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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Main Authors: Urbański Janusz, Oleszczuk Ryszard, Brandyk Andrzej, Zając Ewelina
Format: Article
Language:English
Published: Sciendo 2018-12-01
Series:Annals of Warsaw University of Life Sciences, Land Reclamation
Subjects:
Online Access:http://www.degruyter.com/view/j/sggw.2018.50.issue-4/sggw-2018-0023/sggw-2018-0023.xml?format=INT
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spelling 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
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