Print Email Facebook Twitter Seismoelectric numerical simulation in 2D vertical transverse isotropic poroelastic medium Title Seismoelectric numerical simulation in 2D vertical transverse isotropic poroelastic medium Author Tohti, Munirdin (Chinese Academy of Sciences) Wang, Yibo (Chinese Academy of Sciences) Slob, E.C. (TU Delft Applied Geophysics and Petrophysics) Zheng, Yikang (Chinese Academy of Sciences) Chang, Xu (Chinese Academy of Sciences) Yao, Yi (Chinese Academy of Sciences) Date 2020 Abstract Seismoelectric coupling in an electric isotropic and elastic anisotropic medium is developed using a primary–secondary formulation. The anisotropy is of vertical transverse isotropic type and concerns only the poroelastic parameters. Based on our finite difference time domain algorithm, we solve the seismoelectric response to an explosive source. The seismic wavefields are computed as the primary field. The electric field is then obtained as a secondary field by solving the Poisson equation for the electric potential. To test our numerical algorithm, we compared our seismoelectric numerical results with analytical results obtained from Pride's equation. The comparison shows that the numerical solution gives a good approximation to the analytical solution. We then simulate the seismoelectric wavefields in different models. Simulated results show that four types of seismic waves are generated in anisotropic poroelastic medium. These are the fast and slow longitudinal waves and two separable transverse waves. All of these seismic waves generate coseismic electric fields in a homogenous anisotropic poroelastic medium. The tortuosity has an effect on the propagation of the slow longitudinal wave. The snapshot of the slow longitudinal wave has an oval shape when the tortuosity is anisotropic, whereas it has a circular shape when the tortuosity is isotropic. In terms of the Thomsen parameters, the radiation anisotropy of the fast longitudinal wave is more sensitive to the value of ε, while the radiation anisotropy of the transverse wave is more sensitive to the value of δ. Subject Poroelastic mediumSeismoelectric couplingThomsen parametersVertical transverse isotropy To reference this document use: http://resolver.tudelft.nl/uuid:282697ba-7bee-41a1-b4f9-79972cca891e DOI https://doi.org/10.1111/1365-2478.12958 Embargo date 2020-10-13 ISSN 0016-8025 Source Geophysical Prospecting, 68 (6), 1927-1943 Bibliographical note Green Open Access added to TU Delft Institutional Repository ‘You share, we take care!’ – Taverne project https://www.openaccess.nl/en/you-share-we-take-care Otherwise as indicated in the copyright section: the publisher is the copyright holder of this work and the author uses the Dutch legislation to make this work public. Part of collection Institutional Repository Document type journal article Rights © 2020 Munirdin Tohti, Yibo Wang, E.C. Slob, Yikang Zheng, Xu Chang, Yi Yao Files PDF 1365_2478.12958.pdf 9.6 MB Close viewer /islandora/object/uuid:282697ba-7bee-41a1-b4f9-79972cca891e/datastream/OBJ/view