Conductivity tomography at two frequencies

Author:

Cao Junxing1,He Zhenhua1,Zhu Jieshou1,Fullagar Peter K.2

Affiliation:

1. Chengdu University of Technology, State Key Laboratory of Oil and Gas Reservoir Geology and Exploration, Chengdu, 610059 China.

2. Fullagar Geophysics Pty Ltd., Level 1, 1 Swann Road, Taringa, Queensland 4068, Australia.

Abstract

We present a new approach for crosshole radio tomography. Conductivity images of the investigated area are reconstructed from the ratio of the electric field intensities measured at two similar frequencies. The method largely avoids assumptions about the radiation pattern and in‐situ intensity of the transmitting antenna, which introduce errors in conventional single‐frequency crosshole electromagnetic‐absorption tomography. Application of the method to field data achieved an improvement in resolution of anomalies over traditional single‐frequency absorption tomography. The dual‐frequency method is not a universal approach; it is suitable for moderately conductive media (<0.01 S/m) over the approximate frequency range 1–100 MHz.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference18 articles.

1. Cao, J., Nie, Z., and Zhu, J., 1998, Dual frequency conductivity tomography: 4th Internat. Symp., Soc. Expl. Geophys. Japan, Proc., 227–230.

2. Cao, J., Zhu, J., and Yan, Z., 1995, Fracture imaging using electromagnetic crosswell tomography: Proc. 3rd Soc. Expl. Geophys. Japan/Soc. Expl. Geophys. Internat. Symp. Geomography–Fracture Imaging, 220–287.

3. Computerized geophysical tomography

4. Feng, R., Zhou, H., Tao, Y., and Zhang, J., 1995, Application of electromagnetic tomography in fractured zones prospecting: Proc. 3rd Soc. Expl. Geophys. Japan Internat. Symp. Geomography–Fracture Imaging, 228–235.

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