1) Collapse accumulation
崩塌堆积体
1.
Through the slope safely monitoring in Jin anqiao Hydropower Station,it is shown that the influence upon the stability of slope of B20 collapse accumulation from the excavation shear pin of the lower retaining wall and the rainfall in flood period is very sensitive,and the deformation characteristics and instability mechanism of slope of the accumulation are analyzed.
金安桥水电站边坡安全监测表明:左岸B20崩塌堆积体边坡的稳定性受下部挡墙基坑开挖切脚及汛期降雨影响十分敏感,分析了堆积体边坡的变形特征和失稳机理。
2) landslide-mass flow deposit
崩塌-块体流堆积
3) collapse deposits
崩塌堆积
1.
The collapse deposits of the 3 scenic .
结果发现组成水湫池堰塞坝的沉积物具有典型的泥砾结构;堰塞坝体外围的崩塌堆积,不仅是多期和多种成因崩塌活动的结果,而且现存的崩积砾石都覆盖在堰塞坝表面的古地形面上,层序关系表明其形成时间晚于堰塞坝。
4) engineering geologic conditions
崩塌坡积体
1.
This paper summarizes the landform and engineering geologic conditions of the left dam abutment of Yonghe Reservoir of Qingyuan County, Shanxi Province, analyzes the stratum structure and distributional characteristics of the sliding body and collapse clinosol, and analyzes the geneses of the sliding body and collapse clinosol.
概述了沁源县永和水库左坝肩地形地貌及工程地质条件,介绍了坍滑体和崩塌坡积体的地层结构与分布特征,分析了坍滑体和崩塌坡积体的成因。
5) Cave collapse deposit
洞穴崩塌堆积
6) riverside slumping mass
崩滑堆积体
1.
Based on the analysis of the physical components,characteristics of the weak layer,the interface between the riverside slumping mass and bedrock and the characteristics of hydrogeology,combined with the numerical simulation and stability calculation,the variation of stability of the riverside slumping mass after the rising of the water level in the Three Gorges reservoir area is studied.
通过对三峡库区巴东县黄土坡滑坡临江崩滑堆积体的物质组成、软弱面特征、与基岩接触面的关系以及水文地质特征进行分析,结合数值分析和稳定性计算,阐述了三峡库区蓄水后的坡体稳定性变化,为进一步对黄土坡滑坡进行治理提供了参考。
2.
The data of shear strength experiments of the landslide slip layer used in different methods in Huangtupo landslide riverside slumping mass are analyzed.
分析了前期黄土坡滑坡临江崩滑堆积体对于滑带土采用不同方法进行抗剪强度试验的资料,结合反演分析成果,综合分析了黄土坡滑坡临江崩滑堆积体与基岩接触面软弱土层的抗剪强度,为崩滑堆积体稳定性评价提供了一定的依据。
补充资料：崩塌
| 崩塌 avalanche 陡峻山坡上岩块、土体在重力作用下 ，发生突然的急剧的倾落运动。多发生在大于60°～70°的斜坡上。崩塌的物质，称为崩塌体。崩塌体为土质者，称为土崩；崩塌体为岩质者，称为岩崩；大规模的岩崩，称为山崩。崩塌可以发生在任何地带，山崩限于高山峡谷区内。崩塌体与坡体的分离界面称为崩塌面，崩塌面往往就是倾角很大的界面，如节理、片理、劈理、层面、破碎带等。崩塌体的运动方式为倾倒、崩落。崩塌体碎块在运动过程中滚动或跳跃，最后在坡脚处形成堆积地貌——崩塌倒石锥。崩塌倒石锥结构松散、杂乱、无层理、多孔隙；由于崩塌所产生的气浪作用，使细小颗粒的运动距离更远一些，因而在水平方向上有一定的分选性。
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参考词条