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孕震过程中次声波的产生机理

A Mechanism Model for Infrasound Emission During Earthquake Incubation

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【作者】 秦飞郑菲李均之夏雅琴陈维升

【Author】 QIN Fei, ZHENG Fei, LI Jun-zhi, XIA Ya-qin, CHEN Wei-sheng (College of Mechanical Engineering and Applied Electronic Technology, Beijing University of Technology, Beijing 100022, China;The Institute of Earthquake Research, Beijing University of Technology, Beijing 100022, China)

【机构】 北京工业大学机械工程与应用电子技术学院北京工业大学地震研究所北京工业大学地震研究所 北京100022北京100022

【摘要】 提出了一个临震次声波产生的机理模型,认为孕震末期地质结构动力行为引起的地表变形与空气耦合运动导致可观测次声波.并以日本地震板块为研究对象,建立其数值模型,采用二维瞬态有限元分析方法,分层考虑不同深度地质参数,模拟了日本东北部地区地表的运动,计算了地表位移及次声波压力变化曲线,模拟出了临震次声波,次声信号波形特征、频率范围与实际观测基本一致,结果表明孕震一次声机理模型是合理的.

【Abstract】 A mechanism model of infrasound producing in earthquake incubating was proposed, in which interaction between atmosphere and deformation of Earth surface generated by dynamic behavior of geologic bodies in the final stage of earthquake incubation causes the observable infrasound. As an example to verify the model of geological behavior an earthquake in the Northeast area of Japan was modeled numerically and analyzed by two dimensional finite element method (FEM). A layer geological model and effect of the Pacific subducting plate were included in the numerical model. Based on the dynamic coupling theory between structures and fluids, infrasound was obtained by numerical simulations. Good agreement between the observed and the simulated suggests that the proposed model is reasonable.

【关键词】 地震次声波有限元消减板块
【Key words】 earthquakesinfrasonic wavesfinite elementsubducting plate
  • 【文献出处】 北京工业大学学报 ,Journal of Beijing University of Technology , 编辑部邮箱 ,2006年06期
  • 【分类号】P315.3
  • 【被引频次】9
  • 【下载频次】292
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