J4 ›› 2012, Vol. 42 ›› Issue (2): 545-553.

• 地球探测与信息技术 • 上一篇    下一篇

论直流电位场拟解析近似中的电位与电荷反射函数的物理意义

孙 建 国   

  1. 1.吉林大学地球探测科学与技术学院|长春130026;
    2.国土资源部应用地球物理综合解释理论开放实验室/波动理论与成像技术实验室|长春130026
  • 收稿日期:2011-10-26 出版日期:2012-03-26 发布日期:2012-03-26
  • 作者简介:孙建国(1956-)|男|教授|博士生导师|主要从事地下波动理论与成像技术、地震资料处理方法等方面的教学和研究工作|E-mail:sun_jg@jlu.edu.cn
  • 基金资助:

    国家自然科学基金项目(40074029);国家“863”计划项目(2006AA06Z109)

On the Physical Meaning of the Surface Potential and the Surface Charge Density Reflection Functionsin in the Quasi-Analytical Approximations of the D.C. Electrical Potential Field

SUN Jian-guo   

  1. 1.College of GeoExploration Science and Technology, Jilin University, Changchun130026, China;
    2.Laboratory for Integrated Geophysical Interpretation Theory of Ministry for Land and Resources/Laboratory for Wave Theory and Imaging Technology, Changchun130026, China
  • Received:2011-10-26 Online:2012-03-26 Published:2012-03-26

摘要:

为了避开由大型代数方程组数值求解所带来的问题,将电场反射张量的基本概念和拟解析近似的基本思想引入到了直流电位场的数值模拟中,定义了体电位反射函数、面电荷反射函数和面电位反射函数等3个辅助函数,并给出了其在一般条件下的拟解析近似解和在简单条件下(均匀或点电流源背景场、均匀导电柱体或球体)的分析解。简单的对比分析证明:面电荷反射函数是异常体表面上自由面电荷密度的函数;在简单条件下,这种函数关系转化成为比例关系;类似的结论对于简单条件下的面电位反射函数也成立;然而,在一般条件下难以建立面电位反射函数和自由面电荷密度之间的明确关系。

关键词: 地球物理勘探-电法, 直流电位场, 拟解析近似, 反射函数, 物理意义

Abstract:

For avoiding the problems caused by solving large linear equation systems numerically, we introduce the basic concept of the electrical reflectivity tensor and the basic idea of the quasi-analytical approximation into D.C. electrical potential field, and define three auxiliary functions, namely the volume potential reflection function, the surface potential reflection function, and the surface charge density reflection function. Also, we give the quasi-analytical approximations to the reflection functions for general cases and the analytical solutions of the reflection function in simple situations, i.e. a uniform or a point current source background electrical field and uniform cylinders and spheres as the anomalous body. Simple comparison shows that the surface charge density reflection function is a function of the free surface charge density on the surface of the anomalous body under consideration. In simple situations described above, the function reduces into a simple proportional relationship. The same is true for the surface potential reflection function in simple cases. However, in general cases it is difficult to establish an explicit relationship between the surface reflection function and the free surface charge density.

Key words: geophysical prospecting-electrical, D. C. electrical potential field, quasi-analytical approximation, reflection function, physical meaning

中图分类号: 

  • P631.3
[1] 刘永亮, 李桐林, 朱成, 关振伟, 苏晓波. 基于拟线性积分方程法的三维电磁场数值模拟精度分析[J]. 吉林大学学报(地球科学版), 2017, 47(4): 1268-1277.
[2] 张金会, 孙建国. 三维直流电场积分方程中奇异性的近似处理[J]. J4, 2009, 39(5): 923-928.
[3] 孙建国. 声波散射数值模拟的两种新方案[J]. J4, 2006, 36(05): 863-868.
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