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Experimental Study on Silt Incipient Motion Under Wave Action
作者姓名:洪大林  高亚军  谢瑞  姬昌辉  申霞
作者单位:State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering Nanjing Hydraulic Research Institute,State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,Nanjing 210029,China,Nanjing 210029,China,Nanjing 210029,China,Nanjing 210029,China,Nanjing 210029,China
基金项目:国家高技术研究发展计划(863计划)
摘    要:Experiments on silt incipient motion under wave action were carried out.Under wave action,for different wave periods,water depths and bulk densities of silt,the shear stress or height of waves for incipient motion was determined,and a relation between the shear stress and bulk density of silt was established.Results indicate that the critical shear stress depends on the structure of the silt itself,related to the tightness between the grains(or bulk density).Exterior condition is only an external cause of silt incipient motion,and the critical shear stress for the incipient motion is the token of exterior condition.

关 键 词:波浪  压力  海水  分析方法

Experimental Study on Silt Incipient Motion Under Wave Action
HONG Da-lin,GAO Ya-jun,XIE Rui,JI Chang-hui,SHEN Xia.Experimental Study on Silt Incipient Motion Under Wave Action[J].China Ocean Engineering,2007,21(4):677-688.
Authors:HONG Da-lin  GAO Ya-jun  XIE Rui  JI Chang-hui  SHEN Xia
Institution:State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineerirng, Nanjing Hydraulic Research Institute, Nanjing 210029, China
Abstract:Experiments on silt incipient motion under wave action were carried out.Under wave action,for different wave periods,water depths and bulk densities of silt,the shear stress or height of waves for incipient motion was determined,and a relation between the shear stress and bulk density of silt was established.Results indicate that the critical shear stress depends on the structure of the silt itself,related to the tightness between the grains(or bulk density).Exterior condition is only an external cause of silt incipient motion,and the critical shear stress for the incipient motion is the token of exterior condition.
Keywords:wave  silt  incipient motion  bulk density  shear stress
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