通过地理空间工具和统计方法绘制埃塞俄比亚西北部德布雷塔博-安贝尔公路沿线的滑坡易发性地图

Q3 Social Sciences
Betelhem Tesfaye, Muralitharan Jothimani, Zerihun Dawit
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引用次数: 0

摘要

本研究旨在确定埃塞俄比亚北部 Debretabor-Alember 路段沿线易发生山体滑坡的地区。利用地理空间工具,特别是频率比 (FR) 和信息值 (IV),绘制了滑坡易发区地图 (LSM)。对谷歌地球图像进行了全面的现场调查和分析,探测并分析了 89 次滑坡,包括当前和历史事件。用于验证的数据集包括 78% 以前记录的滑坡,其余 22% 用于训练。本研究在确定滑坡易发性时考虑了多个因素,包括 "坡度、坡向、曲率、海拔、岩性、与溪流的距离、土地利用和覆盖、降水、归一化差异植被指数(NDVI)"以及 FR 和 IV 模型。根据 FR 方法得出的结果,特定区域表现出不同程度的易感性,从极低到中等偏高、中等、高和极高不等。这些地区的总面积分别为 18.4 平方公里(19.9%)、18.9 平方公里(20.5%)、19.7 平方公里(20.3%)、17.7 平方公里(20%)和 17.7 平方公里(19%)。IV 模型生成的 LSM 显示了研究区域的多个易感等级,从极低到极高不等。这些地图显示,18.4 平方公里 (19.8%)、18.8 平方公里 (20%)、18.9 平方公里 (19.5%)、18.8 平方公里 (20.5%) 和 18.3 平方公里 (19.8%) 的区域属于这些易感等级。采用滑坡密度指标法来验证 LSM。FR 模型和 IV 模型表明,在已确认的过去和当前滑坡记录中,有很大一部分(分别为 72.16% 和 73.86%)发生在滑坡易发性较高或极高的地区。总体而言,在自变量模型中采用潜变量结构模型(LSM)的 IV 模型优于固定效应回归模型(FR)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mapping landslide susceptibility in the Debretabor-Alember road sector, Northwestern Ethiopia through geospatial tools and statistical approaches
This study aimed to locate areas along the Debretabor-Alember route segment in northern Ethiopia that are susceptible to landslides. Geospatial tools, specifically frequency ratios (FR) and information values (IV), were used to develop landslide susceptibility maps (LSMs). A comprehensive on-site investigation and analysis of Google Earth imagery were conducted, resulting in the detection and analysis of 89 landslides, including current and historical events. The dataset used for validation comprised 78% of the previously documented landslides, whereas the remaining 22% was used for training. Several factors were considered in this study to determine landslide susceptibility, including "slope, aspect, curvature, elevation, lithology, distance from streams, land use and cover, precipitation, normalized difference vegetation index (NDVI)", and the FR and IV models. Based on the results obtained using the FR approach, specific areas exhibited different levels of susceptibility, ranging from very low to moderately high, medium, high, and very high. These areas covered a total of 18.4 km2 (19.9%), 18.9 km2 (20.5%), 19.7 km2 (20.3%), 17.7 km2 (20%), and 17.7 km2 (19%), respectively. The LSMs generated by the IV model indicated multiple susceptibility classes in the study area, varying from very low to very high. These maps revealed that 18.4 km2 (19.8%), 18.8 km2 (20%), 18.9 km2 (19.5%), 18.8 km2 (20.5%), and 18.3 km2 (19.8%) of the area fell into these susceptibility classes. The landslide density indicator method was employed to validate the LSMs. The FR and IV models demonstrated that a significant proportion of confirmed past and current landslide records (72.16% and 73.86%, respectively) occurred in regions with a high or very high susceptibility to landslides. Overall, the IV model, which utilized latent variable structural modeling (LSM) in the independent variable model, outperformed the fixed effects regression model (FR).
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来源期刊
Journal of Degraded and Mining Lands Management
Journal of Degraded and Mining Lands Management Environmental Science-Nature and Landscape Conservation
CiteScore
1.50
自引率
0.00%
发文量
81
审稿时长
4 weeks
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