Ground-penetrating radar theory and application of thin-bed offset-dependent reflectivity

Author:

Bradford John H.12,Deeds Jacob C.12

Affiliation:

1. Boise State University, Center for Geophysical Investigation of the Shallow Subsurface, 1910 University Drive, Boise, Idaho 83725-1536.

2. ChevronTexaco, ETC-Contractor Acquisition and Processing QC Team, 4800 Fournace Place, Room W645, Bellaire, Texas 77401.

Abstract

Offset-dependent reflectivity or amplitude-variation-with-offset (AVO) analysis of ground-penetrating radar (GPR) data may improve the resolution of subsurface dielectric permittivity estimates. A horizontally stratified medium has a limiting layer thickness below which thin-bed AVO analysis is necessary. For a typical GPR signal, this limit is approximately 0.75 of the characteristic wavelength of the signal. Our approach to modeling the GPR thin-bed response is a broadband, frequency-dependent computation that utilizes an analytical solution to the three-interface reflectivity and is easy to implement for either transverse electric (TE) or transverse magnetic (TM) polarizations. The AVO curves for TE and TM modes differ significantly. In some cases, constraining the interpretation using both TE and TM data is critical. In two field examples taken from contaminated-site characterization data, we find quantitative thin-bed modeling agrees with the GPR field data and available characterization data.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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