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首页> 外文期刊>Journal of Earth System Science >Landslide susceptibility analysis using Probabilistic Certainty Factor Approach: A case study on Tevankarai stream watershed, India
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Landslide susceptibility analysis using Probabilistic Certainty Factor Approach: A case study on Tevankarai stream watershed, India

机译:基于概率确定性因子方法的滑坡敏感性分析:以印度特万卡拉河流域为例

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This paper reports the use of a GIS based Probabilistic Certainty Factor method to assess the geo-environmental factors that contribute to landslide susceptibility in Tevankarai Ar sub-watershed, Kodaikkanal. Landslide occurrences are a common phenomenon in the Tevankarai Ar sub-watershed, Kodaikkanal owing to rugged terrain at high altitude, high frequency of intense rainfall and rapidly expanding urban growth. The spatial database of the factors influencing landslides are compiled primarily from topographical maps, aerial photographs and satellite images. They are relief, slope, aspect, curvature, weathering, soil, land use, proximity to road and proximity to drainage. Certainty Factor Approach is used to study the interaction between the factors and the landslide, highlighting the importance of each factor in causing landslide. The results show that slope, aspect, soil and proximity to roads play important role in landslide susceptibility. The landslide susceptibility map is classified into five susceptible classes – low, very low, uncertain, high and very high − 93.32% of the study area falls under the stable category and 6.34% falls under the highly and very highly unstable category. The relative landslide density index (R index) is used to validate the landslide susceptibility map. R index increases with the increase in the susceptibility class. This shows that the factors selected for the study and susceptibility mapping using certainty factor are appropriate for the study area. Highly unstable zones show intense anthropogenic activities like high density settlement areas, and busy roads connecting the hill town and the plains.
机译:本文报告了使用基于GIS的概率确定性因子方法来评估在Kodaikkanal的Tevankarai Ar子流域中导致滑坡敏感性的地质环境因素。由于高海拔地区崎,的地形,频繁的强降雨和城市快速增长,滑坡的发生是科代卡纳尔省Tevankarai Ar子流域的普遍现象。影响滑坡的因素的空间数据库主要从地形图,航拍照片和卫星图像中收集。它们是浮雕,坡度,纵横比,曲率,风化,土壤,土地利用,靠近道路和靠近排水系统。确定性因素法用于研究因素与滑坡之间的相互作用,强调了每个因素在引起滑坡中的重要性。结果表明,坡度,坡向,土壤和靠近道路的路段在滑坡敏感性方面起着重要作用。滑坡敏感性图分为五个敏感类别-低,非常低,不确定,高和非常高-研究区域的93.32%属于稳定类别,而6.34%属于高度和非常高度不稳定类别。相对滑坡密度指数(R指数)用于验证滑坡敏感性图。 R指数随磁化率等级的增加而增加。这表明为研究选择的因子和使用确定性因子的敏感性作图适用于研究区域。高度不稳定的地区表现出强烈的人为活动,例如高密度的定居区以及连接小山镇和平原的繁忙道路。

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