A Siltation Simulation and Desiltation Measurement Study Downstream of the Suzhou Creek Sluice, China
The Suzhou Creek Sluice is currently the largest underwater plain gate in the world, with a single span of 100 m. It is located in a tidal estuary at the junction of the Huangpu River and Suzhou Creek in Shanghai, China. In this study, physical and 2D vertical mathematical models were used to invest...
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Veröffentlicht in: | China ocean engineering 2013-12, Vol.27 (6), p.781-793 |
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description | The Suzhou Creek Sluice is currently the largest underwater plain gate in the world, with a single span of 100 m. It is located in a tidal estuary at the junction of the Huangpu River and Suzhou Creek in Shanghai, China. In this study, physical and 2D vertical mathematical models were used to investigate and distinguish the mechanism of siltation downstream of an underwater plain gate from that of other gates types. According to quantitative data obtained by site investigation and the application of the physical hydrodynamic models, it was found that the characteristics of the tidal estuary as well as the fact that the sluice span is equal to the creek width are the major reasons contributing to siltation. A possible desiltation treatment system is proposed for the underwater plain gate. The system includes selection of a suitable location that allows the determination of a reasonable top elevation of the sluice floor, reserving sufficient space under the gate to accommodate siltation, setting up a mechanical desiltation system, and flushing silt along with overflow over the top of the gate. Furthermore, on-site hydraulic silt flushing experiments and a topography survey were conducted. These results showed that the measurement system is effective, and by maintaining this scheduled operation once a month, the downstream riverbed has been maintained in a good condition. |
doi_str_mv | 10.1007/s13344-013-0064-2 |
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Furthermore, on-site hydraulic silt flushing experiments and a topography survey were conducted. 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It is located in a tidal estuary at the junction of the Huangpu River and Suzhou Creek in Shanghai, China. In this study, physical and 2D vertical mathematical models were used to investigate and distinguish the mechanism of siltation downstream of an underwater plain gate from that of other gates types. According to quantitative data obtained by site investigation and the application of the physical hydrodynamic models, it was found that the characteristics of the tidal estuary as well as the fact that the sluice span is equal to the creek width are the major reasons contributing to siltation. A possible desiltation treatment system is proposed for the underwater plain gate. The system includes selection of a suitable location that allows the determination of a reasonable top elevation of the sluice floor, reserving sufficient space under the gate to accommodate siltation, setting up a mechanical desiltation system, and flushing silt along with overflow over the top of the gate. Furthermore, on-site hydraulic silt flushing experiments and a topography survey were conducted. These results showed that the measurement system is effective, and by maintaining this scheduled operation once a month, the downstream riverbed has been maintained in a good condition.</description><subject>Brackish</subject><subject>China</subject><subject>Coastal Sciences</subject><subject>Desilting</subject><subject>Desilting basins</subject><subject>Engineering</subject><subject>Fluid flow</subject><subject>Fluid- and Aerodynamics</subject><subject>Flushing</subject><subject>Gates</subject><subject>Marine</subject><subject>Marine & Freshwater Sciences</subject><subject>Numerical and Computational Physics</subject><subject>Oceanography</subject><subject>Offshore Engineering</subject><subject>Simulation</subject><subject>Sluices</subject><subject>Underwater</subject><subject>中国</subject><subject>机械清淤</subject><subject>水闸底板</subject><subject>泥沙淤积</subject><subject>流体动力学模型</subject><subject>测量系统</subject><subject>潮汐河口</subject><subject>苏州河</subject><issn>0890-5487</issn><issn>2191-8945</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkEtv1TAQhS0EEpfCD2BndiwIjJ-xl9Utj0pFLC6sLceZ9KYkdmvHqsqvJ1epuoTVHGnOmcdHyFsGHxlA-6kwIaRsgIkGQMuGPyM7zixrjJXqOdmBsdAoadqX5FUpNwCKKcl2BM_pYZwWv4wprmqu0yZ97OkFlqfWd_SlZpwxLvSw1P6BXqT7WJaMfqZpoMsR6aH-OaZK9xnxNz1MdQz4ge6PY_SvyYvBTwXfPNYz8uvL55_7b83Vj6-X-_OrJggDS9OxQRvQAttBdMEq24IOomWaQw-DCJzJ1gTeg-m6Xlnfhb63Q9dp0dmAehBn5P029zanu4plcfNYAk6Tj5hqcUxLzg1Tiv_fqlas2jLWrla2WUNOpWQc3G0eZ58fHAN3ou82-m6l70703Wk83zJl9cZrzO4m1RzX5_8Zeve46Jji9d2ae9okDZdarnf_Ba7jkvI</recordid><startdate>20131201</startdate><enddate>20131201</enddate><creator>季永兴 杨绯 张汉云 卢永金</creator><general>Springer Berlin Heidelberg</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20131201</creationdate><title>A Siltation Simulation and Desiltation Measurement Study Downstream of the Suzhou Creek Sluice, China</title><author>季永兴 杨绯 张汉云 卢永金</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c380t-b1f68063e7f3bc959706c371620d0f3c21478c2d08bbd59abcdd9fbb63b9ce6f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Brackish</topic><topic>China</topic><topic>Coastal Sciences</topic><topic>Desilting</topic><topic>Desilting basins</topic><topic>Engineering</topic><topic>Fluid flow</topic><topic>Fluid- and Aerodynamics</topic><topic>Flushing</topic><topic>Gates</topic><topic>Marine</topic><topic>Marine & Freshwater Sciences</topic><topic>Numerical and Computational Physics</topic><topic>Oceanography</topic><topic>Offshore Engineering</topic><topic>Simulation</topic><topic>Sluices</topic><topic>Underwater</topic><topic>中国</topic><topic>机械清淤</topic><topic>水闸底板</topic><topic>泥沙淤积</topic><topic>流体动力学模型</topic><topic>测量系统</topic><topic>潮汐河口</topic><topic>苏州河</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>季永兴 杨绯 张汉云 卢永金</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</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>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>China ocean engineering</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>季永兴 杨绯 张汉云 卢永金</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A Siltation Simulation and Desiltation Measurement Study Downstream of the Suzhou Creek Sluice, China</atitle><jtitle>China ocean engineering</jtitle><stitle>China Ocean Eng</stitle><addtitle>China Ocean Engineering</addtitle><date>2013-12-01</date><risdate>2013</risdate><volume>27</volume><issue>6</issue><spage>781</spage><epage>793</epage><pages>781-793</pages><issn>0890-5487</issn><eissn>2191-8945</eissn><abstract>The Suzhou Creek Sluice is currently the largest underwater plain gate in the world, with a single span of 100 m. It is located in a tidal estuary at the junction of the Huangpu River and Suzhou Creek in Shanghai, China. In this study, physical and 2D vertical mathematical models were used to investigate and distinguish the mechanism of siltation downstream of an underwater plain gate from that of other gates types. According to quantitative data obtained by site investigation and the application of the physical hydrodynamic models, it was found that the characteristics of the tidal estuary as well as the fact that the sluice span is equal to the creek width are the major reasons contributing to siltation. A possible desiltation treatment system is proposed for the underwater plain gate. The system includes selection of a suitable location that allows the determination of a reasonable top elevation of the sluice floor, reserving sufficient space under the gate to accommodate siltation, setting up a mechanical desiltation system, and flushing silt along with overflow over the top of the gate. 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subjects | Brackish China Coastal Sciences Desilting Desilting basins Engineering Fluid flow Fluid- and Aerodynamics Flushing Gates Marine Marine & Freshwater Sciences Numerical and Computational Physics Oceanography Offshore Engineering Simulation Sluices Underwater 中国 机械清淤 水闸底板 泥沙淤积 流体动力学模型 测量系统 潮汐河口 苏州河 |
title | A Siltation Simulation and Desiltation Measurement Study Downstream of the Suzhou Creek Sluice, China |
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