Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope

The aim of the study was to analyse the possibility of using dimensionless coordinates in order to determine the typical shape of the overflow stream at the gabion sill, as well as identify the flow zone therein and evaluate the characteristic dimensions of the profile. The analysed weir consists of...

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Main Authors: Sławomir Bajkowski, Aneta Tymińska
Format: Article
Language:English
Published: Publishing House of the University of Agriculture in Krakow 2018-12-01
Series:Acta Scientiarum Polonorum. Formatio Circumiectus
Subjects:
Online Access:http://www.formatiocircumiectus.actapol.net/pub/17_4_15.pdf
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spelling doaj-68eb2f0ea2ba4e0497c5b882f63aa7a92020-11-25T00:28:53ZengPublishing House of the University of Agriculture in KrakowActa Scientiarum Polonorum. Formatio Circumiectus1644-07652018-12-01174155510.15576/ASP.FC/2018.17.4.15Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slopeSławomir Bajkowski0Aneta Tymińska1Department of Hydraulic Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life SciencesFaculty of Civil and Environmental Engineering, Warsaw University of Life SciencesThe aim of the study was to analyse the possibility of using dimensionless coordinates in order to determine the typical shape of the overflow stream at the gabion sill, as well as identify the flow zone therein and evaluate the characteristic dimensions of the profile. The analysed weir consists of a permeable part filled with natural stone material, and a solid part in the form of sharp-crested weir on sloping upstream face. The shape of the upper profile of the stream has been determined along with its parameters. Three flow zones at the length of the crest sill were identified: the free flow zone, the inlet wave zone and the sill part, which is free of water. The water flow rate influences the formation of water stream profile flowing over the tested sill. The full correlation dependence of variables was obtained in the analysis. The obtained results can be used in the design of this type of field structures.http://www.formatiocircumiectus.actapol.net/pub/17_4_15.pdfgabion sillsharp-crested weirstream shape
collection DOAJ
language English
format Article
sources DOAJ
author Sławomir Bajkowski
Aneta Tymińska
spellingShingle Sławomir Bajkowski
Aneta Tymińska
Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
Acta Scientiarum Polonorum. Formatio Circumiectus
gabion sill
sharp-crested weir
stream shape
author_facet Sławomir Bajkowski
Aneta Tymińska
author_sort Sławomir Bajkowski
title Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
title_short Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
title_full Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
title_fullStr Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
title_full_unstemmed Water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
title_sort water surface profile of the trapezoidal permeable sill with sharp-crested weir on the upstream slope
publisher Publishing House of the University of Agriculture in Krakow
series Acta Scientiarum Polonorum. Formatio Circumiectus
issn 1644-0765
publishDate 2018-12-01
description The aim of the study was to analyse the possibility of using dimensionless coordinates in order to determine the typical shape of the overflow stream at the gabion sill, as well as identify the flow zone therein and evaluate the characteristic dimensions of the profile. The analysed weir consists of a permeable part filled with natural stone material, and a solid part in the form of sharp-crested weir on sloping upstream face. The shape of the upper profile of the stream has been determined along with its parameters. Three flow zones at the length of the crest sill were identified: the free flow zone, the inlet wave zone and the sill part, which is free of water. The water flow rate influences the formation of water stream profile flowing over the tested sill. The full correlation dependence of variables was obtained in the analysis. The obtained results can be used in the design of this type of field structures.
topic gabion sill
sharp-crested weir
stream shape
url http://www.formatiocircumiectus.actapol.net/pub/17_4_15.pdf
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AT anetatyminska watersurfaceprofileofthetrapezoidalpermeablesillwithsharpcrestedweirontheupstreamslope
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