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Macro-Level Assessment of Seismically Induced Landslide Hazard for the State of Sikkim, India Based On GIS Technique

机译:基于GIS技术的地震诱导地震诱导岩石滑坡危害的宏观级评估

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This paper presents a macro-level seismic landslide hazard assessment for the entire state of Sikkim, India, based on the Newmark's methodology. The slope map of Sikkim was derived from ASTER Global Digital Elevation Model (GDEM). Seismic shaking in terms of peak horizontal acceleration (PHA) at bedrock level was estimated from deterministic seismic hazard analysis (DSHA), considering point source model. Peak horizontal acceleration at the surface level for the study area was estimated based on nonlinear site amplification technique, considering B-type NEHRP site class. The PHA at surface was considered to induce driving forces on slopes, thus causing landslides. Knowing the surface level PHA and slope angle, the seismic landslide hazard assessment for each grid point was carried out using Newmark's analysis. The critical static factor of safety required to resist landslide for the PHA (obtained from deterministic analysis) was evaluated and its spatial variation throughout the study area is presented. For any slope in the study area, if the in-situ (available) static factor of safety is greater than the static factor of safety required to resist landslide as predicted in the present study, that slope is considered to be safe.
机译:本文基于纽马克的方法,为印度锡克基姆的整个状态展示了宏观级地震滑坡危害评估。 Sikkim的斜率图来自艾斯特全球数字高度模型(GDEM)。考虑到点源模型,估计基岩水平峰水平加速度(PHA)峰值水平加速度(PHA)的地震振动。考虑到B型NEHRP站点类,估计了研究区域的表面级别的峰值水平加速度。表面的PHA被认为是在斜坡上诱导驱动力,从而导致滑坡。了解表面级PHA和斜坡角度,使用Newmark分析进行每个网格点的地震滑坡危害评估。评估抵抗PHA滑坡所需的临界静态因子(从确定性分析中获得),并介绍了整个研究区域的空间变化。对于研究区域中的任何斜率,如果原位(可用)静态安全性大于当前研究中预测的抵抗滑坡所需的安全性因子,则认为斜坡被认为是安全的。

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