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Landslide susceptibility mapping using Bayesian approach in the Sultan Mountains (Akşehir, Turkey)

机译:在苏丹山脉(土耳其阿克希尔)使用贝叶斯方法绘制滑坡敏感性图

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摘要

Landslides cause heavy damage to property and infrastructure, in addition to being responsible for the loss of human lives in many parts of the Turkey. The paper presents GIS-based spatial data analysis for landslide susceptibility mapping in the regions of the Sultan Mountains, West of Akşehir, and central part of Turkey. Landslides occur frequently in the area and seriously affect local living conditions. Therefore, spatial analysis of landslide susceptibility in the Sultan Mountains is important. The relationships between landslide distributions with the 19 landslide affecting parameters were analysed using a Bayesian model. In the study area, 90 landslides were observed. The landslides were randomly subdivided into 80 training landslides and 10 test landslides. A landslide susceptibility map was produced by using the training landslides. The test landslides were used in the accuracy control of the produced landslide susceptibility map. Approximately 9% of the study area was classified as high susceptibility zone. Medium, low and very low susceptibility zones covered 8, 23 and 60% of the study area, respectively. Most of the locations of the observed landslides actually fall into moderate (17.78%) and high (77.78. %) susceptibility zones of the produced landslide susceptibility map. This validates the applicability of proposed methods, approaches and the classification scheme. The high susceptibility zone is along both sides of the Akşehir Fault and at the north-eastern slope of the Sultan Mountains. It was determined that the surface area of the Harlak and Deresenek formations, which have attained lithological characteristics of clayey limestone with a broken and separated base, and where area landslides occur, possesses an elevation of 1,100–1,600 m, a slope gradient of 25°–35° and a slope aspect of 22.5°–157.5° facing slopes.
机译:滑坡不仅造成了土耳其许多地区的人员伤亡,还严重损害了财产和基础设施。本文介绍了基于GIS的空间数据分析,用于苏丹山,阿克谢希尔以西和土耳其中部地区的滑坡敏感性地图绘制。该地区经常发生山体滑坡,严重影响当地的生活条件。因此,苏丹山滑坡敏感性的空间分析很重要。使用贝叶斯模型分析了滑坡分布与19个滑坡影响参数之间的关系。在研究区域,观察到90个滑坡。滑坡被随机分为80个训练滑坡和10个测试滑坡。使用训练滑坡绘制了滑坡敏感性图。测试滑坡用于控制所生成滑坡敏感性图的准确性。大约9%的研究区域被归类为高敏感区。中,低和极低的磁化率区分别覆盖了研究区域的8、23和60%。实际上,所观察到的滑坡的大多数位置实际上都位于生成的滑坡敏感性图的中等(17.78%)和高(77.78。%)敏感性区。这验证了所提出的方法,方法和分类方案的适用性。高磁化率带位于阿克谢希尔断裂的两侧和苏丹山脉的东北坡。经确定,哈拉克和德雷塞内克地层的表面积达到了1,100–1,600 m,坡度为25°,海拔高度为1,100–1,600 m,已达到具有碎裂和分离基底的粘土质石灰岩的岩性特征。 –35°,面向斜坡的坡度为22.5°–157.5°。

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  • 来源
    《Natural Hazards》 |2011年第3期|p.1573-1607|共35页
  • 作者

    Adnan Ozdemir;

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  • 正文语种 eng
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