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起伏地表条件下三维直流电场拟解析近似方法

张金会 刘德鹏 张亚东

物探与化探2012,Vol.36Issue(4):692-696,5.
物探与化探2012,Vol.36Issue(4):692-696,5.

起伏地表条件下三维直流电场拟解析近似方法

THE QUASI-ANALYTICAL METHOD FOR THE THREE-DIMENSIONAL D.C.ELECTRICAL FIELD MODELING ON UNDULATE TOPOGRAPHY

张金会 1刘德鹏 1张亚东2

作者信息

  • 1. 安徽省勘查技术院,安徽 蚌埠 233005
  • 2. 长庆油田公司勘探部,陕西 西安 710021
  • 折叠

摘要

Abstract

The quasi-analytical method is a means for solving integration equations. To study the three-dimensional D. C. electrical field under surface topography, this paper puts forward the formula of the quasi-analytical theory for the three-dimensional D. C. electrical field under the surface topography based on the quasi-analytical theory for the whole space. The authors divide the anomalous electric field at the surface into two parts, one is the body anomalous electric field caused by the anomalous body, which can be solved by the body integral, whereas the other is the surface anomalous electric field resulting from the interface between the earth and the air, which can be calculated by the surface integral. The authors inferred the body electrical reflectivity tensor and the surface electrical reflectivity tensor separately. The quasi-analytical theory was used to deduce the formula of the quasi-analytical theory under the surface topography. This formula can give us a train of thought for solving the surface topography problem. It can enrich the quasi-analytical theory and promote the forward and inverse modeling of the D. C. electrical field, thus laying a foundation for eliminating the effect of the surface topography.

关键词

起伏地表/拟解析近似/三维直流电场/电反射函数

Key words

surface topography/quasi-analytical method/three-dimensional D. C. electric field/electric reflectivity

分类

天文与地球科学

引用本文复制引用

张金会,刘德鹏,张亚东..起伏地表条件下三维直流电场拟解析近似方法[J].物探与化探,2012,36(4):692-696,5.

物探与化探

OACSCDCSTPCD

1000-8918

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