We describe in this paper the theoretical background for the electrokinetics in rocks and in
porous media, to be included in the special issue “Electrokinetics in Earth Sciences” of …

We solve the 3-D gravity inverse problem using a massively parallel voxel (or finite element)
implementation on a hybrid multi-CPU/multi-GPU (graphics processing units/GPUs) cluster …

We present a new unified model for the permeability, electrical conductivity and streaming
potential coupling coefficient in variably saturated fractured media. For those, we …

Potential field interpretation can be carried out using multiscale methods. This class of
methods analyses a multiscale data set, which is built by upward continuation of the original …

The understanding of electrokinetics for unsaturated conditions is crucial for numerous of
geophysical data interpretation. Nevertheless, the behaviour of the streaming potential …

Streaming‐potentials are produced by electrokinetic effects in relation to fluid flow and are
used for geophysical prospecting. The aim of this study is to model streaming potential …

The electrokinetics methods have great potential to characterize hydrogeological processes
in porous media, especially in complex partially saturated hydrosystems (eg, the vadose …

Seismoelectromagnetic conversions are induced through electrokinetic phenomena
occurring when passing seismic waves induce relative fluid to solid displacements …

Global optimization for the interpretation of Self-Potential (SP) anomaly using a very fast
simulated-annealing (VFSA) inversion code is developed in the present study. The SP …

Streaming potential is the result of coupling between a fluid flow and an electric current in
porous rocks. The modified Helmholtz–Smoluchowski equation derived for capillary tubes is …