Abstract

We consider the effects of oblique incidence of a wave on the creation of a 3-D image of a planar interface with an array-type directional borehole radar. In this study, we focus on the situation where the radar probe is close to the planar interface. In such circumstances, the reflected wave from the planar interface may be incident on the receiving array antenna at very steep elevation angles. As a result, borehole effects cause differences in the arrival times of the wave at the array elements, and consequently some errors emerge in imaging the planar interface. Observing the arrival time differences, we present an algorithm to compensate those errors in creating a 3-D image of a planar interface. Computer simulations predict that the errors may occur when the circular dipole array antenna is in an air-filled borehole in rock. Numerical simulations show that our proposed algorithm generates a 3-D image of an interface around an exact position, whereas conventional methods produce some spurious images opposite to the correct position (i.e., out of position by 180°). We then applied the proposed method to analyze reflected waves from a real-world fault in rock. A 3-D image of the fault could be successfully created, which was not possible using the conventional method.

Highlights

  • T HREE-DIMENSIONAL reconstruction of geological interfaces, faults, and fractures in rocks is essential for effective use of underground space

  • We find that the existence of critical receiver position zrc (CRP) would influence the planar interface measurement significantly, especially when we use the CAB in an air-filled borehole in rock

  • We present an algorithm to create a 3-D image of a planar interface with the CAB directional borehole radar in situations where the antennas are close to the interface

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Summary

INTRODUCTION

T HREE-DIMENSIONAL reconstruction of geological interfaces, faults, and fractures in rocks is essential for effective use of underground space. The singlehole borehole radar can image rock interfaces with energy flow domain reverse-time migration [10]. The order of arrival at the dipole elements at a steeper incident elevation angle than the CEA is opposite to that for normal incidence In this case, the azimuthal component of the electric field on the cylindrical boundaries has a larger magnitude than the vertical one. The azimuthal component of the electric field on the cylindrical boundaries has a larger magnitude than the vertical one This fact causes the difference in the arrival order between the normal and oblique incidence cases. Such phenomena should influence DOA estimation with the CAB.

DOA ESTIMATION WITH THE CAB
REFLECTION FROM A PLANAR INTERFACE
Formulation
Analysis
CAB Signal Generation With MoM
FIELD EXPERIMENTS
CONCLUSION
Relationship Between the CEA and the Interface Dip Angle
Dependency of CEA on Permittivity in Outermost Layer
Slope of Reflected Wave Arrival Time in Radargram
Electric Field Radiated by a z-Directed Dipole in a Borehole
Error of Calculation of Reflection at a Planar Interface
Findings
Verification of the MoM Signal With FDTD
Full Text
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