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The fly ash and cesium-137 determined erosion amounts and annual soil erosion rate for cropland landscapes positions were highest for the upper and lower backslopes.
On the hillslopes, soil loss by tillage erosion amounts to 26.6 ton ha− 1 y− 1 while sedimentation occurs at a rate of 21.1 ton ha− 1 y− 1.
DSK interprets the behavior of slope change in the watershed with positive (negative) values pointing to high erosion amounts in the upper (lower) regions of the watershed; hence, the positive value of DSK was an indication of accelerated forms of erosion in the upper reaches and dominance of fluvial landforms (Luo 2000).
On this basis, using the LAndscape Management and Planning Tool for the Mo River basin (LAMPT_Mo), we (1) modelled soil erosion patterns in relation with land use/cover change (LUCC), land protection regime, and landforms, and (2) examined the efficiency of landscape redesign options on soil erosion amounts at basin scale.
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The increase of water yield can accumulate the soil erosion amount.
The improvement of NPP is good for decreasing water yield and soil erosion amount and increasing soil conservation amount.
The ratio of erosion amount increases faster (0.15 %) when B D increases by 0.1, for values of B D greater than 0.5.
These methods provide a way to document past cropland soil erosion amount and rates for three different time periods (1910 to 1960, 1960 to 2009 and 1910 to 2009).
The highest surface runoff coefficient and erosion amount were found on bare land in all five rainfall regimes, and the lowest were found on grass cover.
With a constant value of A D = 0.2, the ratio of erosion amount increases by 0.1%% when B D increases by 0.1, for values of B D less than 0.5.
The excess pore water pressure can reduce the resistance to shear stress from the erodible bed and lead to a higher erosion amount and longer moving distance of the landslide.
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