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Statistical analysis of excavation model of the loess landslide developmental characteristics

机译:黄土滑坡发育特征挖掘模型的统计分析

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In recent years, with the increasing of excavation activity, caused the landslide more and more increasing, the landslide occurred gradually aroused public concern. For typical loess landslides caused by excavation, respectively from the distribution features of the landslide, landslide characteristics after wall, slope high on the impact of landslides and landslides trailing edge fracture characteristics were analyzed. Statistics show that the engineering loess landslides in the distribution respectively are selectivity of landform, strata of selectivity and zonal distribution. The excavation methods are rapid excavation and "eating" excavation. Landslide back wall angle is between 60-80°. The height of the scarp is between 3-20m, controlled by the thickness of the Malan loess. The slope high is more than 60m, with the increase of height. The risk of slide is higher. Trailing edge crack development is "wild goose feather" type and "bilateral ears" type. It provides conditions for trailing edge of evolution.
机译:近年来,随着挖掘活动的增加,导致滑坡越来越多,山体滑坡逐渐激起了公众关注。对于由挖掘引起的典型黄土滑坡,分别从滑坡的分布特征,墙壁后的滑坡特性,分析了滑坡和滑坡后坡度的影响的坡度高。统计数据显示,分布中的工程黄土滑坡分别是地貌,选择性和区域分布层的选择性。挖掘方法是快速的挖掘和“进食”挖掘。 Landslide后壁角度在60-80°之间。围巾的高度在3-20米之间,由马兰黄土的厚度控制。坡度高于60米,随着高度的增加。幻灯片的风险更高。尾部裂纹开发是“野鹅羽毛”类型和“双侧耳朵”类型。它为进化的后缘提供条件。

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