Agricultural Engineering > GATE 2026 > Wind Erosion
In wind erosion, the amount of soil transported varies
A
directly as the cube of the threshold wind velocity and inversely as the square of the mean soil particle diameter
B
directly as the cube of the actual wind velocity and inversely as the square of the mean soil particle diameter
C
directly as the cube of the difference in actual and threshold wind velocity and the square of the mean soil particle diameter
D
directly as the cube of the difference in actual and threshold wind velocity and the square root of the mean soil particle diameter

Correct : d

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