大学物理 ›› 2008, Vol. 27 ›› Issue (6): 6-6.

• 著者文摘 • 上一篇    下一篇

水平层状介质并矢Green函数的递推矩阵方法

魏宝君[1,2] 张庚骥[1] LIU Q H[2]   

  1. [1]中国石油大学(华东)物理科学与技术学院,山东东营257061 [2]Department of Electrical & Computer Engineering, Duke University, Durham, NC 27708,USA
  • 出版日期:2008-06-25 发布日期:2008-06-20

Recursive matrix method of dyadic Green's functions for horizontally stratified media

  • Online:2008-06-25 Published:2008-06-20

摘要: 采用递推矩阵方法计算任意数目水平层状介质的并矢Green函数.根据层界面处电场和磁场的连续性条件得到3个确定Sommerfeld积分待定系数的矩阵方程组,分别对应于垂向单位电偶极子产生的TM波、水平方向单位电偶极子产生的TE波和TM波,这些方程组均可通过递推方法快速求解.只需改变3个方程组中源项元素的位置,就可以方便地得到当源点和场点在任意层时的并矢Green函数.本文给出的并矢Green函数表达式形式简洁且不含指数增加项,计算时不会出现溢出现象.

关键词: 并矢Green函数, 层状介质, 递推矩阵方法, Sommerfeld积分

Abstract: A recursive matrix method is adopted for the computation of dyadic Green' s functions in horizontally stratified media with arbitrary number of layers. Three matrix equation groups for computing the coefficients of the Sommerfeld integrals are obtained according to the continuity condition of electric and magnetic fields across the interface between different layers, which are in correspondence with the TM wave produced by a vertical unit electric dipole and the TE or TM wave produced by a horizontal unit electric dipole, respectively. All the equation groups can be quickly solved via the recursive method. The dyadic Green's functions with source point and field point be- ing in any layer can be conveniently obtained by merely changing the position of the elements within the source term of the equation groups. The expression of the dyadic Green's functions provided by this paper is terse in form and does not have exponentially increasing term, so it does not overflow during computation.

Key words: dyadic Green's functions, stratified media, recursive matrix methed, Sommerfeld integrals

中图分类号: 

  • O441.4