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求解弹性波方程的辛RKN格式
  • ISSN号:0001-5733
  • 期刊名称:地球物理学报
  • 时间:2015.4.15
  • 页码:1355-1366
  • 分类:P315[天文地球—地震学;天文地球—固体地球物理学;天文地球—地球物理学]
  • 作者机构:[1]中国科学院地质与地球物理研究所,中国科学院地球与行星物理重点实验室,北京100029, [2]中国科学院大学,北京100049, [3]华北水利水电大学资源与环境学院,郑州450045, [4]宁夏大学数学计算机学院,银川750021
  • 相关基金:国家自然科学基金项目(41174047,40874024,41204041)资助
  • 相关项目:全球尺度地震波传播的保结构算法研究
中文摘要:

大地震等诸多激励均能激发全球自由振荡现象,通常表现为驻波形式的全球整体振荡.现有的地震波数值模拟方法多为非保结构方法,无法压制长时程计算中的积累误差.本文采用优化的三阶辛格式谱元法,对地球自由振荡及全球尺度的地震波传播进行了长时程模拟.通过与传统的基于Newmark算法的谱元方法结果对比分析,明确验证了本文所得优化的三阶辛格式谱元法在模拟地球自由振荡等大规模长时程问题上的优越性和准确性.上述进展在方法论层面为今后探测、刻画全球尺度地球非均匀结构的驻波数值方法奠定了部分基础,并为相关研究领域提供了新的选择.

英文摘要:

Free oscillations of the Earth are usually as standing waves of entire globe,which can be excited by many factors such as a great earthquake.The oscillation types of this physical phenomenon depend on Earth′s structure and physical parameters.Therefore,intrinsic characters of the Earth can be revealed by studying Earth′free oscillations.Numerical simulation is an effective way to research seismic waves travelling in different earth models.In essence,the numerical simulation of Earth′s free oscillations is a long-term tracing of variable coefficient wave equation.The majority of numerical methods for seismic wave simulation are non-structurepreserving methods,which cannot suppress the accumulative error in long-time computation,e.g.,finite difference methods,pseudo-spectral methods,and finite element methods.In comparison,the symplectical methods based on the Hamilton system possess fine structure-preserving ability which makes them be suitable for the physical problem acquiring good precision in long-time simulation.The spectral element method combines the generality of the finite element method with the accuracy of spectral techniques.This method expands the solution in trigonometric series,of which a chief advantage is that the resulting method is of very high order.It also chooses high-degree piecewise polynomial basis functions,also achieving a very high order of accuracy.Symplectical methods introduced into spectral element methods may be an accurate and effective choice.In this research,a three-order symplectical spectral element method is modified for long-time simulation of Earth′s free oscillations and seismic waves propagating in the global range.The event simulated is a great earthquake(Mw8.6)off the west coast of northern Sumatra on 11 April 2012.The PREM earth model is used for simulation.Our method and traditional spectrum element method using Newmark time scheme are chosen for simulation respectively with the same parameters and computation scales.The time step adopted by our method is

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期刊信息
  • 《地球物理学报》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院
  • 主办单位:中国地球物理学会 中国科学院地质与地球物理研究所
  • 主编:刘光鼎
  • 地址:北京9825信箱
  • 邮编:100029
  • 邮箱:actageop@mail.igcas.ac.cn
  • 电话:010-82998105
  • 国际标准刊号:ISSN:0001-5733
  • 国内统一刊号:ISSN:11-2074/P
  • 邮发代号:2-571
  • 获奖情况:
  • 首届国家期刊奖,第二届国家期刊奖,中国期刊方阵“双高”期刊,第三届中国出版政府奖
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  • 被引量:31618