Rapid assessment of the September 5, 2022 ​MS 6.8 Luding earthquake in Sichuan, China

Dengjie Kang , Wenkai Chen , Huaiqun Zhao , Dun Wang
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引用次数: 8

Abstract

At 12:52, September 5, 2022, an MS 6.8 earthquake occurred in Luding, Sichuan. The earthquake caused serious casualties and property loss, and was determined to have an epicenter intensity of IX degree. In this study, we used three earthquake intensity rapid assessment methods (i.e. WFM, BPM and ASM) to evaluate the intensity of this earthquake. Then, we comparatively analyzed the three methods based on strong ground motion observation data and actual intensity maps. The results show that: (1) The earthquake is associated with a southeast-oriented single-sided rupture. The WFM method can only evaluate earthquakes with two-sided ruptures, which has some limitations; (2) The intensity of BPM and ASM was overestimated on the southwest and north sides of the epicenter, but other high-intensity zones were similar to the intensities measured by actual surveys; (3) The residuals of the three intensity assessment methods were all between −0.5 and 1. Although a small number of stations were underestimated, the overall residuals were good, and the residuals gradually approached 0 with the increase of distance; (4) The number of towns and villages evaluated by the three methods in the earthquake area was almost all lower than the field survey results. One exception is the area of VIII degree, where the BPM and ASM were higher than the survey results; (5) The area of the earthquake area evaluated by the three methods was low in VI and VII degree, moderate in VIII degree, and low in IX degree (the area from ASM is similar to the area measured by actual survey). Overall, ASM is applicable to this earthquake intensity assessment.

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2022年9月5日中国四川泸定6.8级地震的快速评估
2022年9月5日12时52分,四川泸定发生里氏6.8级地震。地震造成严重人员伤亡和财产损失,确定震中烈度为九度。在本研究中,我们使用了三种地震烈度快速评估方法(WFM、BPM和ASM)来评估本次地震的烈度。然后,基于强地震动观测数据和实际强度图,对三种方法进行了比较分析。结果表明:(1)本次地震为东南向单侧破裂。WFM方法只能评估具有双侧破裂的地震,这有一定的局限性;(2) 震中西南侧和北侧的BPM和ASM强度被高估,但其他高强度区与实际测量的强度相似;(3) 三种强度评估方法的残差均在−0.5和1之间。尽管低估了少量站点,但总体残差良好,并且随着距离的增加,残差逐渐接近0;(4) 三种方法评估的震区乡镇数量几乎都低于现场调查结果。一个例外是VIII度地区,BPM和ASM高于调查结果;(5) 三种方法评价的震区面积分别为VI度和VII度低、VIII度中等、IX度低(ASM测得的面积与实测面积相似)。总体而言,ASM适用于本次地震烈度评估。
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