The amount of soil transported by wind erosion depends on the wind's ability to move particles and the characteristics of the particles themselves.
Based on established principles (simplified and represented by the options), the soil transport rate is primarily influenced by the excess wind energy available to move particles beyond the minimum required (threshold velocity). It is also affected by particle size.
The relationship described in the correct option highlights two main factors:
Combining these, the amount of soil transported ($Q$) can be expressed proportionally as:
$Q \propto (V_{actual} - V_{threshold})^3 \times \sqrt{d_{mean}}$
This formula indicates that higher wind velocities exceeding the threshold significantly increase soil transport, and the influence of particle size follows a square root relationship.
In wind erosion, the maximum portion of soil is transported by the process of ____________.
A windbreak, 15 m in height and 200 m in length, is established to protect the land from wind erosion in an arid area. The minimum wind velocity at the height of 15 m above the ground required to move the most erodible soil fraction is $9.6\ m\cdot s^{-1}$. If 5-year return period wind velocity at 15 m height is $16\ m\cdot s^{-1}$ and the wind direction deviates $20^\circ$ from the line perpendicular to the windbreak, the area protected by the windbreak in ha is ________________.
[round off to 2 decimal places]