Induced polarization response of porous media with metallic particles — Part 8: Influence of temperature and salinity

IV, we show that when the foam is confined, the connection between a local scale (typically that of a single bubble) and the global foam flow is not direct and other scales come

Besides, Raman spectra also shows that the final impregnated catalyst contains MoO 4 2- ions in electrostatic and covalent interaction with the alumina support, at equilibrium

We use tail expectiles to estimate alternative measures to the Value at Risk (VaR) and Marginal Expected Shortfall (MES), two instruments of risk protection of utmost importance

In this equation, θ denotes the liquid water content (dimensionless) and σ w is the pore water conductivity at saturation (and therefore at the initial salinity and following

Different geophysical methods can be used to detect preferential flow paths in embankment dams and dikes including ground pene- trating radar, passive and active seismic methods

In the next two subsections, we first summarize the dynamic Stern layer model above the freezing temperature and then we discuss how freezing conditions are expected to affect

Cole Cole relaxation time τ 1 versus the instantaneous conductivity of the mixture. The data of Experiments 2, 9, 10, 14 have not been added to the graph