Implementation of ADI-FDTD subgrids in ground penetrating radar FDTD models

被引:46
作者
Diamanti, Nectaria [1 ]
Giannopoulos, Antonios [1 ]
机构
[1] Univ Edinburgh, Sch Engn & Elect, Inst Infrastruct & Environm, Edinburgh EH9 3JL, Midlothian, Scotland
基金
英国工程与自然科学研究理事会;
关键词
Alternating-direction implicit finite-difference time-domain (ADI-FDTD) method; GPR modeling; Subgridding; Unconditionally stable; FINITE-DIFFERENCE METHOD; PERFECTLY MATCHED LAYER; NUMERICAL-SOLUTION; MAXWELLS EQUATIONS; ALGORITHM; SIMULATION; MEDIA; WAVES;
D O I
10.1016/j.jappgeo.2008.07.004
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Realistic numerical modeling of ground penetrating radar (GPR) using, the finite-difference time-domain (FDTD) method could greatly benefit from the implementation of subgrids - supporting finer spatial resolution - into the conventional FDTD mesh. This is particularly important, when parts of the computational domain need to be modeled in detail or when there are features or regions in the overall computational mesh with values of high dielectric constant Supporting propagation of waves at very short wavelengths. A scheme that simplifies the process of implementing these subgrids into the traditional FDTD method is presented. This scheme is based oil the combination of the standard HAD method and the unconditionally stable alternating-direction implicit (ADI) FDTD technique. Because ADI-FDTD is unconditionally stable its time-step can be set to ally Value that facilitates the accurate Calculation Of the fields. By doing so, the two grids call efficiently communicate information across their boundary Without requiring to use a costly time-interpolation scheme. This paper discusses the performance of ADI-FDTD subgrids when implemented into the traditional FDTD method, Using different communication schemes for the information exchange at the boundary of the two grids. The developed algorithm, call handle cases where the subgrid crosses dielectrically inhomogeneous media. In addition, results from the comparison between the proposed scheme and a commonly employed purely FDTD subgridding technique are presented. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:309 / 317
页数:9
相关论文
共 27 条
[1]   A PERFECTLY MATCHED LAYER FOR THE ABSORPTION OF ELECTROMAGNETIC-WAVES [J].
BERENGER, JP .
JOURNAL OF COMPUTATIONAL PHYSICS, 1994, 114 (02) :185-200
[2]   Finite-difference modeling of electromagnetic wave propagation in dispersive and attenuating media [J].
Bergmann, T ;
Robertsson, JOA ;
Holliger, K .
GEOPHYSICS, 1998, 63 (03) :856-867
[3]   A fully three-dimensional simulation of a ground-penetrating radar: FDTD theory compared with experiment [J].
Bourgeois, JM ;
Smith, GS .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 1996, 34 (01) :36-44
[4]  
CASSIDY NJ, 2001, THESIS KEELE U UK
[5]   FDTD local grid with material traverse [J].
Chevalier, MW ;
Luebbers, RJ ;
Cable, VP .
IEEE TRANSACTIONS ON ANTENNAS AND PROPAGATION, 1997, 45 (03) :411-421
[6]   Perfectly matched layers for elastodynamics: A new absorbing boundary condition [J].
Chew, WC ;
Liu, QH .
JOURNAL OF COMPUTATIONAL ACOUSTICS, 1996, 4 (04) :341-359
[7]  
DIAMANTI N, 2007, P 2007 INT S ANT PRO
[8]   A nonsplit complex frequency-shifted PML based on recursive integration for FDTD modeling of elastic waves [J].
Drossaert, Francis H. ;
Giannopoulos, Antonios .
GEOPHYSICS, 2007, 72 (02) :T9-T17
[9]   On the dispersion relation of ADI-FDTD [J].
Garcia, Salvador G. ;
Rubio, R. Godoy ;
Bretones, A. Rubio ;
Martin, R. Gomez .
IEEE MICROWAVE AND WIRELESS COMPONENTS LETTERS, 2006, 16 (06) :354-356
[10]   An anisotropic perfectly matched layer-absorbing medium for the truncation of FDTD lattices [J].
Gedney, SD .
IEEE TRANSACTIONS ON ANTENNAS AND PROPAGATION, 1996, 44 (12) :1630-1639