INCIPIENT MOTION OF NON-COHESIVE SEDIMENT UNDER ICE COVER-AN EXPERIMENTAL STUDY
Based on a series of experiments under both ice-covered and free surface conditions, the present article discusses the role of flow velocity and critical shear Reynolds number for incipient motion of bed material. The influence of the resistance coefficients of both the underside of the ice cover an...
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Veröffentlicht in: | Journal of Hydrodynamics 2008-02, Vol.20 (1), p.117-124 |
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description | Based on a series of experiments under both ice-covered and free surface conditions, the present article discusses the role of flow velocity and critical shear Reynolds number for incipient motion of bed material. The influence of the resistance coefficients of both the underside of the ice cover and the channel bed on the location of the maximum velocity has been discussed. In addition, the impacts of ice and composite resistance coefficients on flow velocity for incipient motion of bed material have been assessed. The diagram describing the critical shear Reynolds number and the dimensionless shear stress for the incipient motion of sediment under ice covered conditions with different under cover resistance coefficient has been established. The effects of grain size on densimetric Froude number for incipient motion of bed material have been investigated. A relationship between the densimetric Froude number for incipient motion of bed material and the median grain size of bed material as well as the roughness coefficient of channel bed and roughness coefficient of ice cover has been established. |
doi_str_mv | 10.1016/S1001-6058(08)60036-0 |
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The influence of the resistance coefficients of both the underside of the ice cover and the channel bed on the location of the maximum velocity has been discussed. In addition, the impacts of ice and composite resistance coefficients on flow velocity for incipient motion of bed material have been assessed. The diagram describing the critical shear Reynolds number and the dimensionless shear stress for the incipient motion of sediment under ice covered conditions with different under cover resistance coefficient has been established. The effects of grain size on densimetric Froude number for incipient motion of bed material have been investigated. A relationship between the densimetric Froude number for incipient motion of bed material and the median grain size of bed material as well as the roughness coefficient of channel bed and roughness coefficient of ice cover has been established.</description><identifier>ISSN: 1001-6058</identifier><identifier>EISSN: 1878-0342</identifier><identifier>EISSN: 1000-4874</identifier><identifier>DOI: 10.1016/S1001-6058(08)60036-0</identifier><language>eng</language><publisher>Singapore: Springer Singapore</publisher><subject>Engineering ; Engineering Fluid Dynamics ; Hydrology/Water Resources ; Numerical and Computational Physics ; Simulation ; 冰覆盖量 ; 原始运动 ; 电阻率</subject><ispartof>Journal of Hydrodynamics, 2008-02, Vol.20 (1), p.117-124</ispartof><rights>China Ship Scientific Research Center 2008</rights><rights>Copyright © Wanfang Data Co. Ltd. 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The influence of the resistance coefficients of both the underside of the ice cover and the channel bed on the location of the maximum velocity has been discussed. In addition, the impacts of ice and composite resistance coefficients on flow velocity for incipient motion of bed material have been assessed. The diagram describing the critical shear Reynolds number and the dimensionless shear stress for the incipient motion of sediment under ice covered conditions with different under cover resistance coefficient has been established. The effects of grain size on densimetric Froude number for incipient motion of bed material have been investigated. A relationship between the densimetric Froude number for incipient motion of bed material and the median grain size of bed material as well as the roughness coefficient of channel bed and roughness coefficient of ice cover has been established.</description><subject>Engineering</subject><subject>Engineering Fluid Dynamics</subject><subject>Hydrology/Water Resources</subject><subject>Numerical and Computational Physics</subject><subject>Simulation</subject><subject>冰覆盖量</subject><subject>原始运动</subject><subject>电阻率</subject><issn>1001-6058</issn><issn>1878-0342</issn><issn>1000-4874</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqFkVtLw0AQhYMoWC8_QQg-iILRyW52snks6aqBmpTe0Kdlm25qa5po1qL115u0FR99moH5zsxwjmWduXDjgou3AxfAdRAYvwR-hQAUHdizWi73uQPUI_t1_4scWkfGLBomAK9lJVEcRr1IxEP7MRlGSWwnd3acxE6YPIhBNBb2QHSix2Y-ijuib0ehsMNkLPpOO7bFU0_0N9N21x4MR53nE-sgU7nRp7t6bI3uxDB8cLrJfRS2u05KGX44OqAeY5QRMmUkUH4aKCSEZsiRex5JFQJOfF9lgaZBRrjHFUuVQj5VE66UT4-t6-3eT1VkqpjJRbmqivqiNNP8a71YL76lJgAcaosa_GKLv1Xl-0qbD7mcm1TnuSp0uTKSUkBEFvwLugHz0GPNRrYF06o0ptKZfKvmS1WtpQuyiUVuYpGN5xK43MQiodbhVmdqvpjp6u_z_4Tnu4MvZTF7r7VyotLXbJ5rSbC2jQCnPw1Gk8Q</recordid><startdate>20080201</startdate><enddate>20080201</enddate><creator>Wang, Jun</creator><creator>Sui, Jue-yi</creator><creator>Karney, Bryan W.</creator><general>Springer Singapore</general><general>School of Civil Engineering, Hefei University of Technology, Hefei 230009, China%Environmental Science and Environmental Engineering Program, University of Northern British Columbia, British Columbia, Canada, V2N 4Z9%Department of Civil Engineering, University of Toronto, Toronto, Ontario, Canada, M5S 1A4</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W92</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7TB</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20080201</creationdate><title>INCIPIENT MOTION OF NON-COHESIVE SEDIMENT UNDER ICE COVER-AN EXPERIMENTAL STUDY</title><author>Wang, Jun ; Sui, Jue-yi ; Karney, Bryan W.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c356t-e934553522d529a7c9a6223f6868442ca606b77af9e39f2848a5caa68dab8aa73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Engineering</topic><topic>Engineering Fluid Dynamics</topic><topic>Hydrology/Water Resources</topic><topic>Numerical and Computational Physics</topic><topic>Simulation</topic><topic>冰覆盖量</topic><topic>原始运动</topic><topic>电阻率</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Jun</creatorcontrib><creatorcontrib>Sui, Jue-yi</creatorcontrib><creatorcontrib>Karney, Bryan W.</creatorcontrib><collection>维普_期刊</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>维普中文期刊数据库</collection><collection>中文科技期刊数据库-工程技术</collection><collection>中文科技期刊数据库- 镜像站点</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>Mechanical & Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of Hydrodynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Jun</au><au>Sui, Jue-yi</au><au>Karney, Bryan W.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>INCIPIENT MOTION OF NON-COHESIVE SEDIMENT UNDER ICE COVER-AN EXPERIMENTAL STUDY</atitle><jtitle>Journal of Hydrodynamics</jtitle><stitle>J Hydrodyn</stitle><addtitle>Journal of Hydrodynamics</addtitle><date>2008-02-01</date><risdate>2008</risdate><volume>20</volume><issue>1</issue><spage>117</spage><epage>124</epage><pages>117-124</pages><issn>1001-6058</issn><eissn>1878-0342</eissn><eissn>1000-4874</eissn><abstract>Based on a series of experiments under both ice-covered and free surface conditions, the present article discusses the role of flow velocity and critical shear Reynolds number for incipient motion of bed material. The influence of the resistance coefficients of both the underside of the ice cover and the channel bed on the location of the maximum velocity has been discussed. In addition, the impacts of ice and composite resistance coefficients on flow velocity for incipient motion of bed material have been assessed. The diagram describing the critical shear Reynolds number and the dimensionless shear stress for the incipient motion of sediment under ice covered conditions with different under cover resistance coefficient has been established. The effects of grain size on densimetric Froude number for incipient motion of bed material have been investigated. A relationship between the densimetric Froude number for incipient motion of bed material and the median grain size of bed material as well as the roughness coefficient of channel bed and roughness coefficient of ice cover has been established.</abstract><cop>Singapore</cop><pub>Springer Singapore</pub><doi>10.1016/S1001-6058(08)60036-0</doi><tpages>8</tpages></addata></record> |
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subjects | Engineering Engineering Fluid Dynamics Hydrology/Water Resources Numerical and Computational Physics Simulation 冰覆盖量 原始运动 电阻率 |
title | INCIPIENT MOTION OF NON-COHESIVE SEDIMENT UNDER ICE COVER-AN EXPERIMENTAL STUDY |
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