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CRITICAL UNIT STREAM POWER FOR SEDIMENT TRANSPORT
引用本文:Huang Cai an College of Hydraulic and Civil Engineering,Yangzhou University,Yangzhou 225009,ChinaChih Ted Yang Technical Service Center,U.S. Bureau of Reclamation,Denver,Colorado 80225,USA. CRITICAL UNIT STREAM POWER FOR SEDIMENT TRANSPORT[J]. 水动力学研究与进展(B辑), 2003, 15(1)
作者姓名:Huang Cai an College of Hydraulic and Civil Engineering  Yangzhou University  Yangzhou 225009  ChinaChih Ted Yang Technical Service Center  U.S. Bureau of Reclamation  Denver  Colorado 80225  USA
作者单位:Huang Cai an College of Hydraulic and Civil Engineering,Yangzhou University,Yangzhou 225009,ChinaChih Ted Yang Technical Service Center,U.S. Bureau of Reclamation,Denver,Colorado 80225,USA
摘    要:1 . INTRODUCTIONANDLITERATUREREVIEWIncipientmotionisaspecialcaseofsedimenttransport ,andthetransportrateorconcentrationiszeroorasmallvaluethen .Withtheexceptionofprobabilisticandregressionapproach ,sedimenttransportequationcanbeexpressedinoneofthefollowi…


CRITICAL UNIT STREAM POWER FOR SEDIMENT TRANSPORT
HUANG Cai-an,Chih Ted YANG. CRITICAL UNIT STREAM POWER FOR SEDIMENT TRANSPORT[J]. Journal of Hydrodynamics, 2003, 15(1)
Authors:HUANG Cai-an  Chih Ted YANG
Abstract:Yang's (1996) sediment transport theory based on unit stream power is one of the most accurate theories, but in his equations the use of product of slope and critical velocity instead for critical unit stream power is not suitable. Dimensionless critical unit stream power required at incipient motion can be derived from the principle of conservation of power as a function of dimensionless particle diameter and relative roughness. Based on a lot of data sets, this new criterion was developed. By use of this new criteria, Yang's (1973) sand transport formula and his 1984 gravel transport formula could be improved when sediment concentration is less than about 100 ppm by weight.
Keywords:sediment transport   unit stream power   incipient motion
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