The seismo-electromagnetic method (SEM) can be used for non-invasive subsurface
exploration. It shows interesting results for detecting fluids such as water, oil, gas, CO 2, or …

The self-potential method enables non-intrusive assessment and imaging of disturbances in
electrical currents of conductive subsurface materials. It has an increasing number of …

Seismic waves propagating in a porous medium, under favourable conditions, generate
measurable electromagnetic fields due to electrokinetic effects. It has been proposed …

We consider a linear poroelastic material filled with a linear viscoelastic solvent like wet
heavy oils (oil as opposed to water or brines is wetting the surfaces of the pores). We extend …

To better understand and interpret seismoelectric measurements acquired over vadose
environments, both the existing theory and the wave propagation modelling programmes …

I review current understanding of the low-frequency electrical properties of glaciers and ice
sheets, and identify future research directions that challenge near-surface geophysicists and …

The seismoelectric method consists of measuring electromagnetic signals associated with
the propagation of seismic waves or seismic sources in porous media. This method is useful …

Is groundwater abundant in Antarctica and does it modulate ice flow? Answering this
question matters because ice streams flow by gliding over a wet substrate of till. Water fed to …

The interpretation of seismoelectrical signals is a difficult task because coseismic and
seismoelectric converted signals are recorded simultaneously and the seismoelectric …

A new approach of seismoelectric imaging has been recently proposed to detect saturation
fronts in which seismic waves are focused in the subsurface to scan its heterogeneous …