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地震 ›› 2008, Vol. 28 ›› Issue (4): 1-12.

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自转速率快速变化引起的全球位移场和应力场

陈绍林1, 张怀1, 朱桂芝1,2, 石耀霖1   

  1. 1.中国科学院研究生院计算地球动力学重点实验室, 北京 100049;
    2.中国地震局第二监测中心, 陕西 西安 710054
  • 收稿日期:2008-06-03 修回日期:2008-06-23 出版日期:2008-10-31 发布日期:2021-10-29
  • 作者简介:陈绍林(1982-), 男, 安徽泗县人,2005级在读硕士研究生,主要从事并行计算、可视化等研究。
  • 基金资助:
    国家科学自然基金(40774049, 40474038)和中国科学院知识创新工程重要方向项目(kzcx2-yw-123)联合资助

Global Displacement and Stress Fields Induced by Fast Change of Earth's Angular Velocity

CHEN Shao-lin1, ZHANG Huai1, ZHU Gui-zhi2, SHI Yao-lin1   

  1. 1. Laboratory of Computational Geodynamics, Graduate University of the Chinese Academy of Sciences, Beijing 100049;
    2. No.2 Monitoring Center of China Earthquake Administration, Xi'an 710054, China
  • Received:2008-06-03 Revised:2008-06-23 Online:2008-10-31 Published:2021-10-29

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141

摘要： 该文建立了百万网格的分层PREM地球模型, 利用并行有限元方法计算了自转速率快速变化所引起的全球附加的位移场和应力场。 计算模型中不仅考虑了地球的径向分层, 同时还考虑椭率和地形的影响。 利用数值试验的方法, 系统分析了地球自转速率变化为Δω/ω=2×10-10时所引起的全球应力分布特征, 研究表明椭率对地表各个应力分量的影响在千分之几, 而地形的影响则表现为径向应力与地形正相关, 且相同高度的地形在低纬度影响较大, 纬向和经向的应力大小分别与地形在SN向和EW向的地形梯度直接相关。

关键词: 地球自转, 横向不均匀性, 全球网格模型, 并行有限元计算

Abstract: This paper constructed a layered earth model based on PREM, with more than one million meshes. The displacement and stress fields induced by the fast change of earth's angular velocity were also computed using parallel finite element method. In this model, the lateral heterogeneity was taken into consideration, and the topography data and ellipticity of the earth were also integrated in this model to simulate a more realistic earth. The characteristics of the displacement and stress distribution were systematically analyzed, with the assumption that the fast angular velocity change is Δω/ω=2×10-10 per year.

Key words: Earth's self-rotation, Lateral heterogeneity, PREM model, Parallel finite element computing

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