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Soil loss begins at the bedrock interface.
That means more flooding, more soil loss, more siltation, more trouble all round.
The soil loss due to interrill erosion was obtained by subtracting soil loss through rill erosion from the total soil loss measured in the Gerlarch troughs.
Soil loss is one of the greatest catastrophes facing the world today.
Rainstorms ≥30 mm were important for runoff and soil loss.
Sheet erosion was the major form of soil loss.
Land use and management influence the magnitude of soil loss.
Vegetative barriers impeded run-off and controlled soil loss.
For leucaena barriers, soil loss increased quadratically with rainfall.
To analyze correlations between the landscape indicator and soil loss processes, variables expressing soil loss status should be first quantified.
We applied the Revised Soil Loss Equation RUSLEE) to assess levels of soil loss in a Geographic Information System (GIS).
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