陕西咸阳市大型滑坡的可自由获取资源及空间分布

Jingyu Chen , Lei Li , Chong Xu , Yuandong Huang , Zhihua Luo , Xiwei Xu , Yuejun Lyu
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引用次数: 1

摘要

在这项研究中,我们使用谷歌地球平台上的高分辨率光学卫星图像绘制了中国陕西省咸阳市大规模山体滑坡的地图。经过测绘,获得了一份全面详细的大型滑坡清单,其中包括2924个大型滑坡。我们分析了滑坡的空间分布,包括高程、坡角、坡向、曲率、岩性、到河流的距离和到断层的距离等七个影响因素。选取滑坡数量、滑坡面积、滑坡数量密度(LND)和滑坡面积百分比(LAP)作为空间分布分析的指标。结果表明,1000–1200海拔范围内的滑坡数量和面积​m是最高的。滑坡数量最多的是25°-30°的斜坡角。朝北的斜坡容易滑动。当边坡曲率在-1.28到0之间时,滑坡的面积和数量最大。当斜率曲率小于-2.56时,LND和LAP达到最大值。具有弱化细粒砂岩和粉砂岩的第三系地层覆盖的区域显示出最高的LND和LAP值。关于到河流的距离,LAP峰值在300–600之间​m、 而LND在大于2100的区域中达到峰值​m.LND和LNP的值随着距断层距离的增加而增加,位置30除外​距离活动断层公里。这种现象是因为该地区的活动断层穿过平原地区,而滑坡大多发生在山区。对咸阳市滑坡发展情况进行分类,为今后滑坡研究提供了重要的科学依据。此外,空间分布结果对滑坡灾害的预防决策具有参考价值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Freely accessible inventory and spatial distribution of large-scale landslides in Xianyang City, Shaanxi Province, China

In this study, we used high-resolution optical satellite images on the Google Earth platform to map large-scale landslides in Xianyang City, Shaanxi Province, China. After mapping, a comprehensive and detailed large-scale landslide inventory that contains 2924 large-scale landslides was obtained. We analyzed the spatial distribution of landslides with seven influencing factors, including elevation, slope angle, aspect, curvature, lithology, distance to a river, and distance to the fault. Landslide Number, Landslide Area, Landslide Number Density (LND), and Landslide Area Percentage (LAP) were selected as indexes for the spatial distribution analysis. The results show that the number and area of landslides in the elevation range of 1000–1200 ​m is the highest. The highest number of landslides was observed in the slope angle of 25°–30°. North-facing slopes are prone to sliding. The area and number of landslides are the largest when the slope curvature ranges from −1.28 to 0. The LND and LAP reach their maxima when the slope curvature is less than −2.56. Areas covered by the Tertiary stratum with weakened fine-grained sandstone and siltstone show the highest LND and LAP values. Regarding distance to a river, the LAP peaks in the range of 300–600 ​m, whereas the LND peaks in an area larger than 2100 ​m. The values of LND and LNP rise as the distance from the faults increases, except for the locations 30 ​km away from active faults. This phenomenon is because active faults in this area pass through the plain areas, while landslides mostly occur in mountainous areas. The cataloging of landslide development in Xianyang City provides a significant scientific foundation for future research on landslides. In addition, the spatial distribution results are useful for landslide hazard prevention decisions and provide valuable references in this area.

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