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Mapping Landslide Hazards in Western Nepal: Comparing Qualitative and Quantitative Approaches

机译:绘制尼泊尔西部滑坡灾害的地图:定性和定量方法的比较

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摘要

Each year dozens of people are killed in Nepal as a result of landslides. To promote safe human occupation of this dynamic landscape, a priori understanding of the geologic circumstances of landslides, and knowledge of the characteristics and locations of landslides are essential. Furthermore, a method of constructing maps of natural hazards is necessary that is simple, efficient, and, above all, accurate. This paper assesses two different methods to identify landslides in western Nepal and demonstrates the capabilities of each technique. Eighty-eight landslides were mapped in the Andhi Khola River watershed in western Nepal. Instability in this area is influenced by joint patterns, rock weathering, shallow soils, and geomorphic, geodynamic, and groundwater conditions. The major triggers of landslides are excessive rainfalls, road cuts, and undercutting of slope toes by rivers. Two approaches, a qualitative approach and a statistical or quantitative approach, have been developed to identify landslide hazards. The qualitative map of hazards classified 23 percent of the area as high hazard, 22 percent as medium hazard, and 55 percent as low hazard. The statistical map of hazards classified 10 percent of the area as high hazard, 70 percent as medium hazard, and 20 percent as low hazard. The prediction accuracy of the statistical hazard map is better than that of the qualitative hazard map.
机译:每年,由于 滑坡,尼泊尔有数十人丧生。为了促进人类对这一动态 景观的安全占领,对滑坡的地质情况 有先验的了解,并了解滑坡的特征和位置 是必不可少的此外,有必要构建一种简单,有效, 且最重要的是准确的自然灾害图 。本文评估了两种不同的 方法来识别尼泊尔西部的滑坡,并证明了 每种技术的功能。在尼泊尔西部的安迪·霍拉河流域绘制了88个滑坡 该地区的不稳定性受联合模式,岩石 风化,浅层土壤,地貌,地球动力学和地下水 条件。滑坡的主要诱因是降雨过多, 道路开挖以及河流对坡脚趾的侵蚀。已经开发了两种方法, 定性方法和统计或定量方法, 来识别滑坡灾害。定性的 危害图将23%的区域划分为高危害区域, 的22%划分为中度危害区域,将55%的区域划分为低危害区域。危害的 统计图将区域 的10%划分为高危害,将70%划分为中等危害,将20%的 划分为低危害。统计危害图 的预测精度优于定性危害图。

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  • 来源
    《Environmental and Engineering Geoscience》 |2010年第2期|127-142|共16页
  • 作者单位

    High Alpine and Arctic Research Program (HAARP), Department of Geology and Geophysics, Texas A&M UniversityCollege Station, TX 77843;

    High Alpine and Arctic Research Program (HAARP), Department of Geology and Geophysics, Texas A&M UniversityCollege Station, TX 77843;

    High Alpine and Arctic Research Program (HAARP), Department of Geology and Geophysics, Texas A&M UniversityCollege Station, TX 77843;

    Department of Geology, Tri-Chandra Campus, Tribhuvan UniversityKatmandu Nepal;

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