Conductivity Dependence of Seismoelectric Wave Phenomena in Fluid-Saturated Sediments
نویسندگان
چکیده
Seismoelectric phenomena in sediments arise from acoustic wave-induced fluid motion in the pore space, which perturbs the electrostatic equilibrium of the electric double layer on the grain surfaces. Experimental techniques and the apparatus built to study the conductivity dependence of the electrokinetic (EK) effect are described and outcomes for studies in loose glass microspheres and medium-grain sand are presented. By varying the NaCl concentration in the pore fluid, we measured the conductivity dependence of two kinds of EK behavior: (1) the electric fields generated within the samples by the passage of transmitted acoustic waves, and (2) the electromagnetic waves produced at the fluid–sediment interface by the incident acoustic wave. Both phenomena are caused by relative fluid motion in the sediment pores—this feature is characteristic of poroelastic (Biot) media, but not predicted by either viscoelastic fluid or solid models. A model of plane-wave reflection from a fluid–sediment interface using EK–Biot theory leads to theoretical predictions that compare well to the experimental data for both loose glass microspheres and medium-grain sand.
منابع مشابه
Experimental and Theoretical Studies of Seismoelectric Effects in Boreholes
In a fluid-saturated porous formation, an impinging seismic wave induces fluid motion. The motion of fluid relative to the rock frame generates an electric streaming current. This current produces electric and magnetic fields, which are called seismoelectric and seismomagnetic fields, respectively. When there is a fracture or a discontinuity, a radiating electromagnetic wave is also generated, ...
متن کاملAn Algorithm for Modeling and Interpretation of Seismoelectric Data
Generally speaking, seismoelectric modeling is a prospecting method based on seismic and electromagnetic waves, in which waves generated by a seismic source at the boundary of the two environments generate a relative fluid-solid motion formed as a result of antagonism between the elastic properties of the environment with the saturated fluid. This research has as its objective, a study of the e...
متن کاملE ects of Saturant Conductivity on Seismoelectric Conversion
When a seismic wave propagates in a uid-saturated porous medium, a seismoelectric eld can be induced in the medium due to an electric double layer at the interface between solid and uid. The strength of the seismoelectric eld depends on the characteristics of the double layer and the conductivity of the saturant uid. In our experiments two kinds of seismoelectric elds, a radiating electromagnet...
متن کاملhy si cs Seismoelectric wave propagation numerical modelling in partially saturated materials
To better understand and interpret seismoelectric measurements acquired over vadose environments , both the existing theory and the wave propagation modelling programmes, available for saturated materials, should be extended to partial saturation conditions. We propose here an extension of Pride's equations aiming to take into account partially saturated materials, in the case of a water–air mi...
متن کاملExperimental Studies of Electrokinetic Conversions in a Fluid-saturated Porous Medium
The electrokinetic effect in a fluid-saturated porous rock is defined as the coupling and conversion between seismic and electric energies. When seismic waves propagate through a fluid-saturated formation and cause a pore fluid-flow relative to the solid matrix, the motion of the cations in the fluidflow forms a streaming electrical current and induces an electromagnetic wave at any discontinuo...
متن کامل