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Question: The speed of the water in a river is 'V near the surface. If the coefficient of viscosity of water i...

The speed of the water in a river is 'V near the surface. If the coefficient of viscosity of water is 'η\eta' and the depth of the river is 'H, then the shearing stress between the horizontal layers of water is

A

η\etaH/V

B

η\etaV/H

C

VηH\frac{V}{\eta H}

D

η\etaV/H

Answer

B, D

Explanation

Solution

Newton's law of viscosity states that the shearing stress (τ\tau) is proportional to the velocity gradient (dvdy\frac{dv}{dy}): τ=ηdvdy\tau = \eta \frac{dv}{dy} Assuming a linear velocity profile, where the velocity is 0 at the riverbed and V at the surface over a depth H, the velocity gradient is VH\frac{V}{H}. Substituting this into the formula gives: τ=ηVH\tau = \eta \frac{V}{H}