1) rock glacier side
石流坡
1.
Research purposes:The rock glacier side s sort,distribution range,distribution thickness,geological cause and stability etc are made clear by making integrated survey and on which the influence on railway construction is evaluated for the purpose of presenting the resolution to the railway crossing talus area.
研究目的:通过采用综合勘察准确地查明石流坡的分类、分布范围、分布厚度、地质成因、稳定程度等,评价其对铁路工程的影响,为线路安全通过岩堆提出解决方案。
2) slope debris flow
坡面泥石流
1.
Taking the Beibei of Chongqing City as an example,the paper analyzes the self-organization criticality of solid loose materials,and the criticality of geomorphology and rainfall while slope debris flow occurs.
坡面泥石流是山区常见的一种自然灾害。
2.
On the basis of analyzing general characters of slope debris flow triggered by landslides or collapses , the authors apply the debris flow of 1995 in Wuming gully as a model, which occurs a time in a hundred years.
在分析崩滑坡面泥石流的基本特征和其峰值流速流量一般规律的基础上 ,以康定雅拉河无名沟 1 995年的百年一遇泥石流为研究示范 ,在了解该流域的基本特征 ,分析该次泥石流的形成、容重、颗粒组成等基本特性的基础上 ,用弯道超高的理论和用古乡沟泥石流建立的流速计算公式 ,计算测量断面的流速及泥石流峰值流速沿程变化。
3.
The possibility of slope debris flow occurrence is the difficulty area and importance area ofgeography.
本文在对重庆市北碚区坡面泥石流进行大量研究的基础上，从研究区泥石流的形成条件着手，重点分析了研究区坡面泥石流形成的降雨条件。
3) hill slope debris flow
山坡泥石流
1.
Vulnerability assessment of site with hill slope debris flow;
山坡泥石流场地易损性评价
2.
The preliminarily discussion of site-specific vulnerability of hill slope debris flow was made and the assessment method and formula were given.
鉴于山坡泥石流的危险性主要表现为冲击破坏作用,运用能量守恒原理,将泥石流场地危险性评价公式改进为“危险度=能量×频率”。
4) debris flow on slope
坡面泥石流
1.
Based on dynamic geomorphology,general developing model for debris flow on slope was put for- ward.
运用动力地貌学方法提出了坡面泥石流演化模式;从几何相似、模型土体和降水装置三方面构建了坡面泥石流半定量-定性物理试验模型,拟定了模型试验过程,降雨历时140～300min,其中第0～70min属于前期降雨阶段,降雨速度控制在1。
5) landslide and debris flow
滑坡泥石流
1.
Meanwhile, Lanzhou is one of the cities that severely threatened by landslide and debris flow.
同时兰州又是在中国各大城市中,滑坡泥石流频发率较高,受危害最严重的城市之一。
2.
The correlation among rainfall, landslide and debris flow is revealed with the moisture content distribution changed.
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。
6) Mud-rock flow and landslip
泥石流滑坡
1.
Mud-rock flow and landslip often happen on the east side of Qinghai-Xizang Plateau, and the severe precipitation is the main cause of the mud-rock flow and landslip events.
青藏高原东部是泥石流滑坡灾害的多发区, 强降水是产生泥石流滑坡灾害的主要原因。
补充资料：石流
1.石山中的溪流。 2.在山岳地区大小不同的岩块沿斜坡滑动的现象。通常是由于岩块下面的粘性土被水浸湿后滑动所引起。
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