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Numerical Simulation of the Effect of a DC Electric Field on Seismic Wave Propagation with the Pseudospectral Time Domain Method

机译:伪谱时域法对直流电场对地震波传播影响的数值模拟

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We have modeled the effect of a direct current (DC) electric field on the propagation of seismic waves by the pseudospectral time domain (PSTD) method, based on a set of governing equations for the poroelastic media. This study belongs to the more general term of the seismoelectric coupling effect. The set of physical equations consists of the poroelastodynamic equations for the seismic waves and the Maxwell's equations for the electromagnetic waves; the magnitude of the seismoelectric coupling effect is characterized by the charge density, the electric conductivity, the Onsager coefficient, a function of the dielectric permittivity, the fluid viscosity, and the zeta potential. The poroelastodynamic vibration of a solid matrix generates an electric oscillation with the form of streaming current via the fluctuation of pore pressure. Meanwhile, fluctuating pore pressure also causes oscillatory variation of the electric resistivity of the solid matrix. The simulated poroelastic wave propagation and electric field variation with an existing background DC electric field are compared with the results of a physical experiment carried out in an oilfield. The results show that the DC electric field can significantly affect the propagating elastic energy through the seismoelectric coupling in a wide range of the seismic frequency band.
机译:我们基于多孔弹性介质的一组控制方程,通过伪谱时域(PSTD)方法对直流(DC)电场对地震波传播的影响进行了建模。这项研究属于地震电耦合效应的更广义术语。物理方程组由地震波的孔隙弹性方程和电磁波的麦克斯韦方程组成。地震电耦合效应的大小由电荷密度,电导率,昂萨格系数,介电常数,流体粘度和ζ电势的函数表征。固体基质的孔隙弹性动力学振动通过孔隙压力的波动产生以流动电流形式的电振荡。同时,孔隙压力的波动还引起固体基质的电阻率的振荡变化。将模拟的多孔弹性波传播和电场变化与现有的背景直流电场进行了比较,并与在油田进行的物理实验结果进行了比较。结果表明,直流电场可以在较大的地震频带范围内通过地震电耦合显着影响传播的弹性能。

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