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 …

The self-potential (SP) method is a passive geophysical method based on the natural
occurrence of electrical fields on the Earth's surface. Combined with other geophysical …

The electrokinetic potential results from the coupling between the water flow and the
electrical current because of the presence of ions within water. The electrokinetic coefficient …

Downhole measurements of electrokinetic potential are a promising new technology for
hydrocarbon reservoir monitoring. Using a 3D finite-element model combining both …

Spontaneous potentials associated with volcanic activity are often interpreted by means of
the electrokinetic potential, which is usually positive in the flow direction (ie Zeta potential of …

Earthquakes are induced by man‐made changes of the stress field by injection or
withdrawal of fluids in hydrocarbon production, geothermal exploitation, and wastewater …

In this paper, we report on a series of experiments aimed at testing the possibility of
detecting concentration or pH fronts advected through a well‐controlled, laboratory‐scale …

We measured the variations of the self‐potential (SP) during periodic pumping tests
performed at a test site located near a freshwater reservoir (Kemnader See, Bochum …

We report on an experiment aimed at testing the use of self-potential measurements to
monitor the motion and mixing of redox reactants advected through a well-controlled …

In this paper, a numerical method for solving the Biot poroelastic equations is developed.
These equations comprise acoustic (typically water) and elastic (porous medium frame) …