提出了饱和黄土流滑破坏的产生条件和利用稳态强度判断饱和黄土能否产生液化流滑的方法。
Occurrence conditions of liquefaction for loess and the judgment method of flow slide of saturated loess by steady state strength are presented.
黄土泥流是黄土地区一类重要的灾害地貌过程，是泥石流的一个特殊类型，是水土流失的一种特殊形式，也是山地环境恶化、水土流失极严重的标志。
Triggered by outburst flood, mudflow is a kind of debris flow and also a form of soil erosion, and it is an indicator of the most serious soil erosion process in the Loess Plateau.
强震引发土石流，曾经位在西苏门答腊巴东帕里亚曼，如画的山林美景，如今被厚重的黄土夷为平地。
The massive earthquake brought down a landslide this beautiful mountain valley in the Padang Pariaman region of West Sumatra, leveling the ground and turning it into a wasteland .
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