Case Study of College Veng Road Section Landslide, Aizawl, Mizoram, India

R. Verma
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引用次数: 1

Abstract

Landslide is a very common feature along highways, roads and inhabited areas, in and around Mizoram. It is one of the most problematic hazards in the region. The present case of landslide, is in the ‘College Veng’ road section. It lies in the south eastern parts of the Aizawl town. This section is situated along the Sikulpuikawn-Bethlehem Veng road. The Coordinates of the “College Veng” slide are between 23°43՛28.56՛՛/92°43՛28.28՛՛ to 23°43՛28.56՛՛/92°43՛28.34՛՛. The slide took place on 17th September, 2017, at mid night. The section had a relatively high amount of dip (48°-50°), and has a lithology comprising of Shale and Sandstone intercalation. The total length of the slide section along the road was 75 feet, with a height of 25 feet. After the critical observation of the incidence, the major aggravating factors were found to be that the heavy rainfall induced the top most shale bed to move down the dip slope. Improper sewage and subsequent mud erosion at the bottom of the shale layer, further accelerated the down slope movement of the slided block.
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印度米佐拉姆邦Aizawl College Veng公路段滑坡案例研究
在米佐拉姆邦及其周边的高速公路、道路和居民区,滑坡是一个非常常见的特征。这是该地区最棘手的危险之一。本次滑坡发生在“学院峰”路段。它位于Aizawl镇的东南部。这一段位于Sikulpuikawn-Bethlehem Veng路。“学院风”幻灯片的坐标在23°43 28.56 /92°43 28.28 到23°43 28.56 /92°43 28.34 之间。滑坡发生在2017年9月17日午夜。该段倾角较大(48°-50°),岩性为页岩和砂岩夹层。沿着道路的滑坡部分的总长度为75英尺,高度为25英尺。通过对发生率的临界观测,发现主要的加重因素是强降雨导致最顶部的页岩层向倾斜斜坡下移。泥岩层底部污水处理不当及后续泥浆侵蚀,进一步加速了滑块的下坡运动。
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