Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows
Autor(a) principal: | |
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Data de Publicação: | 2008 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
Texto Completo: | http://hdl.handle.net/10316/3950 https://doi.org/10.1016/j.advwatres.2008.03.001 |
Resumo: | The logarithmic layer of double-averaged (in time and space) streamwise velocity profiles obtained from field measurements made in the Swiss rivers, Venoge and Chamberonne is parameterized and discussed. Velocity measurements were made using a 3D Acoustic Doppler Velocity Profiler. Both riverbeds are hydraulically rough, composed of coarse gravel, with relative submergences (h/D50) of 5.25 and 5.96, respectively. From the observations, the flow may be divided into three different layers: a roughness layer near the bed, an equivalent logarithmic layer and a surface or outer layer. It was found that a logarithmic law can describe the double-averaged profiles in the layer 0.30 < z/h < 0.75. The parameterization of the logarithmic law is discussed. Special emphasis is given to the geometric parameters roughness and zero-displacement heights and to the equivalent von Karman constant. |
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Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flowsDouble-averaged velocity profilesLogarithmic lawVelocity field measurementsThe logarithmic layer of double-averaged (in time and space) streamwise velocity profiles obtained from field measurements made in the Swiss rivers, Venoge and Chamberonne is parameterized and discussed. Velocity measurements were made using a 3D Acoustic Doppler Velocity Profiler. Both riverbeds are hydraulically rough, composed of coarse gravel, with relative submergences (h/D50) of 5.25 and 5.96, respectively. From the observations, the flow may be divided into three different layers: a roughness layer near the bed, an equivalent logarithmic layer and a surface or outer layer. It was found that a logarithmic law can describe the double-averaged profiles in the layer 0.30 < z/h < 0.75. The parameterization of the logarithmic law is discussed. Special emphasis is given to the geometric parameters roughness and zero-displacement heights and to the equivalent von Karman constant.http://www.sciencedirect.com/science/article/B6VCF-4S33NBV-1/1/bbf4c14ea5ed4a1062a36f1c5b373f122008info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleaplication/PDFhttp://hdl.handle.net/10316/3950http://hdl.handle.net/10316/3950https://doi.org/10.1016/j.advwatres.2008.03.001engAdvances in Water Resources. 31:6 (2008) 915-925Franca, Mário J.Ferreira, Rui M. L.Lemmin, Ulrichinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2020-11-06T16:48:45Zoai:estudogeral.uc.pt:10316/3950Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:57:13.349235Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse |
dc.title.none.fl_str_mv |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
title |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
spellingShingle |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows Franca, Mário J. Double-averaged velocity profiles Logarithmic law Velocity field measurements |
title_short |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
title_full |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
title_fullStr |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
title_full_unstemmed |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
title_sort |
Parameterization of the logarithmic layer of double-averaged streamwise velocity profiles in gravel-bed river flows |
author |
Franca, Mário J. |
author_facet |
Franca, Mário J. Ferreira, Rui M. L. Lemmin, Ulrich |
author_role |
author |
author2 |
Ferreira, Rui M. L. Lemmin, Ulrich |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Franca, Mário J. Ferreira, Rui M. L. Lemmin, Ulrich |
dc.subject.por.fl_str_mv |
Double-averaged velocity profiles Logarithmic law Velocity field measurements |
topic |
Double-averaged velocity profiles Logarithmic law Velocity field measurements |
description |
The logarithmic layer of double-averaged (in time and space) streamwise velocity profiles obtained from field measurements made in the Swiss rivers, Venoge and Chamberonne is parameterized and discussed. Velocity measurements were made using a 3D Acoustic Doppler Velocity Profiler. Both riverbeds are hydraulically rough, composed of coarse gravel, with relative submergences (h/D50) of 5.25 and 5.96, respectively. From the observations, the flow may be divided into three different layers: a roughness layer near the bed, an equivalent logarithmic layer and a surface or outer layer. It was found that a logarithmic law can describe the double-averaged profiles in the layer 0.30 < z/h < 0.75. The parameterization of the logarithmic law is discussed. Special emphasis is given to the geometric parameters roughness and zero-displacement heights and to the equivalent von Karman constant. |
publishDate |
2008 |
dc.date.none.fl_str_mv |
2008 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
http://hdl.handle.net/10316/3950 http://hdl.handle.net/10316/3950 https://doi.org/10.1016/j.advwatres.2008.03.001 |
url |
http://hdl.handle.net/10316/3950 https://doi.org/10.1016/j.advwatres.2008.03.001 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
Advances in Water Resources. 31:6 (2008) 915-925 |
dc.rights.driver.fl_str_mv |
info:eu-repo/semantics/openAccess |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
aplication/PDF |
dc.source.none.fl_str_mv |
reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação instacron:RCAAP |
instname_str |
Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
instacron_str |
RCAAP |
institution |
RCAAP |
reponame_str |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
collection |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) |
repository.name.fl_str_mv |
Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação |
repository.mail.fl_str_mv |
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1799133860178427904 |