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基于经验模态分解的泸定6.8级地震地下水流量异常识别

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基于 2022 年 9 月 5 日 12 时 52 分泸定 6.8 级地震,通过经验模态分解(EMD)方法对西昌、昭觉和盐源台站流量观测数据进行分析处理,发现 3 个台站异常出现时间集中在震前 4~5 天左右的短临阶段,异常变化形态均表现为"上升-下降-上升"类型,且西昌、昭觉和盐源台站的流量异常频段分别为 3.5×10-7~3.8×10-6 Hz、3.5×10-7~3.5×10-6 Hz和 3.8×10-7~3.4×10-6 Hz.结果表明,EMD方法有效提高了地震前流量异常信息的获取能力,在地下水流量异常特征识别与信号分析方面具有较好的应用前景.
Groundwater Flow Anomalies Related to the Luding M6.8 Earthquake Identified by the Empirical Mode Decomposition
Groundwater flow is one of the seismic observation items sensitive to seismic reflection.Based on the Luding M6.8 earthquake at 12:52 am on September 5,2022,this paper analyzes and processes the flow data of Xichang,Zhaojue and Yanyuan stations by empirical mode decomposition(EMD)method.It is found that the occurrence time of anomalies at the three stations is concentrated in the short imminent stage about 4 to 5 days before the earthquake,and the abnormal variation forms are of the"up-down-up"type.The abnormal flow frequency bands of Xichang,Zhaojue and Yanyuan stations are 3.5×10-7 Hz~3.8×10-6 Hz,3.5×10-7 Hz~3.5×10-6 Hz and 3.8×10-7 Hz~3.4×10-6 Hz.The results show that the EMD method can effectively improve the capability to obtain the abnormal flow information before the earthquake,so it has a good application prospect in the field of groundwater flow anomaly feature identification and signal analysis.

the Luding M6.8 earthquakegroundwater flowEMDabnormal recognition

尤宝鑫、刘爱春、刘冠中、范良龙、方创首

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中国科学院大学应急管理科学与工程学院,北京 100049

应急管理部国家自然灾害防治研究院,北京 100085

复合链生自然灾害动力学应急管理部重点实验室,北京 100085

北京一联科技有限公司,北京 102400

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泸定6.8级地震 地下水流量 经验模态分解 异常识别

国家重点研发计划中央级公益性科研院所基本科研业务费专项重点项目

2022YFC3070103-1ZDJ2018-23

2024

华北地震科学
河北省地震局

华北地震科学

CSTPCD
影响因子:0.598
ISSN:1003-1375
年,卷(期):2024.42(2)
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