Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes

The stability of river channels results from the impact of spatially diversified natural characteristics of the catchment, which are additionally intensified by the pressure of human activities. The aim of the current study was the overall assessment of the riverbed stability in the Brda River catch...

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Main Authors: Dawid Aleksander Szatten, Oleksandr Obodovskyi, Marta Brzezińska
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2025-02-01
Series:International Journal of Sediment Research
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Online Access:http://www.sciencedirect.com/science/article/pii/S1001627924001239
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author Dawid Aleksander Szatten
Oleksandr Obodovskyi
Marta Brzezińska
author_facet Dawid Aleksander Szatten
Oleksandr Obodovskyi
Marta Brzezińska
author_sort Dawid Aleksander Szatten
collection DOAJ
description The stability of river channels results from the impact of spatially diversified natural characteristics of the catchment, which are additionally intensified by the pressure of human activities. The aim of the current study was the overall assessment of the riverbed stability in the Brda River catchment (Poland) in the two periods 1980–1989 and 1991–2018. The study area is characterized by a high discharge regularity, resulting from the river-lake system in the upper part of the catchment, and strong human pressure caused by the presence of hydrotechnical structures in the middle and lower parts of the catchment. The hydrological, sedimentological, and land cover archival data were used in the current study. Also, in the field campaign, the characteristics of the river channel were delimited. Finally, the erosive stability channel factor is proposed, reflecting the level of pressure on the fluvial system from the catchment. The results show that in the first period, there was a tendency to accumulate sediment on the riverbed, resulting in its instability. However, in the second period, the river channel was stable, and erosion and sedimentation processes did not occur. The links between the stability of the bed of the Brda River, and the temporal and area-related pressures made it possible to identify long-term trends in the degradation of the fluvial environment as a result of human activities and to indicate the directions for sustainable sediment management in the catchment.
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publisher KeAi Communications Co., Ltd.
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series International Journal of Sediment Research
spelling doaj-art-0186b64ea28e45ff892690e48408204a2025-01-12T05:24:19ZengKeAi Communications Co., Ltd.International Journal of Sediment Research1001-62792025-02-01401146157Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changesDawid Aleksander Szatten0Oleksandr Obodovskyi1Marta Brzezińska2Department of Waterways Revitalization, Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz 85-064, Poland; Corresponding author.Department of Waterways Revitalization, Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz 85-064, Poland; Faculty of Geography, Taras Shevchenko National University, Kiev 03127, UkraineDepartment of Waterways Revitalization, Faculty of Geographical Sciences, Kazimierz Wielki University, Bydgoszcz 85-064, PolandThe stability of river channels results from the impact of spatially diversified natural characteristics of the catchment, which are additionally intensified by the pressure of human activities. The aim of the current study was the overall assessment of the riverbed stability in the Brda River catchment (Poland) in the two periods 1980–1989 and 1991–2018. The study area is characterized by a high discharge regularity, resulting from the river-lake system in the upper part of the catchment, and strong human pressure caused by the presence of hydrotechnical structures in the middle and lower parts of the catchment. The hydrological, sedimentological, and land cover archival data were used in the current study. Also, in the field campaign, the characteristics of the river channel were delimited. Finally, the erosive stability channel factor is proposed, reflecting the level of pressure on the fluvial system from the catchment. The results show that in the first period, there was a tendency to accumulate sediment on the riverbed, resulting in its instability. However, in the second period, the river channel was stable, and erosion and sedimentation processes did not occur. The links between the stability of the bed of the Brda River, and the temporal and area-related pressures made it possible to identify long-term trends in the degradation of the fluvial environment as a result of human activities and to indicate the directions for sustainable sediment management in the catchment.http://www.sciencedirect.com/science/article/pii/S1001627924001239Channel stabilityErosive stability channel factorCatchment degradationSediment transportHuman impact
spellingShingle Dawid Aleksander Szatten
Oleksandr Obodovskyi
Marta Brzezińska
Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
International Journal of Sediment Research
Channel stability
Erosive stability channel factor
Catchment degradation
Sediment transport
Human impact
title Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
title_full Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
title_fullStr Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
title_full_unstemmed Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
title_short Erosive stability channel factor for Brda River (Poland): A key assessment of the human impact of the catchment changes
title_sort erosive stability channel factor for brda river poland a key assessment of the human impact of the catchment changes
topic Channel stability
Erosive stability channel factor
Catchment degradation
Sediment transport
Human impact
url http://www.sciencedirect.com/science/article/pii/S1001627924001239
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