Borehole acoustic full-waveform inversion

Author:

Tang Huaigu1ORCID,Cheng Arthur Chuen Hon2,Li Yunyue Elita3ORCID,Fang Xinding4ORCID,Wang Ruijia5ORCID,Wu Xiang5ORCID

Affiliation:

1. National University of Singapore, Department of Civil and Environmental Engineering, Singapore and Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China.

2. The Chinese University of Hong Kong, Earth Systems Science Programme, Shatin, Hong Kong SAR and National University of Singapore, Department of Civil and Environmental Engineering, Singapore.

3. Purdue University, Department of Earth, Atmospheric, and Planetary Sciences, Indiana, USA and National University of Singapore, Department of Civil and Environmental Engineering, Singapore. (corresponding author)

4. Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China.

5. Halliburton, Singapore, Singapore.

Abstract

Full-waveform inversion (FWI) is a technique that has the potential for building high-resolution elastic velocity models. We apply this technique to wireline monopole acoustic logging data to image the near-wellbore formation velocity structures, which can be used in a fluid intrusion evaluation. Our FWI workflow is established in cylindrical coordinates instead of Cartesian coordinates to adapt to the borehole geometry. Assuming that the acoustic logging tool is centralized and formation properties are azimuthally invariant, we can simplify the problem to two dimensions in the inversion. Synthetic tests find that the high-resolution P- and S-wave velocity model around the borehole could be successfully inverted using FWI once a reasonable starting velocity model is given. However, borehole FWI differs from seismic FWI in that strong borehole-guided waves exist near the borehole wall due to the elastic effects. The borehole-guided waves have little sensitivity to velocity away from the borehole wall. In addition, it is difficult to simultaneously match the waveform of the body waves and guided waves in synthetic data and field data. Therefore, for field data applications, we propose to obtain the formation velocity structures around the borehole by FWI using only the first arrived P waves. The field data tests find that the proposed method is applicable for inverting the P-wave velocity structure around the borehole with a similar resolution compared with ray-tracing tomography. FWI may achieve higher resolution in field applications in the future with better assumptions made in the forward modeling and using more information in the field data.

Funder

Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology

National Natural Science Foundation of China

Shenzhen Science and Technology Program

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference46 articles.

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