滑坡治理过程中岩土体变形场的演绎趋势分析——以西(昌)木 (里)路新烧房滑坡为例

以西(昌)木(里)路新烧房滑坡为例 ,运用FEM数值计算方法比较详尽地分析了处于天然,开挖及治理状态下滑坡体及邻近岩土 体变形场的演绎过程,明晰了滑坡所处岩土环境的变形演绎趋势及过程,与实际情况符.该 方法对于评价、分析滑坡的稳定性态及治理效果具有重要的参考借鉴作用.,Landslide is a kind of universal and serious geologi cal disaster, which usually has characters suchas high happening frequency、high destroy force and many kinds of destroy performs. In modern highway engineering ,because highway is wider and has the higher amount of transport,it has higher demand for the stability of highways slopes.In the paper,taking the XinShao fang landslide in the Highway from Xichang to Muli as example, applying mathemat ical method of calculation and analysis, the author analyse the developing tende ncy of the rock and land mass deformation in the course of harnessing landslid e. This method is feasible and the analyzing result is prototype to some extend, which have value to analyze the slopes stability and harnessing landslide.,     

从泥石流沟的岩土稳定性论冲淤变动型泥石流的物源问题——以西（昌）木（里）路平川泥石流为例

本文以极具典型的平川泥石流为例比较全面的分析了冲淤变动型泥石流的物源问题。根据现场调研及室内岩土分析进行的研究成果显示,川西南高山深谷地区的大型泥石流沟中的松散土体以中、粗粒段为主,其分布与地形密切相关,位于泥石流沟中,前部位的松散土体的稳定性最差,是补给泥石流的重要物源;松散土体的发育主要受控于地质及岩土环境,人类活动只能影响松散土体的稳定性。     

从泥石流沟的岩土稳定性论冲淤变动型泥石流的物源问题——以西[ BF (昌)木(里)路平川泥石流为例

本文以极具典型的平川泥石流为例比较全面的分析 了冲淤变动型泥石流的物源问题.根据现场调研及室内岩土分析进行的研究成果显示,川西 南高山深谷地区的大型泥石流沟中的松散土体以中、粗粒段为主,其分布与地形密切相关; 位于泥石流沟中、前部位的松散土体的稳定性最差,是补给泥石流的重要物源;松散土体的 发育主要受控于地质及岩土环境,人类活动只能影响松散土体的稳定性.,The authors discuss roundly source of loose earth fo r impact-deposit debris flow to develop taking pingchuan debris flow,one of the quite typical impact-deposit debris flows in southwest sichuan province,as an example in this paper. on the basis of detailed investigations in-situ,geotechn ial testing in Lab and theory analysis,all results indicate obviously that moder ate and bulky loose earth in giant debris flow situating in southwest sichuan mo untainous area are main institute,whose tribulation are consistent with landform s.Loose earth locating in mid-forepart catchment are quite unstable,so often be comes main source of loose earth of debris flow.Formation of loose earth is cont rolled principally by geologic and geotechnical environment while human actions is the secondary factor for loose earth to form.In many times,human actions prov ide loose earth through loose earth stability.,