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.
研究成果可作为青藏高原东北部黄土区采用优势护坡灌木植物，防治坡面浅层滑坡、崩塌、泥石流等地质灾害发生的理想依据之一。
The achievements can be taken as criteria for choosing shrubs for protecting slope and preventing shallow landslide, collapsing and debris flow in loess area of northeast qinghai-tibetan plateau.
谷风产生的大片类黄土堆积与滑坡体共同参与泥石流的形成；
Under the influence of the gully wind, there is filled with lots of wind accumulated deposit which triggers the form of debris flow with landslides;
谷风产生的大片类黄土堆积与滑坡体共同参与泥石流的形成；
Under the influence of the gully wind, there is filled with lots of wind accumulated deposit which triggers the form of debris flow with landslides;
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