Linear and angular momentum conservation for the hydraulic jump in converging channels
This note is the final completion of a previously published work concerning the integral conservation of linear and angular momentum in the steady hydraulic jump in a linearly diverging channel [Valiani, A., Caleffi, V. (2011). Linear and angular momentum conservation in hydraulic jump in diverging...
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Veröffentlicht in: | Journal of hydraulic research 2013-10, Vol.51 (5), p.601-607 |
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description | This note is the final completion of a previously published work concerning the integral conservation of linear and angular momentum in the steady hydraulic jump in a linearly diverging channel [Valiani, A., Caleffi, V. (2011). Linear and angular momentum conservation in hydraulic jump in diverging channels. Adv. Water Res. 34(2), 227-242]. The same reasoning is applied to a linearly converging channel, and the theoretical framework, which is almost completely the same, is shown to remain valid. Using a proper mechanical scheme, an analytical solution is obtained for the free surface profile of the flow. This solution allows the determination of the sequent depths and their positions. Thus, the length of the jump, which is assumed to be equal to the length of the roller, is also found. The mainstream and roller thicknesses can also be derived. This model may be used to derive the average shear stress exerted by the roller on the mainstream and the related exact expression for the total power loss in the jump, allowing to demonstrate the internal consistency of the proposed conceptual scheme. |
doi_str_mv | 10.1080/00221686.2013.805701 |
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(2011). Linear and angular momentum conservation in hydraulic jump in diverging channels. Adv. Water Res. 34(2), 227-242]. The same reasoning is applied to a linearly converging channel, and the theoretical framework, which is almost completely the same, is shown to remain valid. Using a proper mechanical scheme, an analytical solution is obtained for the free surface profile of the flow. This solution allows the determination of the sequent depths and their positions. Thus, the length of the jump, which is assumed to be equal to the length of the roller, is also found. The mainstream and roller thicknesses can also be derived. This model may be used to derive the average shear stress exerted by the roller on the mainstream and the related exact expression for the total power loss in the jump, allowing to demonstrate the internal consistency of the proposed conceptual scheme.</description><identifier>ISSN: 0022-1686</identifier><identifier>EISSN: 1814-2079</identifier><identifier>DOI: 10.1080/00221686.2013.805701</identifier><identifier>CODEN: JHYRAF</identifier><language>eng</language><publisher>Delft: Taylor & Francis</publisher><subject>Angular momentum balance ; Atmospheric pressure ; converging channel ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; free surface flow ; hydraulic jumps ; Hydraulics ; Hydrology ; Hydrology. 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(2011). Linear and angular momentum conservation in hydraulic jump in diverging channels. Adv. Water Res. 34(2), 227-242]. The same reasoning is applied to a linearly converging channel, and the theoretical framework, which is almost completely the same, is shown to remain valid. Using a proper mechanical scheme, an analytical solution is obtained for the free surface profile of the flow. This solution allows the determination of the sequent depths and their positions. Thus, the length of the jump, which is assumed to be equal to the length of the roller, is also found. The mainstream and roller thicknesses can also be derived. This model may be used to derive the average shear stress exerted by the roller on the mainstream and the related exact expression for the total power loss in the jump, allowing to demonstrate the internal consistency of the proposed conceptual scheme.</description><subject>Angular momentum balance</subject><subject>Atmospheric pressure</subject><subject>converging channel</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>free surface flow</subject><subject>hydraulic jumps</subject><subject>Hydraulics</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>linear momentum balance</subject><subject>Meteorology</subject><subject>radial flow</subject><subject>wave breaking</subject><issn>0022-1686</issn><issn>1814-2079</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LxDAQhoMouK7-Aw8B8dh1kvQjPYksfsGCB8VrSNNkt0ubrEmr7L83pbsePYTMwPPOMA9C1wQWBDjcAVBKcp4vKBC24JAVQE7QjHCSJhSK8hTNRiQZmXN0EcI2tnle5jP0uWqslh5LW8e3HtpYd67Tth86rJwN2n_LvnEWG-dxv9F4s6-9HNpG4e3Q7XBjR-xb-3Vj11htpLW6DZfozMg26KvDP0fvT48fy5dk9fb8unxYJYrlWZ_wyoCKJ2gOpclYWsfSGEqlKgmlSnOisozJtKhIVnDKWVVyyU1JU1BQsTm6mabuvPsadOjF1g3exoWCpCmneTyeRyqdKOVdCF4bsfNNJ_1eEBCjP3H0J0Z_YvIXY7eH4TIo2RovrWrCX5ZyIMCKkbufuMZGRZ38cb6tRS_3rfPHEPt30y8shYOG</recordid><startdate>20131001</startdate><enddate>20131001</enddate><creator>Valiani, Alessandro</creator><creator>Caleffi, Valerio</creator><general>Taylor & Francis</general><general>International Association for Hydraulic Research</general><general>Taylor & Francis Ltd</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TB</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope></search><sort><creationdate>20131001</creationdate><title>Linear and angular momentum conservation for the hydraulic jump in converging channels</title><author>Valiani, Alessandro ; Caleffi, Valerio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c365t-8bf0c108e809f534d08eff22ac9122ce81c553a47b1578283b98a8f9240c0b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Angular momentum balance</topic><topic>Atmospheric pressure</topic><topic>converging channel</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>free surface flow</topic><topic>hydraulic jumps</topic><topic>Hydraulics</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>linear momentum balance</topic><topic>Meteorology</topic><topic>radial flow</topic><topic>wave breaking</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Valiani, Alessandro</creatorcontrib><creatorcontrib>Caleffi, Valerio</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of hydraulic research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Valiani, Alessandro</au><au>Caleffi, Valerio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Linear and angular momentum conservation for the hydraulic jump in converging channels</atitle><jtitle>Journal of hydraulic research</jtitle><date>2013-10-01</date><risdate>2013</risdate><volume>51</volume><issue>5</issue><spage>601</spage><epage>607</epage><pages>601-607</pages><issn>0022-1686</issn><eissn>1814-2079</eissn><coden>JHYRAF</coden><abstract>This note is the final completion of a previously published work concerning the integral conservation of linear and angular momentum in the steady hydraulic jump in a linearly diverging channel [Valiani, A., Caleffi, V. (2011). Linear and angular momentum conservation in hydraulic jump in diverging channels. Adv. Water Res. 34(2), 227-242]. The same reasoning is applied to a linearly converging channel, and the theoretical framework, which is almost completely the same, is shown to remain valid. Using a proper mechanical scheme, an analytical solution is obtained for the free surface profile of the flow. This solution allows the determination of the sequent depths and their positions. Thus, the length of the jump, which is assumed to be equal to the length of the roller, is also found. The mainstream and roller thicknesses can also be derived. This model may be used to derive the average shear stress exerted by the roller on the mainstream and the related exact expression for the total power loss in the jump, allowing to demonstrate the internal consistency of the proposed conceptual scheme.</abstract><cop>Delft</cop><pub>Taylor & Francis</pub><doi>10.1080/00221686.2013.805701</doi><tpages>7</tpages></addata></record> |
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subjects | Angular momentum balance Atmospheric pressure converging channel Earth sciences Earth, ocean, space Exact sciences and technology free surface flow hydraulic jumps Hydraulics Hydrology Hydrology. Hydrogeology linear momentum balance Meteorology radial flow wave breaking |
title | Linear and angular momentum conservation for the hydraulic jump in converging channels |
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