Elastic wave radiation and reception of a borehole dipole source in a vertically transverse isotropic formation

Author:

Gu Xi-Hao1ORCID,Tang Xiao-Ming2ORCID,Su Yuan-Da3ORCID,Li Sheng-Qing3ORCID

Affiliation:

1. China University of Petroleum (East China), School of Geosciences, Qingdao, China and Key Laboratory of Deep Oil and Gas (China University of Petroleum (East China)), Qingdao, China.

2. China University of Petroleum (East China), School of Geosciences, Qingdao, China; Key Laboratory of Deep Oil and Gas (China University of Petroleum (East China)), Qingdao, China; and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China. (corresponding author)

3. China University of Petroleum (East China), School of Geosciences, Qingdao, China; Key Laboratory of Deep Oil and Gas (China University of Petroleum (East China)), Qingdao, China; and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China.

Abstract

Single-well acoustic imaging using a dipole tool has been applied in anisotropic formations. For this application, the effect of anisotropy on the radiation and reception of acoustic waves in the borehole needs to be analyzed and a proper analysis method needs to be developed. We use the far-field asymptotic solution of the wavefield to calculate the radiation pattern of the dipole source in a borehole penetrating vertically transverse isotropic (VTI) formation. We model the spherical wave propagation characteristics of the radiated and reflected waves in the VTI formation and the receiving of the waves in the borehole for the on- and off-axis positions. Based on the developed analytical modeling methods, we study systematically the effects of the formation anisotropy on the radiation pattern and borehole response characteristics. Our modeling result demonstrates that due to the coupling between the longitudinal and the transverse particle motions, quasi-P-(qP-) and quasi-SV-(qSV-) wave radiation patterns contain two components. The result also indicates that the anisotropy causes the arrival time of the SH-reflection wave to differ from that of the qSV wave, and the misposition of the imaged targets would occur if the velocity measured along the borehole is used for migration. The azimuth sensitivity of the off-axis data can be used to help eliminate the 180° ambiguity for the dipole acoustic imaging in the VTI formation. Understanding the effects of anisotropy on borehole acoustic imaging can help improve the accuracy of the imaging result in anisotropic formations.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Shandong Province

the Innovation fund project for a graduate student of China University of Petroleum (East China), supported by the Fundamental Research Funds for the Central Universities

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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