米佐拉姆邦Aizawl南部地区国道岩崩分析

Zairem mawii, H. Lalhlimpuia, Lalhming Sangi, V. Vanthangliana, Laldin puia, Shivam Kumar
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引用次数: 2

摘要

以落石形式出现的边坡破坏是发生在喜马拉雅山丘陵地区的一种常见现象。作为它的一部分,米佐拉姆邦全年都经历着高比率的岩崩,尤其是在季风季节。本文的重点是在Sumsuih村Midumkham的Aizawl到Lunglei之间的国道上,通过Thenzawl频繁的岩石坠落。在研究区内,由于各种形式的滑坡,客运车辆、公共物品运输车、私家车和路障的损坏是常见的现象。2016年10月14日,一对夫妇因研究区域内的岩崩死亡,引起了政府和当地对该地区状况的关注。因此,必须对该地区进行详细研究,以减少岩崩,并向政府和当地人介绍该地区的实际情况。进行了实地侦察,以收集关节数据进行运动学分析。利用Rocscience软件Dips 6.0对岩崩行为进行运动学分析,立体图显示倾倒、平面和楔型是潜在的破坏模式。根据岩体质量等级(RMR)和边坡质量等级(SMR)对岩石层理进行分类。约90%的站点显示低RMR和低SMR值。研究区暴露岩石的RMR值表明岩体质量很差。平均站立时间为30分钟,跨度为1m,表明该地区岩石侵蚀率高。岩质边坡代表Romana分类的V类,被认为是非常糟糕的岩体,完全不稳定。岩石的回弹数和强度较低,且节理较多,决定了研究区脆弱程度高
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Rockfall Analysis of State Highway along the Southern Vicinity of Aizawl, Mizoram
Slope failure in the form of rockfall is a common phenomenon that occur in the hilly ranges of Himalayas. Mizoram, being a part of it experiences a high rate of rockfall throughout the year especially during the monsoon season. This paper focus on frequent rock fall along the State highway between Aizawl to Lunglei via Thenzawl at Midumkham, Sumsuih village. Damage of passenger vehicles, public goods carrier trucks, private vehicles and road blocks are the common phenomenon due to various forms of landslide within the study area. The death of a couple on 14th October 2016 due to rockfall within the study area captivate attention of government as well as the local about the condition of the area. Thus, detailed study of the area becomes mandatory so as to reduce rockfall and to educate the government and locals about the actual condition of the area. Field reconnaissance has been carried out to collect joint data for kinematic analysis. The behaviour of rockfall was determined by kinematic analysis using Rocscience software Dips 6.0, the stereograph shows that toppling, planar and wedge type are the potential modes of failures. The rock beddings are classified based on RMR (Rock Mass Rating) and SMR (Slope Mass Rating). About 90% of the selected site shows that low RMR as well as SMR value. The RMR values of the rock exposed in the study area indicated a very poor quality of rock mass. The average stand up time obtained 30 min for 1m span suggest high rate of erosion of rocks in the area. The rock slopes represent Class V of Romana classification, considered as very bad rock mass and completely unstable. The low value of rebound number and strength of the rock along with presence of numerous joints determined the high vulnerability of the study area
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