-533 [In Polish with English abstract].
- 15. Giriat D., 2003. Wpływ stopnia wodnego we Włocławku na wybrane cechy teksturalne osadów korytowych na odcinku Włocławek-Grudziądz. PhD thesis (unpublished), University of Warsaw Press [In Polish].
- 16. Gorączko M., 2013. Variability of ice phenomena on the Vistula River in the vicinity of Bydgoszcz. Przegląd Naukowy – Inżynieria i Kształtowanie Środowiska 62, 382-388 [In Polish with English Abstract].
- 17. Gorączko M., 2015. The intensity of shipping traffic at Bydgoszcz section of the waterway E-70 – present state and prospects for development. Geography and Tourism 3(1), 33-38 [In Polish with English abstract].
- 18. Grześ M., 1986. Ice jams and floods on the lower Vistula River. Geographia Polonica 52, 51-68.
- 19. Grześ M., 1991. Ice jams and floods on the lower Vistula River. Mechanism and processes. Instytut Geografii i Prz-estrzennego Zagospodarowania PAN, Warszawa [In Polish with English abstract].
- 20. Habel M., 2007. Erosion and accumulation processes of Vistula River below the Włocławek barrage. Nauka Przyroda Technologie 1(2) [In Polish with English abstract].
- 21. Habel M., 2013. Dynamics of the Vistula River channel deformations downstream of the Włocławek Resevoir. Wydawnictwo UKW, Bydgoszcz.
- 22. Hojan M., Rurek M., 2016. Examples of bioerosion downstream the Włocławek Reservoir. Gospodarka Wodna 8, 270-271 [In Polish with English abstract]
- 23. Ingarden R., 1922. Rzeki i kanały żeglowne w byłych trzech zaborach i znaczenie ich gospodarcze dla Polski, Nakład Ministerstwa Robót Publicznych, 670 [In Polish].
- 24. Kociszewska-Musiał G., 1970. Charakterystyka aluwiów współczesnego koryta dolnej Wisły. Biuletyn Geologiczny, Warszawa, 123-139 [In Polish].
- 25. Kociszewska-Musiał G., 1990. The grain-size of channel deposits of the Vistula. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part III. Geographical Studies Special Issue No 5, 76-79.
- 26. Komunikat 19/2011. Prace remontowe na stopniu stabilizującym [In Polish].
- 27. Kordowski J., 2007. Morphology, sedimentary structures, granulometric properties and origin of sandy ribbons developed on the lower Vistula River valley floodplain between Górsk and Szynych. Przegląd Geologiczny 55 (9), 785-794 [In Polish with English abstract].
- 28. Kostrzewski A., 1970. Graining and abrasion of the Bóbr contemporary alluvia as reflection of the dynamics of river sedimentary environment. Poznańskie Towarzystwo Przyjaciół Nauk, Wydział Matematyczno-Przyrodniczy 8, 4, Poznań [In Polish with English summary].
- 29. Magnuszewski A., Moran S., 2015. Vistula River bed erosion processes and their influence on Warsaw`s flood safety. Sediment Dynamics from the Summit to the Sea. Proccedings of a symposium held in New Orleans, Louisiana, USA, 11-14 December 2014, IAHS Publ. 367, 2014, 147-153.
- 30. Niewiarowski W., 1987. Evolution of the lower Vistula valley in the Unisław Basin and at the river gap to the north of Bydgoszcz-Fordon. [In:] L. Starkel (Eds.), Evolution of the Vistula river valley during the last 15000 years. Part II. Geographical Studies Special Issue No.4, 233-252.
- 31. Pieron Ł., Hojan M., 2013. The mechanism of the channel microforms formation on Lower Vistula in Bydgoszcz. Journal of Health Sciences 3 (15), 287-296 [In Polish with English abstract].
- 32. Pieron Ł., Hojan M., Habel M., 2013. Characteristics of river sandbars on regulated reach of the Lower Vistula River. Journal of Health Sciences 3 (14), 114-123 [In Polish with English abstract].
- 33. Starkel L., Wiśniewski E., 1990. The evolution of the Vistula valley. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part III. Geographical Studies Special Issue No. 5, 141-153.
- 34. Starkel. L., 2001. Evolution of the river Vistula valley since the last glaciation till present. Monografie IGiPZ PAN. Warszawa [In Polish with English abstract].
- 35. Tomczak A., 1982. The evolution of the Vistula river valley between Toruń and Solec Kujawski during the Late Glacial and the Holocene. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part I. Geographical Studies Special Issue No. 1, 109-129 [In Polish with English abstract].
- 36. Tomczak A., 1987. Evolution of the Vistula valley in the Toruń Basin in the Late Glacial and Holocene. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part II. Geographical Studies Special Issue No. 4, 207-231 [In Polish with English abstract].
- 37. Wiśniewski E., 1976. Geomorphological development of the Vistula valley between the Płock Basin and Toruń Basin. Prace Geograficzne Instytutu Geografii i Przestrzennego Zagospodarowania PAN, Warszawa [In Polish with English abstract].
- 38. Wiśniewski E., 1982. The geomorphological evolution of the Vistula river valley between Włocławek and Ciechocinek during the last 15000 years. [In:] L. Starkel (Eds.) Evolution of the Vistula river valley during the last 15000 years. Part I. Geographical Studies Special Issue No.1, 93-107.
- 39. pogodynka.pl
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2024).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-a3695288-baba-41d3-bfa4-60f807baa6a2