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1
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Laboratory study of suspended sediment dynamics over a mildly sloping sandy seabed

100%
Stachurska B., Staroszczyk R.
Oceanologia
|
2019
|
tom 61
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nr 3
2
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Suspended sediment concentration and yield in snowmelt flood events in a small lowland river

100%
Hejduk A., Banasik K.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
|
2010
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tom 42
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nr 1
61-68
Results of investigation on suspended sediment delivery from small lowland, agriculturally used catchment of Zagożdżonka River, located in central Poland, during snowmelt periods of 2001– –2007 are presented. The study catchment‘s area, upstream of the well equipped gauging station at Czarna, is 23.4 km2. Suspended sediment concentration and sediment yield has been calculated and analysed for 15 snowmelt flood events. The relationship between suspended sediment concentration and the discharge has been analyzed. It has been found that the relation, in majority of the cases, has the form of clockwise hysteresis, however the existance of other types of hysteresis i.e. anticlockwise and “8” shape, have been also confi rmed. Signifi cant relation between suspended sediment yield and runoff volume of snowmelt flood events has been also found.
3
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Kelvin-Helmholtz instabilities in the Colorado River Delta, Gulf of California

100%
Carbajal N., Vargas J. T., Rodriguez J. H. G., Montano Ley Y., Salas de Leon D. A.
Oceanologia
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2021
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tom 63
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nr 3
4

Grain size distribution of suspended sediment during rainfall and snowmelt floods in small lowland river

84%
Hejduk L., Hejduk A., Banasik K.
Electronic Journal of Polish Agricultural Universities. Series Environmental Development
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2006
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tom 09
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nr 2
This paper present information on particle size variation during rainfall and snowmelt flood from the small agricultural catchment. The grain size distribution during two rainfall, three snowmelt and one rainfall-snowmelt flood was compared. The average percentage of clays size material (<4 µm) for all samples was 2.7%, silt size material (> 4 µm and <62 µm) was 42.8% and sand (>62 µm) was 54.5%. The average median (d50) for floods ranged between 49.8 microns and 98.3 microns depend on the flood.
5
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Appraisal of suspended sediment concentration on reference level according to van Rijn’s method

84%
Michalec B.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
|
2008
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tom 40
6

Dynamics of suspended material carried out from the Flysch Bystrzanka catchment during selected rainfall events in the period 1997–2008

84%
Kijowska M., Bochenek W.
Quaestiones Geographicae
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2011
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tom 30
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nr 1
7

The transport of material by the rivers of the Northern slope of the Pomeranian Lakeland to the Baltic Sea

84%
Szymczak E.
Oceanological Studies
|
2002
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tom 31
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nr 3-4
8
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Experiments on wave motion and suspended sediment concentration at Nang Hai, Can Gio mangrove forest, Southern Vietnam

84%
Hong Phuoc V. L., Massel S. R.
Oceanologia
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2006
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tom 48
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nr 1
Biogeochemical and trophodynamic processes as well as hydrodynamic factors play a major role in the structure and function of mangrove ecosystems. This study outlines field experiments on wave motion and suspended sediment concentration carried out at Nang Hai, Can Gio mangrove forest, Southern Vietnam. Pressure sensors were used to measure sea surface elevation, and Optical Backscatter Sensors (OBS) were applied to detect infrared (IR) radiation scattered from suspended particles in order to measure turbidity and suspended sediment concentrations. The experimental results indicate that most of the energy is dissipated inside the mangrove forest as a result of wave-trunk interactions and wave breaking. The suspended sediment concentration depends on wave intensity and tidal current velocity. Wave action is one of the main factors forcing sediment transport and coastal erosion at the study site; even the wave field at the study site is not so strong. The establishment of mangrove vegetation can encourage the deposition of sediment, or at least the retention of the flood-tide sediment influx.
9

The transport and distribution of the river load from the Kacza River into the Gulf of Gdansk (Southern Baltic Sea, Poland)

67%
Szymczak E., Rhode D., Piekarek-Jankowska H.
Oceanological and Hydrobiological Studies
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2011
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tom 40
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nr 4
10

Transport of the river load from the Bladzikowski Stream to the Puck Lagoon (Southern Baltic Sea, Poland)

67%
Damaszke M., Szymczak E.
Oceanological and Hydrobiological Studies
|
2013
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tom 42
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nr 2
11
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Variability of suspended sediment grain size distribution in winter floods

67%
Hejduk A., Hejduk L.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
|
2016
|
tom 48
|
nr 2
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