1)  Landslide
崩滑流
2)  collapse and slide
崩滑
1.
The moisture content of slope was measured in the tests, and the surface erosion, collapse and slide, and transfer from landslide into debris were analysed.
通过大型人工降雨滑坡泥石流试验和小型模型试验,对试验现象进行观测和含水量监测,研究暴雨条件下发生的坡面侵蚀、崩滑现象和由此引发滑坡,滑坡土体转化成泥石流的全过程,揭示了蒋家沟流域特殊环境下的暴雨、滑坡、泥石流共生关系。
3)  ancient crumble-sliding body
古崩滑体
4)  rockfall
崩滑体
1.
Simulation of rockfall at Mingshan in Fengdu by discrete element method;
丰都名山崩滑体失稳的离散元模拟
2.
This paper introduced engineering geologic conditions of Baishapo rockfall in the Three Gorge reservoir area,analysed its formation mechanism and calculated its stability under main load compo.
介绍了三峡库区白沙坡崩滑体工程地质条件,分析了其成因机制,计算了该崩滑体在多种工况下的稳定性,对其稳定性作出了评价,并给出了其防治措施的建议。
5)  landslide
崩滑体
1.
Based on the geological exploration of Nanzhu landslide,the stability analysis of the landslide is studied when the water level of the Yangtze River falls from 175 m to 125 m.
基于丰都楠竹崩滑体的地质勘察资料,对该崩滑体在长江水位从175m降至125m时的稳定性进行了计算分析,得出该工况下,崩滑体将处于可能失稳的危险状态,必须进行防治。
2.
According to the characteristics,material structure features,and the geological natures of the landslide, the calculation and evaluation for the stability of the landslide are performed with the consideration of three kinds of loading situations and residual thrust method.
根据崩滑体基本特征和工程地质条件,在考虑各种不同荷载情况下,运用剩余推力法对崩滑体稳定性进行计算和评价,提出了以抗滑桩为主的支挡结构。
3.
The Zuoyituo landslide 83 km from the Three Gorges dam,is one of the major prospecting landslides in the reservoir area of the Three Gorges,lying on the southern bank of the Changjiang River, in the Nanmuyuan Village of Badong County of Hubei Province.
:作揖沱崩滑体是三峡工程库区重点勘察研究的崩滑体之一 ,位于湖北省巴东县楠木园乡长江南岸 ,距三峡工程坝址 83km,作揖沱崩滑体东西宽为 5 40～ 72 0 m,南北长为 2 80～ 40 0 m,前缘高程为 2 0 m(水下 ) ,后缘高程为 2 80 m,体积为 413。
6)  Leipo County colluvial landslide accumulation
崩滑堆积
参考词条
补充资料：滑流
分子式：
CAS号：

性质： 在多孔物料中流动的气体，它们的平均自由程和孔穴的直径相当或比孔穴直径略小。在这种情况下，当气体通过孔穴时气体分子在孔穴的壁处发生滑动，则孔穴壁处的流动速度不等于零。这种流动称为滑流。根据滑流的特性，甚至在压力降为零时，仍具有一定的滑流流动。滑流的空穴速度高于泊谡叶方程的预测值。

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