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本文从相关沉积、侵蚀地形、古土壤和侵蚀面等因素说明:黄土高原的侵蚀历史是由来已久的一个地质过程,而侵蚀又是发展的;侵蚀量的空间变化受控于自然因素,侵蚀量的时间变化受控于人类因素;沟谷侵蚀量的变化受沟谷面积和侵蚀强度的影响。
This paper shows that the erosion history of the Loess Plateau is a long-standing geological process, and the erosion develops again. The spatial variation of erosion volume is controlled by natural factors, erosion The change in the amount of time is controlled by human factors; the change in gully erosion is affected by the gully area and erosion intensity.