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MP I并行的节点大地电磁三维有限元正演

马驹 肖调杰 王赟

物探化探计算技术2016,Vol.38Issue(3):289-296,8.
物探化探计算技术2016,Vol.38Issue(3):289-296,8.DOI:10.3969/j.issn.1001-1749.2016.03.01

MP I并行的节点大地电磁三维有限元正演

Three dimensional modeling of magnetotelluric data using finite element method and MPI parallel computation

马驹 1肖调杰 2王赟1

作者信息

  • 1. 中国科学院 地球化学研究所,贵阳 550002
  • 2. 中国科学院大学,北京 100049
  • 折叠

摘要

Abstract

This paper deals with the forward modeling of three-dimensional (3D)magnetotelluric problem by using the fi-nite element method with fortran language.The validity of this FEM approach is investigated and confirmed by comparing mod-eling results with a layered medium model,a 2D prism model and a 3D model.The bi-conjugate gradient method is applied in solving the governed equations,which reduced the dimensions of the linear system under the first boundary condition.In addi-tion,the memory requirement is reduced obviously in which only nonzero elements stored.The solution of the linear system is obtained by using a massive parallel program based on MPI between frequencies which massively reduced the computing time. A 3D model has been calculated,and the speed-up ratio is up to 2.328 when 4 processes used.

关键词

大地电磁/三维/正演/并行/MPI

Key words

magnetotelluric/three-dimensional/modeling/parallel programing/MPI

分类

天文与地球科学

引用本文复制引用

马驹,肖调杰,王赟..MP I并行的节点大地电磁三维有限元正演[J].物探化探计算技术,2016,38(3):289-296,8.

基金项目

国家科技973项目(2014CB440905) (2014CB440905)

国家重点实验室“十二五”项目群(SKLODG-ZY125-01) (SKLODG-ZY125-01)

物探化探计算技术

OACSCDCSTPCD

1001-1749

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