Electrical transport properties of saturated porous media, such as soils, rocks and fractured
networks, typically composed of a non-conductive solid matrix and a conductive brine in the …

The most common method for in situ assessment of soil salinity, namely the electrical
conductivity (EC) of the soil solution (ECw), is to measure the apparent electrical conductivity …

The five large moons of Uranus are important targets for future spacecraft missions. To
motivate and inform the exploration of these moons, we model their internal evolution …

A model combining low‐frequency complex conductivity and high‐frequency permittivity is
developed in the frequency range from 1 mHz to 1 GHz. The low‐frequency conductivity …

The surface conductivity of porous rocks has two contributions: the first is associated with the
diffuse layer coating the grains and is frequency-independent as long as the diffuse layer is …

Low-frequency geoelectrical methods include mainly self-potential, resistivity, and induced
polarization techniques, which have potential in many environmental and hydrogeological …

The permeability of a sand shale mixture is analyzed as a function of shale fraction and the
permeability of the two end‐members, ie, the permeability of a clay‐free sand and the …

The complex conductivity of soils remains poorly known despite the growing importance of
this method in hydrogeophysics. In order to fill this gap of knowledge, we investigate the …

Many types of mixing model are used widely within the earth sciences to determine the
electrical properties of porous media consisting of solid and fluid phases of known …

A nondestructive and spatially integrated multielectrode method for measuring soil electrical
resistivity was tested in the Beauce region of France during a period of corn crop irrigation to …