Loading…
Flow in Compound Channel with Abrupt Floodplain Contraction
Flooding rivers usually present transition reaches where the floodplain width can significantly vary. The present study focuses on an abrupt floodplain contraction (mean angle 22°) in order to determine whether one-dimensional (1D) models, developed for straight and slightly converging geometry, are...
Saved in:
Published in: | Journal of hydraulic engineering (New York, N.Y.) N.Y.), 2006-09, Vol.132 (9), p.958-970 |
---|---|
Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03 |
---|---|
cites | cdi_FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03 |
container_end_page | 970 |
container_issue | 9 |
container_start_page | 958 |
container_title | Journal of hydraulic engineering (New York, N.Y.) |
container_volume | 132 |
creator | Proust, S Rivière, N Bousmar, D Paquier, A Zech, Y Morel, R |
description | Flooding rivers usually present transition reaches where the floodplain width can significantly vary. The present study focuses on an abrupt floodplain contraction (mean angle 22°) in order to determine whether one-dimensional (1D) models, developed for straight and slightly converging geometry, are equally valid for such a geometry. Experiments on a contraction model were carried out in an asymmetric compound channel flume. Severe mass and momentum transfers from the floodplain towards the main channel were observed, giving rise to a noteworthy transverse slope of the water surface and different head loss gradients in the two subsections. Three 1D models and one 2D simulation were compared to experimental measurements. Each 1D model incorporates a specific approach for the modeling of the momentum exchange at the interface boundary between the main channel and the floodplain. The increase of the lateral mass transfer generates moderate errors on the water level values but significant errors on the discharge distribution. Erroneous results arise because of incorrect estimations of both momentum exchange due to lateral mass transfers and boundary conditions which are imposed by the tested 1D models. |
doi_str_mv | 10.1061/(ASCE)0733-9429(2006)132:9(958) |
format | article |
fullrecord | <record><control><sourceid>proquest_hal_p</sourceid><recordid>TN_cdi_hal_primary_oai_HAL_hal_00274829v1</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>19303759</sourcerecordid><originalsourceid>FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03</originalsourceid><addsrcrecordid>eNp9kFFLwzAUhYMoOKf_oS_q9lC9Sdu1mSCMsjlh4IP6HG6zlHV0SU1ah__e1Ml88yk3h49z4CPklsIdhQm9H81e8_kY0igKecz4iAFMxjRiUz7iSTY-IQPK4yhMOcApGRy5c3Lh3BaAxhOeDcjDojb7oNJBbnaN6fQ6yDeotaqDfdVugllhu6YNPGTWTY0_nG4tyrYy-pKclVg7dfX7Dsn7Yv6WL8PVy9NzPluFGKe0DctMFZL7G8oEOapE0WRC40JlKQOUBUUWc772UQlJUSQIkjH0qUxT5X_RkIwPvRusRWOrHdovYbASy9lK9BkAS-OM8U_q2ZsD21jz0SnXil3lpKpr1Mp0TlAeQZQm3IOPB1Ba45xV5bGZgugFC9ELFr040YsTvWDhBQsuvGBfcP27hE5iXVrUsnJ_LRnEWT82JNMD5zEltqaz2ss6rvw_8g26oIxL</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>19303759</pqid></control><display><type>article</type><title>Flow in Compound Channel with Abrupt Floodplain Contraction</title><source>American Society Of Civil Engineers ASCE Journals</source><creator>Proust, S ; Rivière, N ; Bousmar, D ; Paquier, A ; Zech, Y ; Morel, R</creator><creatorcontrib>Proust, S ; Rivière, N ; Bousmar, D ; Paquier, A ; Zech, Y ; Morel, R</creatorcontrib><description>Flooding rivers usually present transition reaches where the floodplain width can significantly vary. The present study focuses on an abrupt floodplain contraction (mean angle 22°) in order to determine whether one-dimensional (1D) models, developed for straight and slightly converging geometry, are equally valid for such a geometry. Experiments on a contraction model were carried out in an asymmetric compound channel flume. Severe mass and momentum transfers from the floodplain towards the main channel were observed, giving rise to a noteworthy transverse slope of the water surface and different head loss gradients in the two subsections. Three 1D models and one 2D simulation were compared to experimental measurements. Each 1D model incorporates a specific approach for the modeling of the momentum exchange at the interface boundary between the main channel and the floodplain. The increase of the lateral mass transfer generates moderate errors on the water level values but significant errors on the discharge distribution. Erroneous results arise because of incorrect estimations of both momentum exchange due to lateral mass transfers and boundary conditions which are imposed by the tested 1D models.</description><identifier>ISSN: 0733-9429</identifier><identifier>EISSN: 1943-7900</identifier><identifier>DOI: 10.1061/(ASCE)0733-9429(2006)132:9(958)</identifier><identifier>CODEN: JHEND8</identifier><language>eng</language><publisher>Reston, VA: American Society of Civil Engineers</publisher><subject>Applied sciences ; Buildings. Public works ; Computation methods. Tables. Charts ; Environmental Sciences ; Exact sciences and technology ; Freshwater ; Hydraulic constructions ; River flow control. Flood control ; Structural analysis. Stresses ; TECHNICAL PAPERS</subject><ispartof>Journal of hydraulic engineering (New York, N.Y.), 2006-09, Vol.132 (9), p.958-970</ispartof><rights>2007 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03</citedby><cites>FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03</cites><orcidid>0000-0002-5851-2442 ; 0000-0003-2703-4633 ; 0000-0002-1074-5001</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttp://ascelibrary.org/doi/pdf/10.1061/(ASCE)0733-9429(2006)132:9(958)$$EPDF$$P50$$Gasce$$H</linktopdf><linktohtml>$$Uhttp://ascelibrary.org/doi/abs/10.1061/(ASCE)0733-9429(2006)132:9(958)$$EHTML$$P50$$Gasce$$H</linktohtml><link.rule.ids>230,314,780,784,885,3250,10067,27923,27924,75962,75970</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=18048930$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-00274829$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Proust, S</creatorcontrib><creatorcontrib>Rivière, N</creatorcontrib><creatorcontrib>Bousmar, D</creatorcontrib><creatorcontrib>Paquier, A</creatorcontrib><creatorcontrib>Zech, Y</creatorcontrib><creatorcontrib>Morel, R</creatorcontrib><title>Flow in Compound Channel with Abrupt Floodplain Contraction</title><title>Journal of hydraulic engineering (New York, N.Y.)</title><description>Flooding rivers usually present transition reaches where the floodplain width can significantly vary. The present study focuses on an abrupt floodplain contraction (mean angle 22°) in order to determine whether one-dimensional (1D) models, developed for straight and slightly converging geometry, are equally valid for such a geometry. Experiments on a contraction model were carried out in an asymmetric compound channel flume. Severe mass and momentum transfers from the floodplain towards the main channel were observed, giving rise to a noteworthy transverse slope of the water surface and different head loss gradients in the two subsections. Three 1D models and one 2D simulation were compared to experimental measurements. Each 1D model incorporates a specific approach for the modeling of the momentum exchange at the interface boundary between the main channel and the floodplain. The increase of the lateral mass transfer generates moderate errors on the water level values but significant errors on the discharge distribution. Erroneous results arise because of incorrect estimations of both momentum exchange due to lateral mass transfers and boundary conditions which are imposed by the tested 1D models.</description><subject>Applied sciences</subject><subject>Buildings. Public works</subject><subject>Computation methods. Tables. Charts</subject><subject>Environmental Sciences</subject><subject>Exact sciences and technology</subject><subject>Freshwater</subject><subject>Hydraulic constructions</subject><subject>River flow control. Flood control</subject><subject>Structural analysis. Stresses</subject><subject>TECHNICAL PAPERS</subject><issn>0733-9429</issn><issn>1943-7900</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNp9kFFLwzAUhYMoOKf_oS_q9lC9Sdu1mSCMsjlh4IP6HG6zlHV0SU1ah__e1Ml88yk3h49z4CPklsIdhQm9H81e8_kY0igKecz4iAFMxjRiUz7iSTY-IQPK4yhMOcApGRy5c3Lh3BaAxhOeDcjDojb7oNJBbnaN6fQ6yDeotaqDfdVugllhu6YNPGTWTY0_nG4tyrYy-pKclVg7dfX7Dsn7Yv6WL8PVy9NzPluFGKe0DctMFZL7G8oEOapE0WRC40JlKQOUBUUWc772UQlJUSQIkjH0qUxT5X_RkIwPvRusRWOrHdovYbASy9lK9BkAS-OM8U_q2ZsD21jz0SnXil3lpKpr1Mp0TlAeQZQm3IOPB1Ba45xV5bGZgugFC9ELFr040YsTvWDhBQsuvGBfcP27hE5iXVrUsnJ_LRnEWT82JNMD5zEltqaz2ss6rvw_8g26oIxL</recordid><startdate>20060901</startdate><enddate>20060901</enddate><creator>Proust, S</creator><creator>Rivière, N</creator><creator>Bousmar, D</creator><creator>Paquier, A</creator><creator>Zech, Y</creator><creator>Morel, R</creator><general>American Society of Civil Engineers</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0002-5851-2442</orcidid><orcidid>https://orcid.org/0000-0003-2703-4633</orcidid><orcidid>https://orcid.org/0000-0002-1074-5001</orcidid></search><sort><creationdate>20060901</creationdate><title>Flow in Compound Channel with Abrupt Floodplain Contraction</title><author>Proust, S ; Rivière, N ; Bousmar, D ; Paquier, A ; Zech, Y ; Morel, R</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Applied sciences</topic><topic>Buildings. Public works</topic><topic>Computation methods. Tables. Charts</topic><topic>Environmental Sciences</topic><topic>Exact sciences and technology</topic><topic>Freshwater</topic><topic>Hydraulic constructions</topic><topic>River flow control. Flood control</topic><topic>Structural analysis. Stresses</topic><topic>TECHNICAL PAPERS</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Proust, S</creatorcontrib><creatorcontrib>Rivière, N</creatorcontrib><creatorcontrib>Bousmar, D</creatorcontrib><creatorcontrib>Paquier, A</creatorcontrib><creatorcontrib>Zech, Y</creatorcontrib><creatorcontrib>Morel, R</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Journal of hydraulic engineering (New York, N.Y.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Proust, S</au><au>Rivière, N</au><au>Bousmar, D</au><au>Paquier, A</au><au>Zech, Y</au><au>Morel, R</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Flow in Compound Channel with Abrupt Floodplain Contraction</atitle><jtitle>Journal of hydraulic engineering (New York, N.Y.)</jtitle><date>2006-09-01</date><risdate>2006</risdate><volume>132</volume><issue>9</issue><spage>958</spage><epage>970</epage><pages>958-970</pages><issn>0733-9429</issn><eissn>1943-7900</eissn><coden>JHEND8</coden><abstract>Flooding rivers usually present transition reaches where the floodplain width can significantly vary. The present study focuses on an abrupt floodplain contraction (mean angle 22°) in order to determine whether one-dimensional (1D) models, developed for straight and slightly converging geometry, are equally valid for such a geometry. Experiments on a contraction model were carried out in an asymmetric compound channel flume. Severe mass and momentum transfers from the floodplain towards the main channel were observed, giving rise to a noteworthy transverse slope of the water surface and different head loss gradients in the two subsections. Three 1D models and one 2D simulation were compared to experimental measurements. Each 1D model incorporates a specific approach for the modeling of the momentum exchange at the interface boundary between the main channel and the floodplain. The increase of the lateral mass transfer generates moderate errors on the water level values but significant errors on the discharge distribution. Erroneous results arise because of incorrect estimations of both momentum exchange due to lateral mass transfers and boundary conditions which are imposed by the tested 1D models.</abstract><cop>Reston, VA</cop><pub>American Society of Civil Engineers</pub><doi>10.1061/(ASCE)0733-9429(2006)132:9(958)</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-5851-2442</orcidid><orcidid>https://orcid.org/0000-0003-2703-4633</orcidid><orcidid>https://orcid.org/0000-0002-1074-5001</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0733-9429 |
ispartof | Journal of hydraulic engineering (New York, N.Y.), 2006-09, Vol.132 (9), p.958-970 |
issn | 0733-9429 1943-7900 |
language | eng |
recordid | cdi_hal_primary_oai_HAL_hal_00274829v1 |
source | American Society Of Civil Engineers ASCE Journals |
subjects | Applied sciences Buildings. Public works Computation methods. Tables. Charts Environmental Sciences Exact sciences and technology Freshwater Hydraulic constructions River flow control. Flood control Structural analysis. Stresses TECHNICAL PAPERS |
title | Flow in Compound Channel with Abrupt Floodplain Contraction |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-11T19%3A02%3A36IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_hal_p&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Flow%20in%20Compound%20Channel%20with%20Abrupt%20Floodplain%20Contraction&rft.jtitle=Journal%20of%20hydraulic%20engineering%20(New%20York,%20N.Y.)&rft.au=Proust,%20S&rft.date=2006-09-01&rft.volume=132&rft.issue=9&rft.spage=958&rft.epage=970&rft.pages=958-970&rft.issn=0733-9429&rft.eissn=1943-7900&rft.coden=JHEND8&rft_id=info:doi/10.1061/(ASCE)0733-9429(2006)132:9(958)&rft_dat=%3Cproquest_hal_p%3E19303759%3C/proquest_hal_p%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a471t-f8ebc9a470f5a9ae5e15614be8720acb1a2499d614f05bb5a0c22a1a2c77e5a03%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=19303759&rft_id=info:pmid/&rfr_iscdi=true |