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Resistance relationships for alluvial channel flow
Reliability of resistance relationships given by Einstein-Barbarossa, Liu-Hwang, and Shen was studied on basis of available data from flumes, canals, and natural streams; study has revealed that these relationships do not predict resistance of alluvial stream satisfactorily over wide range of pertinent variables; further analysis of these data has indicated that certain parameters described can be used to predict resistance of alluvial stream; flume data collected with materials having different specific gravities are also used in obtaining this resistance relationship; proposed relationship yields decreasing values of `n' with increase in stage over large range of depth.
Resistance relationships for alluvial channel flow
Reliability of resistance relationships given by Einstein-Barbarossa, Liu-Hwang, and Shen was studied on basis of available data from flumes, canals, and natural streams; study has revealed that these relationships do not predict resistance of alluvial stream satisfactorily over wide range of pertinent variables; further analysis of these data has indicated that certain parameters described can be used to predict resistance of alluvial stream; flume data collected with materials having different specific gravities are also used in obtaining this resistance relationship; proposed relationship yields decreasing values of `n' with increase in stage over large range of depth.
Resistance relationships for alluvial channel flow
ASCE -- Proc (J Hydraulics Div)
Garde, R.J. (author) / Ranga Raju, K.G. (author)
1966
24 pages
Article (Journal)
English
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