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地震崩塌滑坡危险性应急评估模型效果对比——以2022年6月1日M_W5.8芦山地震为例

COMPARISON OF THE EFFECTS OF EARTHQUAKE-TRIGGERED LANDSLIDE EMERGENCY HAZARD ASSESSMENT MODELS:A CASE STUDY OF THE LUSHAN EARTHQUAKE WITH M_W5.8ON JUNE 1,2022

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【作者】 马思远许冲陈晓利

【Author】 MA Si-yuan;XU Chong;CHEN Xiao-li;Key Laboratory of Seismic and Volcanic Hazards,Institute of Geology,China Earthquake Administration;National Institute of Natural Hazards,Ministry of Emergency Management of China;Key Laboratory of Compound and Chained Natural Hazards Dynamics,Ministry of Emergency Management of China;

【通讯作者】 许冲;

【机构】 中国地震局地质研究所活动构造与火山重点实验室应急管理部国家自然灾害防治研究院复合链生自然灾害动力学应急管理部重点实验室

【摘要】 震后快速准确获取同震崩塌滑坡的分布范围和评估可能的灾害损失对地震灾害应急救援和安置规划至关重要,2022年MW5.8芦山地震为开展不同评价模型在区域地震崩塌滑坡的快速评估研究提供了宝贵窗口。文中选用基于机器学习方法建立的新一代中国地震滑坡危险性模型(下文称Xu2019模型)和简易Newmark模型进行了2022年MW5.8芦山地震崩塌滑坡快速应急评估研究,基于本次事件的地震滑坡数据库(包括2 352处崩塌滑坡,面积为5.51km2),探讨2种模型的准确性和适用性。结果表明,基于Xu2019模型计算得到的崩塌滑坡面积为5.07km2,与实际崩塌滑坡面积十分吻合,而基于Newmark模型计算预测的崩塌滑坡面积达21.3km2。从评估结果的空间分布上来看,2种模型预测的高危险区域基本一致,高危险区域基本位于发震断层的上盘。但Xu2019模型对于西北区域(崩塌滑坡集中发育区)的危险性预测明显偏低,而Newmark模型对西南区域的危险性预测则明显偏高。总体而言,2种模型在区域同震崩塌滑坡分布预测及快速评估方面均具有较好的实用价值,但Newmark模型需要输入多项参数,而这些参数本身及人为获取方式均具有不确定性,导致该模型在实际应用中受人为影响因素较大。

【Abstract】 Earthquake-induced landslides,as an important secondary geological disaster,typically occurring during or shortly after an earthquake,have the characteristics of large quantity and scale,wide distribution,complex mechanism,serious casualties and economic losses,and long-duration post-earthquake effect.Rapidly and accurately obtaining the spatial distribution and potential hazard assessment of coseismic landslide following an earthquake is critical for emergency rescue and resettlement planning.Currently,the most commonly-used coseismic landslide hazard assessment methods include the data-driven machine learning methods and the Newmark method based on mechanics mechanism.The 2022 MW5.8 Lushan earthquake provides a valuable window for us to carry out rapid emergence assessment of earthquake-induced landslides with different evaluation models.In this study,a new generation of China’s earthquake landslide hazard model(hereinafter referred to as Xu2019 model) and a simplified Newmark model are used to carry out the rapid landslide assessment of Lushan event.The Xu2019 model selects 9 earthquake-induced landslide inventories around China as training samples and uses a total of 13 influencing factors such as elevation,relative elevation,slope angle,and aspect,and etc.to generate a near real-time evaluation model for coseismic landslides based on the LR method.The model can rapidly assess coseismic landslides towards a single earthquake event according to the actual PGA distribution.For Newmark model,the cumulative displacement(Dn) is calculated by the critical acceleration(ac) and PGA maps.For the landslide inventory of this earthquake event,we completed the landslide inventory covering the entire affected area based on high-resolution optical satellite images(Planet) with 3m resolution acquired on6 July 2022.Based on the coseismic landslide inventory including 2 352 landslides with an area of5.51km2,the accuracy and applicability of the two models are estimated.The results show that the landslide area calculated based on Xu2019 model is 5.07km2,which is very close to the actual landslide area,and the predicted area calculated based on Newmark model reaches 21.3km2.From the perspective of the spatial distribution of the prediction results,the distribution of the predicted high failure probabilities of the two models is roughly same,with the high probability values mainly located on the left side of the seismogenic fault.However,the difference lies in the low probability predictions of the northwest region of Baoxing county by the Xu2019 model.A zoomed-in view of a specific area comparing the spatial distribution of predicted landslide probabilities with the landslide abundance area shows that most actual landslide are concentrated in the medium to high failure probability areas predicted by the Xu2019 model,with only a few sporadic events occurring in the low probability zone.On the other hand,the Newmark model primarily identifies high instability probability regions in steep slope areas,which correspond closely to the actual landslide and collapse occurrences.However,the predicted hazard level of the northwest region i.e.the landslide highly developed area is obviously low by Xu2019 model,while the prediction result based on Newmark model for the southwest region is obviously overestimated.In terms of the LR model,the prediction results are very close to the actual landslide distribution,and the majority of the landslides are essentially located in areas with a high failure probability,indicating that the model has a relatively high prediction accuracy.The ROC curve is used to assess the model’s accuracy.The results suggest that the model based on Xu2019 outperforms the Newmark model,with a prediction accuracy of 0.77,while the prediction accuracy of the Newmark model is 0.74.Overall,both two models have good practicability in the rapid evaluation of cosesimic landslide.However,the Newmark model needs multi parameter input,and these parameters themselves and the way of human acquisition are uncertain,which results in that the model evaluation is greatly affected by subjectivity.

【基金】 中国地震局地质研究所基本科研业务专项(IGCEA2202,IGCEA1901);国家重点研发计划项目(2017YFC1501001-1,2018YFC1504703-3)共同资助
  • 【文献出处】 地震地质 ,Seismology and Geology , 编辑部邮箱 ,2023年04期
  • 【分类号】P315.9;P642.22
  • 【下载频次】26
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