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Slope Stability Assessment of Saptashrungi Gad Temple, Vani, Nashik, Maharashtra, India—A Numerical Approach

机译:印度马哈拉施特拉邦,瓦尼,纳西克,Saptashrungi Gad寺的边坡稳定性评估—一种数值方法

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摘要

The worship places in India are usually situated in and around the hilly regions and/or mountainous area and a number of devotees used to visit the holy places in every area for worship. The stability slopes upon which these worship places are located in the hilly and mountainous region are always a major concern. Moreover, heavy precipitation, weathering conditions, seismic disturbances and human activities could cause problem to the stability of such slopes. The effect of slope instability could cause delay in traffic, loss of life of the devotees at pilgrim sites and the loss of the properties. The Saptashrungi gad temple (SGT) situated on basaltic hills belongs to Deccan volcanic and is one among the 51 Shakti Peeths and the most holy place for pilgrims. In this research, the slope stability analysis at SGT hill is assessed using Phase 2, a finite element program along the two parikrama paths: Parikrama Path 1 (or the Badi Parikrama Path “BPP”), and Parikrama Path 2 (or the Chhoti Parikrama Path “CPP”). On the basis of extensive field work, topographic survey, complex geology, orientations of joint sets, hill slope faces and geotechnical conditions, the study area has been divided into eight zones (Zone#01 to Zone#08), and eighteen topographic profiles (AA′ to RR′) are taken from these eight zones for detailed slope stability analysis. The analysis helps to identify the potentially vulnerable slope and zone of instability.
机译:印度的礼拜场所通常位于丘陵地区和/或山区及其周围,许多奉献者用来参观各个地区的圣地进行礼拜。这些礼拜场所位于丘陵和山区的稳定坡度始终是一个主要问题。此外,强降雨,风化条件,地震干扰和人类活动可能对这种斜坡的稳定性造成问题。边坡失稳的影响可能导致交通延误,朝圣者奉献者的生命损失以及财产损失。位于玄武岩山丘上的Saptashrungi gad寺庙(SGT)属于Deccan火山,是51个Shakti Peeths之一,也是朝圣者最圣地。在这项研究中,使用阶段2评估SGT山坡的边坡稳定性分析,这是沿着两个parikrama路径进行的有限元程序:Parikrama路径1(或Badi Parikrama路径“ BPP”)和Parikrama路径2(或Chhoti Parikrama)路径“ CPP”)。根据广泛的现场工作,地形调查,复杂的地质,节理的方向,山坡面和岩土条件,研究区域被划分为八个区域(Zone#01至Zone#08)和18个地形图( AA'至RR')来自这八个区域,用于详细的边坡稳定性分析。该分析有助于确定潜在的脆弱坡度和不稳定区域。

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