袁杰^1,2,,
崔泽飞¹,
朱守彪^1,,,
王进廷²
1. 应急管理部国家自然灾害防治研究院, 北京 100085
2. 清华大学水利水电工程系, 北京 100084

基金项目: 中国地震局地壳应力研究所基本科研业务专项（ZDJ2020-08）及国家自然科学基金项目（41874060，51725901，51639006）共同资助


详细信息

作者简介: 袁杰, 男, 助理研究员, 理学博士.现主要从事震源动力学、工程抗震地震动输入研究.E-mail:yuenjay@sina.cn

通讯作者: 朱守彪, 男, 研究员, 理学博士, 博士生导师.现主要从事地球动力学、地震活动性及地震预报方法研究.E-mail:zhusb@pku.edu.cn; zhushoubiao@gmail.com

中图分类号: P315;P313

收稿日期:2020-06-17
修回日期:2020-09-09
上线日期:2021-02-10

Finite element method simulation of the earthquake preparation, occurrence, and recurrence cycles

YUAN Jie^1,2,,
CUI ZeFei¹,
ZHU ShouBiao^1,,,
WANG JinTing²
1. National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, China
2. Department of Hydraulic Engineering, Tsinghua University, Beijing 100084, China


More Information

Corresponding author: ZHU ShouBiao,E-mail:zhusb@pku.edu.cn; zhushoubiao@gmail.com

MSC: P315;P313

--> Received Date: 17 June 2020
Revised Date: 09 September 2020
Available Online: 10 February 2021


摘要
摘要:强震孕育发生及其复发过程的定量研究对于预测预报地震有着重要的科学意义；合理连续地计算地震孕育、同震破裂过程及其复发循环特征将有助于我们更好地认识强震发生的时空分布规律.为此，本文基于Newmark隐式时间积分法，根据模拟孕震-同震循环过程的特殊要求，发展了一种新的有限单元计算方法.新方法具有以下特点：（1）在不改变时间积分方法的情况下，实现对时间步长进行自动平滑地缩放，进而可以连续的模拟准静态、动态不同力学状态下的孕震-同震循环过程；（2）模型的初始应力场非人为指定，计算时通过施加重力及缓慢的构造加载获得；（3）地震破裂的成核区域及成核方式等亦非人为给定，模拟中破裂成核是自然形成的，这样更加符合实际地震地质情况.通过大量的模型计算，其结果表明，新的计算方法可以连续稳定的模拟断层孕震-同震及其循环过程，计算结果不仅可以给出强震的复发间隔，同时还可以给出地震时断层破裂行为的详细过程.此外，本文还考察了摩擦系数对地震准周期性的影响，发现断层上的静、动摩擦系数差值直接影响着断层的强震复发周期，两者差值越小，复发周期越短；差值越大，复发间隔越长.
关键词: 强震孕育/
同震破裂/
强震复发周期/
连续模拟/
有限单元法

Abstract:The study of the quasi-periodic recurrence behavior of strong earthquakes is important for predicting and mitigating earthquake disasters. Reasonably and continuously simulating the interseismic-coseismic cycle process is the key to researching the spontaneous earthquake sequences. Based on the finite element dynamic implicit algorithm, this work develops a new methodology for simulating the interseismic-coseismic cycle processes. Our approach has the following advantages:(1) Continuously simulate the interseismic-coseismic cycle process without switching algorithms, and the time step size is automatically and smoothly scaled between quasi-static and dynamic states. (2) The stress field of the calculation model can be obtained under slow tectonic loading and gravity without artificially assigned. (3) The nucleation process of each earthquake event is formed slowly and naturally, and does not need to be given artificially. The simulation results show that the new methodology can continuously and steadily simulate the fault interseismic-coseismic cycle behavior, recurrence interval of strong earthquake, and the detailed coseismic rupture process. In addition, we study the influence of friction coefficient on the recurrence interval of strong earthquake. It turns out that the difference between the static and dynamic friction coefficients on the fault directly affect the recurrence interval of strong earthquake. The smaller the difference, the shorter the recurrence period is.
Key words:Pregnant process of strong earthquake/
Coseismic rupture/
Seismic cycle/
Continuous simulation/
Finite element method



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