Abstract
Many constitutive equations describing the flow of sediment-water mixture have been presented. Several ones are chosen for discussions, which are concerned for coarse grains-water mixture flows, and developed by assuming a laminar grain motion. It is reported in their study papers that they successfully predict the flume data obtained by themselves. However the constitutive equations yield different explanations of the same phenomena. The present study gives some results on the characteristics of these constitutive equations by solving velocity profile, sediment concentration profile, flux sediment concentration and flow resistance.
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