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Landslide in fractured and stratified rocks: A case from Aizawl, Mizoram, India

机译:裂缝和分层岩石的滑坡:来自印度的Aizawl,Mizoram的一个案例

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Stratified rock cut slopes for e.g. shale-sandstone-siltstone layers are a common occurrence in some part of the Himalayas. These rocks are highly jointed and bears low strength to sustain significant engineering load. A similar geological condition exists in the north eastern Himalayas (Aizawl, Mizoram) where such rocks have been exposed along cut slopes. The area receives heavy rainfall during the monsoonal months and the presence of clay make these rocks highly susceptible to intense weathering. Further, the presence of widely spaced orthogonal joints along with persistent bedding parallel joints allow water to percolate deeper into the formation. Accumulation of water with time in the pore spaces of rocks and in the interface between the strata leads to opening of the joints and considerable reduction of shear strength. Despite of incompetency of these rocks, large number of transportation lines and settlements are being built to meet the demand of increasing population in India. Unscientific design and inadequate use of geological and geotechnical information during construction allow these rocks to deteriorate and degrade in strength before the engineering life of the structure eventually leading to slope failure and mass destruction. Therefore, the present study mainly deals with the influence of long term weathering on the strength degradation of the exposed rocks by a series of experimental observations followed by numerical simulation of cut slope using distinct element method. The purpose is to gauge into the health of the slope and the processes which leads to slope failure under normal gravity and hydro-mechanical loading conditions. The result of this analysis is very promising which discusses several important issues like effective loading direction, maximum allowed load on the crest of the slope, zones of maximum displacement and maximum flow rate observed along the slope face, mode and depth of failure plane. Understanding these challenges will assist the planners to design appropriate support systems for long term safety and sustainability of the structures and avoid future slope failure.
机译:分层岩石切口斜坡。 Shale-Sandstone-Siltstone层是喜马拉雅山的某些部分的常见情况。这些岩石具有高度关联,并且具有低强度以维持显着的工程载荷。北东喜马拉雅山(Aizawl,Mizoram)存在类似的地质条件,其中这些岩石沿着剪切斜坡暴露。该地区在季风月期间收到大雨,粘土的存在使这些岩石高度易受强烈的风化。此外,随着持久的床上用品平行接头的存在宽带间隔的正交关节允许水渗透到地层中。随着时间的推移在岩石的孔隙空间中积聚水分,在地层之间的界面导致接头的打开,剪切强度的显着降低。尽管这些岩石有着不称谓,正在建立大量的运输线和定居点,以满足印度人口增加的需求。在施工期间,使用地质和岩土信息信息的不科学设计和使用这些岩石在结构的工程生活中最终导致坡度破坏和大规模破坏之前,这些岩石在力量下劣化和降低。因此,本研究主要涉及长期风化对暴露岩石强度降解的影响,通过一系列实验观察,然后使用不同的元素法进行数值模拟。目的是衡量坡度的健康和过程,导致正常重力和水力机械负载条件下的斜率发生故障。该分析的结果非常有前途,讨论了有效的装载方向等几个重要问题,斜坡嵴上的最大允许负载,最大位移区域和沿着斜坡面观察的最大流速,失效平面的模式和深度观察到的最大流速。了解这些挑战将有助于规划人员为长期安全和结构的可持续性设计适当的支持系统,并避免未来的斜坡故障。

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