Hierarchical wave-mode separation in the poroelastic medium using eigenform analysis

Author:

Tian Yiwei1ORCID,Yang Jidong2ORCID,Li Zhenchun3ORCID,Huang Jianping4ORCID,Qin Shanyuan1ORCID

Affiliation:

1. School of Geosciences, Key Laboratory of Deep Oil and Gas, Laboratory for Marine Mineral Resources, and National Laboratory for Marine Science and Technology,China University of Petroleum, Qingdao, China.

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

3. School of Geosciences, Key Laboratory of Deep Oil and Gas, Laboratory for Marine Mineral Resources, and National Laboratory for Marine Science and Technology, China University of Petroleum, Qingdao, China.

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

Abstract

In the elastic medium, the scalar and vector P- and S-waves decomposition has been extensively studied and some strategies can be extended to the poroelastic medium to extract P- and S-wavefields. However, there are three propagation modes in the poroelastic medium in Biot’s theory, namely, a fast P wave, a slow P wave, and an S wave. Because the propagation characteristic of a slow P wave is different from that of a fast P wave and S wave, the wavefield separation methods in the elastic medium cannot be directly applied to the poroelastic medium to produce a complete wave-mode separation. Based on the eigenform analysis, we have developed a hierarchical wavefield decomposition method to completely separate S waves and fast and slow P waves in the poroelastic medium. Using the Helmholtz decomposition, we first compute scalar and vector potential wavefields to separate P and S waves. Then, a cross-product operator is proposed to decompose fast and slow P waves based on their different polarization directions. To produce correct amplitudes and phases, we apply another cross-product operator and an amplitude correction term to the separated wavefields. Three numerical examples demonstrate that our method can produce accurate fast P-wave, slow P-wave, and S-wave separation results, and the decomposed fast and slow P waves have the same phases and amplitudes as the P-wave potential wavefields.

Funder

Major Scientific and Technological Projects of CNPC

Funds for Creative Research Groups of China

National Natural Science Foundation of China

Key Program for International Cooperation Projects of China

National Outstanding Youth Science Foundation

Startup funding of Guanghua Scholar in Geophysics Department, at China University of Petroleum

National Key RD Program of China

Strategic Priority Research Program of the Chinese Academy of Sciences

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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