Migration of ground‐penetrating radar data with a finite‐element method that considers attenuation and dispersion

Author:

Di Qingyun1,Wang Miaoyue2

Affiliation:

1. Chinese Academy of Sciences, Institute of Geology and Geophysics, P.O. Box 9825, Beijing 100029, China.

2. Consultant, Chinese Academy of Sciences, Institute of Geology and Geophysics, Beijing 100029, China.

Abstract

We use a numerical model to study the effects of attenuation and dispersion upon the migration of ground‐penetrating radar (GPR) profiles. A finite‐element method (FEM) is developed that incorporates attenuation and is used to generate synthetic GPR profiles with random noise. These profiles are then migrated with and without the attenuation term using our FEM codes. The misfit between the position of interfaces in the model and the position of corresponding interfaces in the migrated profile is greatly decreased when the attenuation term is considered in the migration process. The improvement in resolution results from the use of the group velocity rather than any phase velocity. Consequently, for dispersive media the attenuation term of high‐frequency GPR waves cannot be ignored in migration.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference13 articles.

1. Christian, S., Dietrich, R., and Nick, K. P., 1994, Eccentricity‐migration for the imaging of pipes in radar reflection data: 56th Annual Meeting, European Association of Geologists and Engineers, Extended Abstracts, 1014.

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