RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1003, doi:10.2205/2017ES000591, 2017
Figure 3. The structure of the electrical double layer and potential distribution in it: 1, the inner Helmholtz plane; 2, the outer Helmholtz plane; 3, the slipping plane. Distance $x$ is measured from the boundary of the phases, and potential $\varphi$ is measured from a certain depth level in the fluid.
Citation: Gavrilov V. A., A. V. Naumov (2017), Modulation of geoacoustic emission intensity by time-varying electric field, Russ. J. Earth Sci., 17, ES1003, doi:10.2205/2017ES000591.
Copyright 2017 by the Geophysical Center RAS.
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