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The Malan loess is a greyish yellow unstratified sediment with uniform lithology, large pores and loose texture. The Malan loess is sensitive to water due to its porous and metastable structure. Water‐induced disintegration is the main cause of soil loss in the Loess Plateau of China and the primary evolutionary driving force of the loess landform. A series of laboratory tests is conducted on undisturbed...
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