The flowrate, Q, of water in an open channel is assumed to be a function of the cross-sectional area of the channel, A, the height of the roughness of the channel surface, _∈, the acceleration of gravity, g, and the slope, So, of the hill on which the channel sits. Put this relationship into dimensionless form.

 

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Status NEW Posted 10 May 2017 02:05 PM My Price 12.00

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