Flow resistance of gravel bed channels

Existing resistance formulas produce a wide range of friction-factor estimates for gravel bed streams. The purpose of this paper is to develop a reliable resistance formula in terms of the Darcy-Weisbach friction factor f Published data were screened and used to establish the formula. The existing f...

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Bibliographic Details
Published inInternational journal of sediment research Vol. 29; no. 1; pp. 126 - 132
Main Authors WANG, Wen C., DAWDY, David R.
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.03.2014
Multech Engineering Consultants, Inc. 1650 Zanker Road, Suite 210, San Jose, CA 95112
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ISSN1001-6279
DOI10.1016/S1001-6279(14)60028-7

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Summary:Existing resistance formulas produce a wide range of friction-factor estimates for gravel bed streams. The purpose of this paper is to develop a reliable resistance formula in terms of the Darcy-Weisbach friction factor f Published data were screened and used to establish the formula. The existing formulas have considered thatfis a function of relative roughness D84/R only, where R is the hydraulic radius and 1984 is the particle size referred to the intermediate diameter that equals or exceeds that of 84 percent of bed sediments. In this paper, f is considered as a ftmction of Froude number in addition to the relative roughness, ffor D84/R〉l displays a different trend than that for Dsn/R〈l perhaps due to the invalid assumption of a logarithmic velocity distribution for D84/R〉l. Anfformula for Dsa/R〈l has been established.
Bibliography:Existing resistance formulas produce a wide range of friction-factor estimates for gravel bed streams. The purpose of this paper is to develop a reliable resistance formula in terms of the Darcy-Weisbach friction factor f Published data were screened and used to establish the formula. The existing formulas have considered thatfis a function of relative roughness D84/R only, where R is the hydraulic radius and 1984 is the particle size referred to the intermediate diameter that equals or exceeds that of 84 percent of bed sediments. In this paper, f is considered as a ftmction of Froude number in addition to the relative roughness, ffor D84/R〉l displays a different trend than that for Dsn/R〈l perhaps due to the invalid assumption of a logarithmic velocity distribution for D84/R〉l. Anfformula for Dsa/R〈l has been established.
11-2699/P
Flow resistance, Darcy-Weisbach friction factor, Relative roughness, Relative submergence, Gravel bedchannels, Open channels
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ISSN:1001-6279
DOI:10.1016/S1001-6279(14)60028-7