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Evaluation of an enhanced FS method for finding the initiation time of earthquake-induced landslides

机译:寻找地震诱发滑坡起始时间的增强FS方法的评估

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摘要

In this paper, an examination of an enhanced FS method used for finding the initiation time of earthquake-induced landslides is presented. Validation was conducted via comparisons between the predicted and reported results of a benchmark site subjected to two major earthquake events: at Chi-Chi in 1999 (7.6 M-w) and Meinong in 2016 (6.4 M-w). To further validate the applicability of the ground motions utilized in this study, a finite element analysis was also carried out. Based on the results, satisfactory agreement between the predictions obtained by the enhanced FS method and the observed results in terms of the landslide initiation time was realized. Conclusions drawn from the study show that (a) the enhanced FS method can be both efficient and practical in finding the likely initiation time of a landslide, and it was found that the initiation time of the Tsaoling landslide during the Chi-Chi earthquake lay between 37.5 and 38.5s; (b) when validating the enhanced FS method, the friction angle of 38.5(o) obtained from direct shear tests rather than a smaller value of 20.8(o) obtained from rotary-shear high-velocity friction experiments, led to a more appropriate results; and (c) the failure surface obtained by finite element codes was satisfactory when compared to the observed result.
机译:本文介绍了一种用于寻找地震诱发滑坡起始时间的增强型FS方法。通过比较遭受两个主要地震事件的基准站点的预测结果和报告结果进行验证:1999年的Chi-Chi(7.6 M-w)和2016年的Meinong(6.4 M-w)。为了进一步验证本研究中使用的地震动的适用性,还进行了有限元分析。根据结果​​,在滑坡起始时间方面,通过改进的FS方法获得的预测与观测结果之间实现了令人满意的一致性。研究得出的结论表明:(a)增强的FS方法在寻找滑坡可能的始发时间上既有效又实用,并且发现在Chi-Chi地震中Tsaoling滑坡的始发时间介于37.5和38.5秒; (b)在验证增强型FS方法时,直接剪切试验获得的摩擦角为38.5(o),而不是旋转剪切高速摩擦试验获得的较小值20.8(o),这导致了更合适的结果; (c)与观察结果相比,通过有限元编码获得的破坏面令人满意。

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