1) instability of the sliding mass
崩滑体失稳
2) ancient crumble-sliding body
古崩滑体
3) rockfall
[英]['rɔkfɔ:l] [美]['rɑk'fɔl]
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。
4) landslide
[英]['lændslaɪd] [美]['lænd'slaɪd]
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。
5) sliding instability
滑落失稳
1.
Moreover, it establishes mechanical model of roof structure after first destruction, and points out that sur-hinge-point is dangerous point by analyzing mechanical condition of sliding instability and rotary instabilit.
通过分析结构滑落失稳和回转失稳的力学条件,指出危险点是上铰接点。
6) instability slide
粘滑失稳
补充资料:裂纹失稳扩展
分子式:
CAS号:
性质:材料内部裂纹尖端的应力场强度因子达到或超过材料的断裂韧性之后发生的裂纹快速扩展。裂纹失稳扩展将导致材料迅速断裂。
CAS号:
性质:材料内部裂纹尖端的应力场强度因子达到或超过材料的断裂韧性之后发生的裂纹快速扩展。裂纹失稳扩展将导致材料迅速断裂。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条