Soil erosion assessment and prediction play critical roles in addressing problems associated with erosion control and environmental rehabilita-tion. The past dynamics of soil erosion can provide information valuable for under standing the relation of soil erosion to environmental change and anthropogenic activity. The Chinese Loess Plateau was once a high, flat plain in northwestern China, but now more than 70% of the area is gully-hill dominated, owing to massive soil erosion during the later Quaternary and human-induced accelerated soil erosion in recent centuries. The present article investigates the dynamics of erosion during the Holocene and the driving forces of human activities and bio-climatic changes. Modern soil erosion on the Loess Plateau is a combination of intensive natural erosion and human-induced erosion, the latter being 4 times as intense as the former.
CITATION STYLE
He, X., Tang, K., & Zhang, X. (2004). Soil erosion dynamics on the Chinese Loess Plateau in the last 10,000 years. Mountain Research and Development, 24(4), 342–347. https://doi.org/10.1659/0276-4741(2004)024[0342:sedotc]2.0.co;2
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