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Assessment of co-seismic landslide hazard using the Newmark model and statistical analyses: a case study of the 2013 Lushan, China, Mw6.6 earthquake

机译:利用纽马克模型和统计分析评估共震滑坡危害 - 以2013年庐山,中国,MW6.6地震为例

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摘要

The April 20, 2013 Mw6.6 earthquake of Lushan County, Sichuan Province, China, has triggered 4540 landslides (>1000m(2)). Exploring a more effective method to assess landslide hazard in the affected area of this event is of great significance for disaster prevention and mitigation. By applying the Newmark model and two statistical analysis models (logic regression and support vector machine, LR and SVM), this study addressed this issue. In the Newmark model, we used the landslide point density, the average gradient (mean slope) and the mean peak ground acceleration to group the lithology and created a critical acceleration (a(c)) map. The Newmark displacements and the probability of the slope instability are mapped by combining the a(c) map and PGA map. In the statistical analysis models of LR and SVM, 7040 samples (4540 landslide sites and 2500 random non-landslide sites) were randomly divided into the training set (5000 samples) and validation set (2040 samples). Based on the relationship between landslide distribution and influence factors, we selected the critical acceleration (a(c)) value, topographic relief, PGA, and distance to rivers as the independent variables for LR and SVM. Finally, the ROC curves for three landslide hazard models were drawn and the AUC values were calculated. The landslide hazard maps produced by LR are similar to those by applying SVM. The AUC values indicate that these two models combined with a(c) data perform better than the simplified Newmark model. In this study, a new method of integrating statistical analysis models (LR and SVM) with critical acceleration (a(c)) for earthquake landslide hazard assessment is presented, which can be used to carry out seismic landslide hazard assessment more effectively than the simplified Newmark model.
机译:2013年4月20日MW6.6中国四川省庐山县地震,已触发4540山滑坡(> 1000米)。探索更有效的方法来评估这一事件的受影响地区的滑坡危害对于防灾和缓解具有重要意义。通过应用纽马克模型和两个统计分析模型(逻辑回归和支持向量机,LR和SVM),这项研究解决了这个问题。在纽马克模型中,我们使用滑坡点密度,平均梯度(均值斜率)和平均峰接地加速度分组岩性,并产生临界加速度(A(C))地图。通过组合A(c)映射和PGA映射来映射纽约标记的位移和斜率不稳定性的概率。在LR和SVM的统计分析模型中,7040个样本(4540个Landslide站点和2500个随机的非滑坡网站)随机分为训练集(5000个样本)和验证集(2040个样本)。基于滑坡分布与影响因素之间的关系,我们选择了临界加速度(A(c))值,地形浮雕,PGA和与河流的距离为LR和SVM的独立变量。最后,绘制了三种滑坡危险模型的ROC曲线,并计算了AUC值。 LR产生的滑坡危险地图与应用SVM类似的危险地图。 AUC值表明这两个模型与(c)数据相结合,比简化的纽马克模型更好。在本研究中,提出了一种将统计分析模型(LR和SVM)与临界加速度(A(c))集成的新方法,用于抗震滑坡危险评估,可用于比简化更有效地进行地震障碍危险评估纽马德模型。

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