2024 MW 7.4花莲地震诱发同震滑坡和液化的高分辨率卫星图像分析

Lingyun Lu , Yueren Xu , Jiacheng Tang , Guiming Hu
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引用次数: 0

摘要

快速获取强震次生灾害空间分布图,对于了解地震灾害链中的致灾过程,制定有效的应急措施和灾后重建计划至关重要。2024年4月3日,中国台湾花莲以东海域发生里氏7.4级地震,引发基岩山区多处同震滑坡,沿海地区土壤严重液化,造成重大经济损失。本研究利用中国高分辨率光学卫星影像的震后应急数据,采用目视解译方法,建立了花莲地震次生灾害部分数据库。共发现5 348个同震滑坡,主要分布在中央山脉流域东坡。在高山峡谷,这些滑坡主要表现为局部基岩崩塌或边坡泥石流,对高速公路和旅游设施造成广泛破坏。其分布与1999年池池地震引发的滑坡集中区有部分重叠。土壤液化事件共6 040次,主要分布在花莲港区和花莲河低洼河谷地区,且集中在6级烈度区。广泛的地表沉降和喷砂是土壤液化的特征。通过对台湾当地实地调查数据的验证,通过震后遥感数据快速成像可以有效地评估高烈度区内同震滑坡和土壤液化的分布。本研究为地震灾害响应提供了有效可靠的数据。此外,研究结果对高山峡谷和沿海低地的地震减灾具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
High-resolution satellite imagery analysis of coseismic landslides and liquefaction induced by the 2024 MW 7.4 Hualien earthquake, Taiwan, China
Rapidly obtaining spatial distribution maps of secondary disasters triggered by strong earthquakes is crucial for understanding the disaster-causing processes in the earthquake hazard chain and formulating effective emergency response measures and post-disaster reconstruction plans. On April 3, 2024, a MW 7.4 earthquake struck offshore east of Hualien, Taiwan, China, which triggered numerous coseismic landslides in bedrock mountain regions and severe soil liquefaction in coastal areas, resulting in significant economic losses. This study utilized post-earthquake emergency data from China's high-resolution optical satellite imagery and applied visual interpretation method to establish a partial database of secondary disasters triggered by the 2024 Hualien earthquake. A total of 5 348 coseismic landslides were identified, which were primarily distributed along the eastern slopes of the Central Mountain Range watersheds. In high mountain valleys, these landslides mainly manifest as localized bedrock collapses or slope debris flows, causing extensive damage to highways and tourism facilities. Their distribution partially overlaps with the landslide concentration zones triggered by the 1999 Chi-Chi earthquake. Additionally, 6 040 soil liquefaction events were interpreted, predominantly in the Hualien Port area and the lowland valleys of the Hualien River and concentrated within the IX-intensity zone. Widespread surface subsidence and sand ejections characterized soil liquefaction. Verified against local field investigation data in Taiwan, rapid imaging through post-earthquake remote sensing data can effectively assess the distribution of coseismic landslides and soil liquefaction within high-intensity zones. This study provides efficient and reliable data for earthquake disaster response. Moreover, the results are critical for seismic disaster mitigation in high mountain valleys and coastal lowlands.
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