摘要
The ground penetrating radar(GPR) forward simulation all aims at the singular and regular models, such as sandwich model, round cavity, square cavity, and so on, which are comparably simple. But as to the forward of curl interface underground or “v” figure complex model, it is difficult to realize. So it is important to forward the complex geoelectricity model. This paper takes two Maxwell’s vorticity equations as departure point, makes use of the principles of Yee’s space grid model theory and the basic principle finite difference time domain method, and deduces a GPR forward system of equation of two dimensional spaces. The Mur super absorbed boundary condition is adopted to solve the super strong reflection on the interceptive boundary when there is the forward simulation. And a self-made program is used to process forward simulation to two typical geoelectricity model.
The ground penetrating radar（GPR） forward simulation all aims at the singular and regular models, such as sandwich model, round cavity, square cavity, and so on, which are comparably simple. But as to the for- ward of curl interface underground or “v” figure complex model, it is difficult to realize. So it is important to for- ward the complex geoelectricity model. This paper takes two Maxwell＇s vorticity equations as departure point, makes use of the principles of Yee＇s space grid model theory and the basic principle finite difference time domain method, and deduces a GPR forward system of equation of two dimensional spaces, The Mur super absorbed boundary condition is adopted to solve the super strong reflection on the interceptive boundary when there is the forward simulation. And a self-made program is used to process forward simulation to two typical geoelectricity model.
基金
Project(50099620)supportedbytheNationalNaturalScienceFoundationofChina
关键词
渗透雷达的地面
有限差别时间领域方法提交模拟
理想的频率分散关系
ground penetrating radar
finite difference time domain method
forward simulation
ideal frequency dispersion relationship
