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Landslide susceptibility assessment in Wenchuan County after the 5.12 magnitude earthquake

机译:汶川县滑坡敏感性评估5.12大地震

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Wenchuan was designated as one of the earthquake-stricken areas after the 2008 5.12-magnitude Wenchuan earthquake. During the decade following the earthquake, many post-earthquake landslides have occurred, seriously threatening the property of the local population's lives and property. At present, there are few long-term spatiotemporal changes studies on landslides generated after the earthquake. The main aim of the present study is to use Landsat multi-period remote sensing image data, combined with post-earthquake landslide interpretation point data, to extract landslide point information from 2011, 2014, and 2018 to analyze the spatial evolution of landslides and define reliable susceptibility models for landslides in 2018 using an assessed certainty factor (CF), an integrated CF with random forest (RF), and an integrated CF with logistic regression (LR). The area under cure (AUC) was used to test the accuracy of the three models and obtain the most reflective susceptibility map. The results show that the RF-CF model produced the optimal result in terms of its AUC value (0.84). Over the past decade, the high-density area has become more concentrated than that of other grades and its coverage small, and its proportion has gradually decreased; the proportion of landslides in low-density areas has been increasing, and its distribution has become more concentrated. These research results fill the gap in the study of temporal and spatial changes in landslides after an earthquake and provide a scientific basis for disaster management and prediction in landslide-prone areas such as Wenchuan.
机译:汶川被指定为2008年5月5日汶川地震后的地震灾区之一。在地震之后的十年中,发生了许多地震后山体滑坡,严重威胁着当地人口的生命和财产的财产。目前,在地震发生后产生的山体滑坡有很少的长期瞬发改变研究。本研究的主要目的是使用Landsat多时期遥感图像数据,结合地震后滑坡解释点数据,从2011年,2014年和2018年提取滑坡点信息,分析山体滑坡的空间演变和定义2018年使用评估的确定性因子(CF),具有随机森林(RF)的集成CF和具有逻辑回归(LR)的集成CF的可靠易感性模型。固化区域(AUC)用于测试三种模型的准确性,并获得最具反射敏感性图。结果表明,RF-CF模型在其AUC值(0.84)方面产生了最佳结果。在过去十年中,高密度区域变得比其他成绩更集中,其覆盖率小,其比例逐渐减少;低密度区域的山体滑坡比例越来越多,其分布变得更加集中。这些研究结果填补了地震后山体滑坡时间和空间变化研究的差距,为汶川等山坡易发地区提供了科学依据灾害管理和预测。

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