Estimation of lowland river cross-section changes for different soils
This paper involves a comparative analysis of cross-sectional changes at selected reaches of a lowland river, flowing through the areas of mineral and organic soils. The comparisons were made at the background of design and execution assumptions from the period 1967–1971. Main processes, responsible...
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doaj-8638195f3be94cae92ee938bb5d80a0f2020-11-24T21:52:56ZengSciendoAnnals of Warsaw University of Life Sciences, Land Reclamation2081-96172018-12-0150429130010.2478/sggw-2018-0023sggw-2018-0023Estimation of lowland river cross-section changes for different soilsUrbański Janusz0Oleszczuk Ryszard1Brandyk Andrzej2Zając Ewelina3Faculty of Civil and Environmental Engineering, Warsaw University of Life Sciences – SGGW, PolandFaculty of Civil and Environmental Engineering, Warsaw University of Life Sciences – SGGW, PolandWater Centre Laboratory, Faculty of Civil and Environmental Engineering, Warsaw University of Life Sciences – SGGW, PolandFaculty of Environmental Engineering and Land Surveying, University of Agriculture in Krakow, PolandThis paper involves a comparative analysis of cross-sectional changes at selected reaches of a lowland river, flowing through the areas of mineral and organic soils. The comparisons were made at the background of design and execution assumptions from the period 1967–1971. Main processes, responsible for the observed changes of riverbeds in mineral soils (silting, conservation works) and organic soils (subsidence, disappearance of the peat deposit), were identified. In case of organic soils, the decrease of cross-sectional area by approximately from 30 to 60% was estimated in comparison to the original project assumptions, and the subsidence of river banks reached even 0.5 m in relation to the level determined in 1967. In the area of mineral soils, more considerable variability of cross-sectional area was noted along with minor changes of river banks elevation, that resulted most likely from the performed maintenance works.http://www.degruyter.com/view/j/sggw.2018.50.issue-4/sggw-2018-0023/sggw-2018-0023.xml?format=INTlowland riverregulation of the riversub-irrigation systemsorganic and mineral soils |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Urbański Janusz Oleszczuk Ryszard Brandyk Andrzej Zając Ewelina |
spellingShingle |
Urbański Janusz Oleszczuk Ryszard Brandyk Andrzej Zając Ewelina Estimation of lowland river cross-section changes for different soils Annals of Warsaw University of Life Sciences, Land Reclamation lowland river regulation of the river sub-irrigation systems organic and mineral soils |
author_facet |
Urbański Janusz Oleszczuk Ryszard Brandyk Andrzej Zając Ewelina |
author_sort |
Urbański Janusz |
title |
Estimation of lowland river cross-section changes for different soils |
title_short |
Estimation of lowland river cross-section changes for different soils |
title_full |
Estimation of lowland river cross-section changes for different soils |
title_fullStr |
Estimation of lowland river cross-section changes for different soils |
title_full_unstemmed |
Estimation of lowland river cross-section changes for different soils |
title_sort |
estimation of lowland river cross-section changes for different soils |
publisher |
Sciendo |
series |
Annals of Warsaw University of Life Sciences, Land Reclamation |
issn |
2081-9617 |
publishDate |
2018-12-01 |
description |
This paper involves a comparative analysis of cross-sectional changes at selected reaches of a lowland river, flowing through the areas of mineral and organic soils. The comparisons were made at the background of design and execution assumptions from the period 1967–1971. Main processes, responsible for the observed changes of riverbeds in mineral soils (silting, conservation works) and organic soils (subsidence, disappearance of the peat deposit), were identified. In case of organic soils, the decrease of cross-sectional area by approximately from 30 to 60% was estimated in comparison to the original project assumptions, and the subsidence of river banks reached even 0.5 m in relation to the level determined in 1967. In the area of mineral soils, more considerable variability of cross-sectional area was noted along with minor changes of river banks elevation, that resulted most likely from the performed maintenance works. |
topic |
lowland river regulation of the river sub-irrigation systems organic and mineral soils |
url |
http://www.degruyter.com/view/j/sggw.2018.50.issue-4/sggw-2018-0023/sggw-2018-0023.xml?format=INT |
work_keys_str_mv |
AT urbanskijanusz estimationoflowlandrivercrosssectionchangesfordifferentsoils AT oleszczukryszard estimationoflowlandrivercrosssectionchangesfordifferentsoils AT brandykandrzej estimationoflowlandrivercrosssectionchangesfordifferentsoils AT zajacewelina estimationoflowlandrivercrosssectionchangesfordifferentsoils |
_version_ |
1725873980121808896 |