4.6 Article

Landslide Risk Mapping Using the Weight-of-Evidence Method in the Datong Mining Area, Qinghai Province

期刊

SUSTAINABILITY
卷 15, 期 14, 页码 -

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MDPI
DOI: 10.3390/su151411330

关键词

mining environment; landslides; hazard mapping; risk mapping; weight of evidence

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This study uses field survey and remote sensing data to comprehensively evaluate landslide susceptibility in the Datong mining area of Qinghai Province. Factors such as topography, lithological structure, mining engineering activities, land use, and dynamic deformation are considered, and the hazard and risk of landslides are quantitatively assessed using the Topographic Wetness Index (TWI) and the Human Engineering Activity Intensity (HEAI). The weight-of-evidence approach is used for mapping landslide hazard and risk. The results show that there are large areas of extremely high-hazard and high-risk areas induced by human engineering activities.
Qinghai is rich in mineral resources, but frequent and large-scale mineral mining has caused secondary damage to the fragile primary surface and produced a large number of landslide disasters. In complex geological environments such as glacier ablation and frequent tectonic movements, a complete quantitative evaluation method for landslide risk in high-cold mining areas has not yet been formed. In view of this, this article uses the field survey and remote sensing data of the Datong mining area in Qinghai Province in 2012 as the basic data. We comprehensively considered five first-level factors (13 s-level factors) including topography, lithological structure, mining engineering activities, land use, and dynamic deformation as evaluation indicators for landslide susceptibility in mining areas, and used the Topographic Wetness Index (TWI) and the Human Engineering Activity Intensity (HEAI) to quantitatively estimate the hazard of landslide according to the landslide trigger mechanism. The weight-of-evidence approach was used for landslide hazard and risk mapping under different landslide--inducing conditions. The results indicate that the extremely high-hazard areas induced by human engineering activities account for 14% of the total area, and the extremely high-risk areas account for 13% of the total area in the Datong mining area, and the area of the extremely high-risk area is large; the landslide risk assessment mapping model constructed in this study can effectively evaluate the probability of slope instability caused by rainfall and human engineering activities. The effective value of the receiver operating characteristic (ROC) curve of the sensitivity assessment model reaches 0.863, and the evaluation results are consistent with reality; using the weight-of-evidence model for landslide risk assessment is more in line with the actual situation in alpine mining areas, and is more suitable for guiding landslide risk management and disaster prevention and mitigation in mining areas.

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