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1

Modelling of the bed load movement in degradated rivers

100%
Parzonka W.
Zeszyty Naukowe Akademii Rolniczej we Wrocławiu. Konferencje
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1995
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tom 10
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nr 2
2

Transportation of sediment carried during flood events in a small urban catchment

75%
Krajewski A., Gladecki J., Banasik K.
Acta Scientiarum Polonorum. Formatio Circumiectus
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2018
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tom 17
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nr 3
The aim of this study is to present results of investigations into rainfall–runoff–suspended sediment transport process, based on field measurements conducted in small (A = 28.7 km²) urban catchment of Służew Creek, located in Warsaw. Hydrological monitoring was carried out by the Department of Hydraulic Engineering at the WULS-SGGW (Warsaw University of Life Sciences). Between 2014–2017, twelve flood events were recorded, during which rainfall, discharge, turbidity, and suspended sediment concentrations were measured. The correlation between the flows and sediment concentration was analysed and clockwise hysteresis for all events was indicated, meaning that sediment concentrations during the increase of water flows were higher than at the same flow values during the fall of the flood wave. Also first flush effect has been noted, that is, most of the sediment loads was washed-off at the beginning of the flood event; whereas the peak concentration occurred prior to the maximum discharge. Statistically significant correlation between direct runoff and suspended sediment has been established.
3

The suspended sediment and bed load in mountain streams

75%
Bartnik W., Madeyski M., Banasik K., Gorski D.
Zeszyty Naukowe Akademii Rolniczej we Wrocławiu. Inżynieria Środowiska
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1992
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tom 01
4
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Bedload transport in the Vistula River mouth derived from dune migration rates, Southern Baltic Sea

63%
Lisimenka A., Kubicki A.
Oceanologia
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2019
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tom 61
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nr 3
5
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The upper Odra as a case study of the impact of channel regulation on its morphodynamics

63%
Czajka A.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
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2014
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tom 46
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nr 4
The aim of the research was to compare morphodynamics of the Odra river channel in three different sectors and to fi nd the main difference in the way of sediment transport before and after regulation in meandering, straight and sinuous channel sectors and compare the data with those calculated for reconstructed, natural channel of the Odra river. Sediment transport in discussed sectors was compared for average, bankfull and fl ood discharges and it proceeds in different ways. Morphodynamics of the preregulated Odra was most similar to the one currently observed in the meandering section. Also the dynamics of bed-material transport and, consequently, the possibility of the occurrence and disappearance of channel forms is greatly varied among the studied sectors. As it was assumed, a diversifi ed channel geometry imposes water fl ow, which entails a series of processes shaping the channel dynamics.
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