探地雷达时域有限差分法正演模拟
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摘要
在以往雷达波的正演模拟中,借鉴地震波中成熟的正演模拟方法,均采用模拟声波方程的方法,精度不够高。因此从麦克思韦方程组出发,采用目前电磁场理论中最常用的时域有限差分法,对探地雷达进行了正演模拟。为了进一步说明其正确性,对正演模拟的结果又进行了偏移处理,从结果看出该方法的正确性及可行性。
The sound wave equation simulation method has been traditionally used in forward simulation of GPR.Nevertheless,as the radar wave is a kind of electromagnetic wave and the spread of the wave accords with Maxwell equation,the result of simulation is not precise enough.To solve this problem,the authors adopted the finite difference time domain method to perform simulation on the basis of Maxwell equation.In addition,the migration processing was conducted for the simulation result.It is found out that this method is correct and feasible.
引文
[1]W ang T l,Tripp A C.S imu lation of electromagnetic wave propaga-tion in three d im ensional m ed ia by an FDTD m ethod[J].1994,247.
    [2]Chen H W,Huang T M.F in ite-d ifference tim e-domain simu lationof GPR data[J].Journal ofApplied Geophysics,1998,40:139.
    [3]王长清,祝西里.电磁场计算中的时域有限差分法[M].北京:北京大学出版社,1994.
    [4]高本庆.时域有限差分法[M].北京:国防工业出版社,1995.
    [5]高本庆,陈金元.色散媒质中电磁场的时域有限差分算法[J].中国科学,1994,24(5):538.
    [6]高本庆,刘波.电磁场时域数值技术新进展[J].北京理工大学学报,2002,22(4):401.

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