Loading…
Riemann solution for a class of morphodynamic shallow water dam-break problems
This paper investigates a family of dam-break problems over an erodible bed. The hydrodynamics is described by the shallow water equations, and the bed change by a sediment-conservation equation, coupled to the hydrodynamics by a sediment transport (bed-load) law. When the initial states $\boldsymbo...
Saved in:
Published in: | Journal of fluid mechanics 2018-01, Vol.835, p.1022-1047 |
---|---|
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-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3 |
---|---|
cites | cdi_FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3 |
container_end_page | 1047 |
container_issue | |
container_start_page | 1022 |
container_title | Journal of fluid mechanics |
container_volume | 835 |
creator | Zhu, Fangfang Dodd, Nicholas |
description | This paper investigates a family of dam-break problems over an erodible bed. The hydrodynamics is described by the shallow water equations, and the bed change by a sediment-conservation equation, coupled to the hydrodynamics by a sediment transport (bed-load) law. When the initial states
$\boldsymbol{U}_{l}$
and
$\boldsymbol{U}_{r}$
are sufficiently close to each other the resulting solutions are consistent with the theory proposed by Lax (Hyperbolic Systems of Conservation Laws and the Mathematical Theory of Shock Waves, 1973, SIAM), that for a Riemann problem of
$n$
equations there are
$n$
waves associated with the
$n$
characteristic families. However, for wet–dry dam-break problems over a mobile bed, there are three governing equations, but only two waves. One wave vanishes because of the presence of the dry bed. When initial left and right bed levels (
$B_{l}$
and
$B_{r}$
) are far apart, it is shown that a semi-characteristic shock may occur, which happens because, unlike in shallow water flow on a fixed bed, the flux function is non-convex. In these circumstances it is shown that it is necessary to reconsider the usual shock conditions. Instead, we propose an implied internal shock structure the concept of which originates from the fact that the stationary shock over a fixed-bed discontinuity can be regarded as a limiting case of flow over a sloping fixed bed. The Needham & Hey (Phil. Trans. R. Soc. Lond. A, vol. 334, 1991, pp. 25–53) approximation for the ambiguous integral term
$\int \!h\,\text{d}B$
in the shock condition is improved based on this internal shock structure, such that mathematically valid solutions that incorporate a morphodynamic semi-characteristic shock are arrived at. |
doi_str_mv | 10.1017/jfm.2017.794 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1973762733</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cupid>10_1017_jfm_2017_794</cupid><sourcerecordid>1973762733</sourcerecordid><originalsourceid>FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3</originalsourceid><addsrcrecordid>eNptkDtPwzAUhS0EEqWw8QMssZLgRxInI6p4SRVICGbr2rFpQhwXO1XVf4-rdmBgunf4zjnSh9A1JTklVNz11uUsPbloihM0o0XVZKIqylM0I4SxjFJGztFFjD0hlJNGzNDre2ccjCOOfthMnR-x9QED1gPEiL3Fzof1yre7EVyncVzBMPgt3sJkAm7BZSoY-Mbr4NVgXLxEZxaGaK6Od44-Hx8-Fs_Z8u3pZXG_zHRByZQxZhmrBS11USsDHJjhhIm61qq0mlRclcwIVnINhoCuG1HyBuqiUCW0VW34HN0cetPwz8bESfZ-E8Y0KWkjuKiY4DxRtwdKBx9jMFauQ-cg7CQlcm9MJmNyb0wmYwnPjzg4Fbr2y_xp_S_wCznVbaM</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1973762733</pqid></control><display><type>article</type><title>Riemann solution for a class of morphodynamic shallow water dam-break problems</title><source>Cambridge University Press</source><creator>Zhu, Fangfang ; Dodd, Nicholas</creator><creatorcontrib>Zhu, Fangfang ; Dodd, Nicholas</creatorcontrib><description>This paper investigates a family of dam-break problems over an erodible bed. The hydrodynamics is described by the shallow water equations, and the bed change by a sediment-conservation equation, coupled to the hydrodynamics by a sediment transport (bed-load) law. When the initial states
$\boldsymbol{U}_{l}$
and
$\boldsymbol{U}_{r}$
are sufficiently close to each other the resulting solutions are consistent with the theory proposed by Lax (Hyperbolic Systems of Conservation Laws and the Mathematical Theory of Shock Waves, 1973, SIAM), that for a Riemann problem of
$n$
equations there are
$n$
waves associated with the
$n$
characteristic families. However, for wet–dry dam-break problems over a mobile bed, there are three governing equations, but only two waves. One wave vanishes because of the presence of the dry bed. When initial left and right bed levels (
$B_{l}$
and
$B_{r}$
) are far apart, it is shown that a semi-characteristic shock may occur, which happens because, unlike in shallow water flow on a fixed bed, the flux function is non-convex. In these circumstances it is shown that it is necessary to reconsider the usual shock conditions. Instead, we propose an implied internal shock structure the concept of which originates from the fact that the stationary shock over a fixed-bed discontinuity can be regarded as a limiting case of flow over a sloping fixed bed. The Needham & Hey (Phil. Trans. R. Soc. Lond. A, vol. 334, 1991, pp. 25–53) approximation for the ambiguous integral term
$\int \!h\,\text{d}B$
in the shock condition is improved based on this internal shock structure, such that mathematically valid solutions that incorporate a morphodynamic semi-characteristic shock are arrived at.</description><identifier>ISSN: 0022-1120</identifier><identifier>EISSN: 1469-7645</identifier><identifier>DOI: 10.1017/jfm.2017.794</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Approximation ; Bed load ; Civil engineering ; Computational fluid dynamics ; Conservation ; Conservation equations ; Conservation laws ; Dam failure ; Flow velocity ; Fluid flow ; Formulas (mathematics) ; Hydrodynamics ; Hyperbolic systems ; JFM Papers ; Mathematical analysis ; Mathematical models ; Problems ; Sediment ; Sediment load ; Sediment transport ; Sediments ; Shallow water ; Shallow water equations ; Shock waves ; Water flow</subject><ispartof>Journal of fluid mechanics, 2018-01, Vol.835, p.1022-1047</ispartof><rights>2017 Cambridge University Press</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3</citedby><cites>FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3</cites><orcidid>0000-0002-2820-2363</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022112017007947/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,72960</link.rule.ids></links><search><creatorcontrib>Zhu, Fangfang</creatorcontrib><creatorcontrib>Dodd, Nicholas</creatorcontrib><title>Riemann solution for a class of morphodynamic shallow water dam-break problems</title><title>Journal of fluid mechanics</title><addtitle>J. Fluid Mech</addtitle><description>This paper investigates a family of dam-break problems over an erodible bed. The hydrodynamics is described by the shallow water equations, and the bed change by a sediment-conservation equation, coupled to the hydrodynamics by a sediment transport (bed-load) law. When the initial states
$\boldsymbol{U}_{l}$
and
$\boldsymbol{U}_{r}$
are sufficiently close to each other the resulting solutions are consistent with the theory proposed by Lax (Hyperbolic Systems of Conservation Laws and the Mathematical Theory of Shock Waves, 1973, SIAM), that for a Riemann problem of
$n$
equations there are
$n$
waves associated with the
$n$
characteristic families. However, for wet–dry dam-break problems over a mobile bed, there are three governing equations, but only two waves. One wave vanishes because of the presence of the dry bed. When initial left and right bed levels (
$B_{l}$
and
$B_{r}$
) are far apart, it is shown that a semi-characteristic shock may occur, which happens because, unlike in shallow water flow on a fixed bed, the flux function is non-convex. In these circumstances it is shown that it is necessary to reconsider the usual shock conditions. Instead, we propose an implied internal shock structure the concept of which originates from the fact that the stationary shock over a fixed-bed discontinuity can be regarded as a limiting case of flow over a sloping fixed bed. The Needham & Hey (Phil. Trans. R. Soc. Lond. A, vol. 334, 1991, pp. 25–53) approximation for the ambiguous integral term
$\int \!h\,\text{d}B$
in the shock condition is improved based on this internal shock structure, such that mathematically valid solutions that incorporate a morphodynamic semi-characteristic shock are arrived at.</description><subject>Approximation</subject><subject>Bed load</subject><subject>Civil engineering</subject><subject>Computational fluid dynamics</subject><subject>Conservation</subject><subject>Conservation equations</subject><subject>Conservation laws</subject><subject>Dam failure</subject><subject>Flow velocity</subject><subject>Fluid flow</subject><subject>Formulas (mathematics)</subject><subject>Hydrodynamics</subject><subject>Hyperbolic systems</subject><subject>JFM Papers</subject><subject>Mathematical analysis</subject><subject>Mathematical models</subject><subject>Problems</subject><subject>Sediment</subject><subject>Sediment load</subject><subject>Sediment transport</subject><subject>Sediments</subject><subject>Shallow water</subject><subject>Shallow water equations</subject><subject>Shock waves</subject><subject>Water flow</subject><issn>0022-1120</issn><issn>1469-7645</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNptkDtPwzAUhS0EEqWw8QMssZLgRxInI6p4SRVICGbr2rFpQhwXO1XVf4-rdmBgunf4zjnSh9A1JTklVNz11uUsPbloihM0o0XVZKIqylM0I4SxjFJGztFFjD0hlJNGzNDre2ccjCOOfthMnR-x9QED1gPEiL3Fzof1yre7EVyncVzBMPgt3sJkAm7BZSoY-Mbr4NVgXLxEZxaGaK6Od44-Hx8-Fs_Z8u3pZXG_zHRByZQxZhmrBS11USsDHJjhhIm61qq0mlRclcwIVnINhoCuG1HyBuqiUCW0VW34HN0cetPwz8bESfZ-E8Y0KWkjuKiY4DxRtwdKBx9jMFauQ-cg7CQlcm9MJmNyb0wmYwnPjzg4Fbr2y_xp_S_wCznVbaM</recordid><startdate>20180125</startdate><enddate>20180125</enddate><creator>Zhu, Fangfang</creator><creator>Dodd, Nicholas</creator><general>Cambridge University Press</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TB</scope><scope>7U5</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>S0W</scope><orcidid>https://orcid.org/0000-0002-2820-2363</orcidid></search><sort><creationdate>20180125</creationdate><title>Riemann solution for a class of morphodynamic shallow water dam-break problems</title><author>Zhu, Fangfang ; Dodd, Nicholas</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Approximation</topic><topic>Bed load</topic><topic>Civil engineering</topic><topic>Computational fluid dynamics</topic><topic>Conservation</topic><topic>Conservation equations</topic><topic>Conservation laws</topic><topic>Dam failure</topic><topic>Flow velocity</topic><topic>Fluid flow</topic><topic>Formulas (mathematics)</topic><topic>Hydrodynamics</topic><topic>Hyperbolic systems</topic><topic>JFM Papers</topic><topic>Mathematical analysis</topic><topic>Mathematical models</topic><topic>Problems</topic><topic>Sediment</topic><topic>Sediment load</topic><topic>Sediment transport</topic><topic>Sediments</topic><topic>Shallow water</topic><topic>Shallow water equations</topic><topic>Shock waves</topic><topic>Water flow</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhu, Fangfang</creatorcontrib><creatorcontrib>Dodd, Nicholas</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>DELNET Engineering & Technology Collection</collection><jtitle>Journal of fluid mechanics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhu, Fangfang</au><au>Dodd, Nicholas</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Riemann solution for a class of morphodynamic shallow water dam-break problems</atitle><jtitle>Journal of fluid mechanics</jtitle><addtitle>J. Fluid Mech</addtitle><date>2018-01-25</date><risdate>2018</risdate><volume>835</volume><spage>1022</spage><epage>1047</epage><pages>1022-1047</pages><issn>0022-1120</issn><eissn>1469-7645</eissn><abstract>This paper investigates a family of dam-break problems over an erodible bed. The hydrodynamics is described by the shallow water equations, and the bed change by a sediment-conservation equation, coupled to the hydrodynamics by a sediment transport (bed-load) law. When the initial states
$\boldsymbol{U}_{l}$
and
$\boldsymbol{U}_{r}$
are sufficiently close to each other the resulting solutions are consistent with the theory proposed by Lax (Hyperbolic Systems of Conservation Laws and the Mathematical Theory of Shock Waves, 1973, SIAM), that for a Riemann problem of
$n$
equations there are
$n$
waves associated with the
$n$
characteristic families. However, for wet–dry dam-break problems over a mobile bed, there are three governing equations, but only two waves. One wave vanishes because of the presence of the dry bed. When initial left and right bed levels (
$B_{l}$
and
$B_{r}$
) are far apart, it is shown that a semi-characteristic shock may occur, which happens because, unlike in shallow water flow on a fixed bed, the flux function is non-convex. In these circumstances it is shown that it is necessary to reconsider the usual shock conditions. Instead, we propose an implied internal shock structure the concept of which originates from the fact that the stationary shock over a fixed-bed discontinuity can be regarded as a limiting case of flow over a sloping fixed bed. The Needham & Hey (Phil. Trans. R. Soc. Lond. A, vol. 334, 1991, pp. 25–53) approximation for the ambiguous integral term
$\int \!h\,\text{d}B$
in the shock condition is improved based on this internal shock structure, such that mathematically valid solutions that incorporate a morphodynamic semi-characteristic shock are arrived at.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/jfm.2017.794</doi><tpages>26</tpages><orcidid>https://orcid.org/0000-0002-2820-2363</orcidid><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0022-1120 |
ispartof | Journal of fluid mechanics, 2018-01, Vol.835, p.1022-1047 |
issn | 0022-1120 1469-7645 |
language | eng |
recordid | cdi_proquest_journals_1973762733 |
source | Cambridge University Press |
subjects | Approximation Bed load Civil engineering Computational fluid dynamics Conservation Conservation equations Conservation laws Dam failure Flow velocity Fluid flow Formulas (mathematics) Hydrodynamics Hyperbolic systems JFM Papers Mathematical analysis Mathematical models Problems Sediment Sediment load Sediment transport Sediments Shallow water Shallow water equations Shock waves Water flow |
title | Riemann solution for a class of morphodynamic shallow water dam-break problems |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T07%3A14%3A55IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Riemann%20solution%20for%20a%20class%20of%20morphodynamic%20shallow%20water%20dam-break%20problems&rft.jtitle=Journal%20of%20fluid%20mechanics&rft.au=Zhu,%20Fangfang&rft.date=2018-01-25&rft.volume=835&rft.spage=1022&rft.epage=1047&rft.pages=1022-1047&rft.issn=0022-1120&rft.eissn=1469-7645&rft_id=info:doi/10.1017/jfm.2017.794&rft_dat=%3Cproquest_cross%3E1973762733%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c410t-22f228715c48bea3a2e302788cb5fc063b52e7253cae0ac897539a844b5ad68e3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1973762733&rft_id=info:pmid/&rft_cupid=10_1017_jfm_2017_794&rfr_iscdi=true |