the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Understanding soil loss in Mollisol permanent gully head cuts through hydrological and hydromechanical responses
Shoupeng Wang
Dongshuo Zheng
Yan Zhang
Jie Tang
Yanru Wen
Jie Dong
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We carried out a series of field studies on woodland and shrubland slopes on China’s Loess Plateau. We found that woodland slopes allow water to move deeper into the ground, which helps them remain more stable, whereas shrubland slopes tend to hold more water near the surface and are more likely to fail. This means that landslides may play a bigger role in moving soil than previously thought, so soil loss on the Loess Plateau should be re-evaluated rather than linked only to surface runoff.
We carried out a series of field studies on woodland and shrubland slopes on China’s Loess Plateau. We found that woodland slopes allow water to move deeper into the ground, which helps them remain more stable, whereas shrubland slopes tend to hold more water near the surface and are more likely to fail. This means that landslides may play a bigger role in moving soil than previously thought, so soil loss on the Loess Plateau should be re-evaluated rather than linked only to surface runoff.