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Application of the relief degree of land surface in landslide disasters susceptibility assessment in China

机译:地表起伏度在我国滑坡灾害敏感性评价中的应用

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Chinese mountainous area takes 2/3 of its total land area, making it one of the countries most seriously effected by landslide disasters, and the impact of landslide on people's lives and property becomes increasingly serious. Considering the grim situation of landslide disasters and the resulting huge losses, it is a very important work to assess the susceptibility of the landslide disasters under national scale in order to provide the scientific basis for landslide disasters prevention. In many factors affecting the appearance of landslide disasters, such as lithology, geological structure, earthquake zone distribution, etc, the geomorphologic form is one of the main factors to control the spatial distribution of landslide disasters in China, also plays an important role as the main factor in the assessment of the landslide susceptibility. The relief degree of land surface is an important reference factor of geomorphologic form classification used to describe and reflect the macroscopic characteristics of topography of the surface in a large area. This paper extracts the relief degree of land surface of China based on the SRTM DEM covering the whole country. Based on the extraction, classify the national geomorphologic form into slow undulation, the low undulation, the moderate undulation, mountainous undulation and alpine undulation based on the classification to the relief degree of land surface with the range of 0~25m,25~75m,75~200m,200~600m and >600m. It analyses the spatial correlation between different landscape patterns and the spatial distribution of the landslide disasters using the information content model. The results show that there is a very good correlation between the relief degree of land surface and the landslide susceptibility, with the increase of the value of relief degree of land surface, its information content gradually increases.
机译:中国山区占总土地面积的2/3,是滑坡灾害影响最严重的国家之一,滑坡对人们的生命和财产的影响日益严重。考虑到滑坡灾害的严峻形势及其造成的巨大损失,评估全国范围内滑坡灾害的敏感性是一项十分重要的工作,为预防滑坡灾害提供科学依据。在影响滑坡灾害发生的许多因素中,如岩性,地质结构,地震带分布等,地貌形态是控制我国滑坡灾害空间分布的主要因素之一,在控制滑坡灾害空间分布方面也起着重要作用。评估滑坡敏感性的主要因素。地表起伏程度是地貌形态分类的重要参考因素,用来描述和反映大面积地表的宏观特征。本文基于覆盖全国的SRTM DEM,提取了中国陆地表面的起伏程度。在提取的基础上,根据地表起伏程度的分类,将国家地貌形态分为慢起伏,低起伏,中起伏,山区起伏和高山起伏,范围为0〜25m,25〜75m, 75〜200m,200〜600m和> 600m。利用信息内容模型分析了不同景观格局与滑坡灾害空间分布的空间相关性。结果表明,地表起伏度与滑坡易感性之间具有很好的相关性,随着地表起伏度值的增加,其信息量逐渐增加。

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