In an open-channel, Fr = V / sqrt(g y). If velocity is constant and depth y doubles, what happens to Fr?

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Multiple Choice

In an open-channel, Fr = V / sqrt(g y). If velocity is constant and depth y doubles, what happens to Fr?

Explanation:
The Froude number in open-channel flow is Fr = V / sqrt(g y), which compares inertial forces to gravitational forces. If the velocity is kept constant and the depth doubles, the term sqrt(g y) in the denominator becomes sqrt(g · 2y) = sqrt(2) · sqrt(g y). That makes the new Fr equal to V / [sqrt(2) · sqrt(g y)] = (1/√2) · [V / sqrt(g y)] = Fr_original / √2. So the Froude number decreases by a factor of √2; it becomes smaller to reflect the relatively stronger influence of gravity at the greater depth. If you relate this to flow regimes, the flow shifts toward more subcritical as Fr decreases.

The Froude number in open-channel flow is Fr = V / sqrt(g y), which compares inertial forces to gravitational forces. If the velocity is kept constant and the depth doubles, the term sqrt(g y) in the denominator becomes sqrt(g · 2y) = sqrt(2) · sqrt(g y). That makes the new Fr equal to V / [sqrt(2) · sqrt(g y)] = (1/√2) · [V / sqrt(g y)] = Fr_original / √2. So the Froude number decreases by a factor of √2; it becomes smaller to reflect the relatively stronger influence of gravity at the greater depth. If you relate this to flow regimes, the flow shifts toward more subcritical as Fr decreases.

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