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Landslide susceptibility mapping for a landslide-prone area (Findikli, NE of Turkey) by likelihood-frequency ratio and weighted linear combination models

机译:基于似然率比和加权线性组合模型的滑坡易发地区(土耳其东北部芬迪克利)的滑坡敏感性图

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Landslides are very common natural problems in the Black Sea Region of Turkey due to the steep topography, improper use of land cover and adverse climatic conditions for landslides. In the western part of region, many studies have been carried out especially in the last decade for landslide susceptibility mapping using different evaluation methods such as deterministic approach, landslide distribution, qualitative, statistical and distribution-free analyses. The purpose of this study is to produce landslide susceptibility maps of a landslide-prone area (Findikli district, Rize) located at the eastern part of the Black Sea Region of Turkey by likelihood frequency ratio (LRM) model and weighted linear combination (WLC) model and to compare the results obtained. For this purpose, landslide inventory map of the area were prepared for the years of 1983 and 1995 by detailed field surveys and aerial-photography studies. Slope angle, slope aspect, lithology, distance from drainage lines, distance from roads and the land-cover of the study area are considered as the landslide-conditioning parameters. The differences between the susceptibility maps derived by the LRM and the WLC models are relatively minor when broad-based classifications are taken into account. However, the WLC map showed more details but the other map produced by LRM model produced weak results. The reason for this result is considered to be the fact that the majority of pixels in the LRM map have high values than the WLC-derived susceptibility map. In order to validate the two susceptibility maps, both of them were compared with the landslide inventory map. Although the landslides do not exist in the very high susceptibility class of the both maps, 79% of the landslides fall into the high and very high susceptibility zones of the WLC map while this is 49% for the LRM map. This shows that the WLC model exhibited higher performance than the LRM model.
机译:滑坡是土耳其黑海地区非常普遍的自然问题,这是由于地形陡峭,土地覆盖使用不当以及滑坡的不利气候条件所致。在该地区的西部,已经进行了许多研究,尤其是在最近十年中,使用确定性方法,滑坡分布,定性,统计和无分布分析等不同的评估方法对滑坡敏感性图进行了研究。这项研究的目的是通过似然频率比(LRM)模型和加权线性组合(WLC)绘制土耳其黑海地区东部易发生滑坡的地区(芬迪克利区,里兹)的滑坡敏感性图。模型并比较获得的结果。为此,通过详细的实地调查和航空摄影研究,编制了该地区1983年和1995年的滑坡清单图。坡度,坡度,岩性,距排水线的距离,距道路的距离和研究区域的土地覆盖被认为是滑坡调节参数。当考虑广泛的分类时,由LRM模型和WLC模型得出的磁化率图之间的差异相对较小。但是,WLC图显示了更多细节,但LRM模型生成的其他图却产生了较弱的结果。认为该结果的原因是这样的事实,即LRM图中的大多数像素具有比WLC衍生的磁化率图更高的值。为了验证两个磁化率图,将它们都与滑坡清单图进行了比较。尽管在两个地图的极高磁化率类别中均不存在滑坡,但79%的滑坡属于WLC图的高磁化率和极高磁化率区域,而对于LRM地图,则为49%。这表明WLC模型表现出比LRM模型更高的性能。

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