吉林大学学报(地球科学版)

• 地球探测与信息技术 • 上一篇    下一篇

电导率连续变化的线源FCSEM有限元正演模拟

汤文武1,2,柳建新1,2,童孝忠1,2   

  1. 1.中南大学地球科学与信息物理学院, 长沙410083;
    2.有色资源与地质灾害探查湖南省重点实验室,长沙410083
  • 收稿日期:2012-12-05 出版日期:2013-09-26 发布日期:2013-09-26
  • 作者简介:汤文武(1987-),男,博士研究生,主要从事电磁法数值模拟及反演成像研究,E-mail:twwtwb@163.com
  • 基金资助:

    国家科技支撑计划项目(2011BAB04B08);有色资源与地质灾害探查湖南省重点实验室项目(2010TP4012-6);中国地质调查局科研项目(资\[2011\]03-01-64);教育部博士点基金项目(20110162120064)

Finite Element Forward Modeling on Line Source of FCSEM for Continuous Conductivity

Tang Wenwu1,2, Liu Jianxin1,2,Tong Xiaozhong1,2   

  1. 1.School of Geosciences and InfoPhysics, Central South University, Changsha410083, China;
    2. Hunan Key Laboratory of NonFerrous Resources and Geological Hazard Detection, Changsha410083, China
  • Received:2012-12-05 Online:2013-09-26 Published:2013-09-26

摘要:

为了更好地模拟地下介质连续变化及开展连续介质的反演,对二维电导率分块线性变化的线源频率域可控源电磁法进行了有限元正演模拟,在剖分单元内同时对电场及电导率参数线性插值,使电导率参数在剖分单元之间保持连续变化。首先,提出有限元正演模拟的边值问题及变分问题,并详细论述了有限元的剖分、插值、单元分析及总体合成的各个步骤;其次,采用稀疏存储及基于不完全LU分解的BICGSTAB算法求解复系数方程组,节省了内存并提高了计算速度;然后,对一个均匀半空间模型进行模拟,计算结果表明,低频及高频的有限元数值解都与解析解吻合,证明了算法的正确性;最后,对水平层状模型及垂直断层模型进行正演计算,视电阻率及相位的等值线图均较好地反映出了异常体,说明文中算法能够对电导率连续变化的线源可控源电磁法进行有效地模拟。

关键词: 分块线性变化, 线源, 频率域可控源电磁法, 有限元正演模拟

Abstract:

In order to simulate continuous conductivity of subsurface medium and inverse continuous medium, we worked on the finite element forward modeling on line source of FCSEM (frequency domain controlled-source electromagnetic) for two-dimensional block linear change of conductivity. In each unit, the linear interpolation both for electrical field and conductivity parameter was used, which would keep conductivity changing continuously between each unit. Firstly, boundary value problem and variational problem were given for finite element simulation. And the meshing, interpolation, unit analysis and total synthesis of FEM (finite element method) were discussed in detail. Secondly, sparse storage and BICGSTAB algorithm based on incomplete LU decomposition were used to solve complex equations, which had saved memory and improved compute speed. Then, a homogenous half space model was simulated and its result showed that the FEM numerical solutions of low and high frequency agreed with analytic solutions very well, which proved the correctness of this algorithm. Finally, a horizontal layered model and a vertical fault model were calculated, the contour maps both for apparent resistivity and phase reflected anomaly quite well. All of these had showed this algorithm can simulate the line source of FCSEM for continuous conductivity effectively.

Key words: block linear change, line source, frequency domain controlled-source electromagnetic, finite element forward modeling

中图分类号: 

  • P631.2
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