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波、流共同作用下的泥沙起动
引用本文:曹祖德,孔令双,焦桂英.波、流共同作用下的泥沙起动[J].海洋学报,2003,25(3):113-119.
作者姓名:曹祖德  孔令双  焦桂英
作者单位:1.交通部, 天津水运工程科学研究所, 天津, 300456
基金项目:华东师范大学河口海岸动力沉积和动力地貌综合国家重点实验室高访学者基金会资助项目(00-1-3)。
摘    要:对波、流共存时的床面剪切力及摩阻系数等作了探讨,根据泥沙起动试验,建立了泥沙起动Shields曲线,导出了波、流共同作用下层流和紊流时的泥沙起动公式和起动波高、起动水深.

关 键 词:波、流共同作用    边界层    床面剪切力    泥沙起动
文章编号:0253-4193(2003)03-0113-07
收稿时间:2002/1/18 0:00:00
修稿时间:2002年1月18日

Initiation of sediment movement for a wave-current coexistent system
CAOZu-de,KONG Ling-shuang and JIAO Gui-ying.Initiation of sediment movement for a wave-current coexistent system[J].Acta Oceanologica Sinica (in Chinese),2003,25(3):113-119.
Authors:CAOZu-de  KONG Ling-shuang and JIAO Gui-ying
Institution:1.Tianjin Research Institute of Water Transport Engineering, Tianjin 300456, China2.Qingdao College of Architecture and Engineering, Qingdao 266033, China3.Marine Disaster Alleviation Research Institute, Ocean University of China, Qingdao 266003, China
Abstract:Bed shear stress and friction coefficient have been studied. Based on the critical condition for the initiation of sediment movement by means of a lot of test data for a wave - current coexistent system, formulas of sediment initial movement for both laminar and turbulent have been set up, and wave height and water depth for initiation of sediment movement are given as well.
Keywords:wave-current coexistent system  boundary layer  bed shear stress  initiation of sediment movement  wave height for initiation of sediment movement  water depth for initiation of sediment movement
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