Reactions at solid–water interfaces play a foundational role in water treatment systems,
catalysis, and chemical separations, and in predicting chemical fate and transport in the …

The soil water density is defined as the ratio of soil water mass to soil water volume. It is a
cornerstone in defining thermodynamic states of either saturated or unsaturated soils for …

When large-section rectangular pipe jacking is performed in anhydrous sand strata, due to
the special geological condition and construction specification, there are specific …

With the fast-paced growth of underground engineering, the performance demands for
construction materials are increasing. It is essential to explore the performance optimization …

Electrostatic interactions, associated with negatively charged surfaces of clay minerals,
produce a so‐called “disjoining pressure” when diffuse layers overlap, ie, at low porosity …

The conditions to obtain a macroscopic model for the thermo-osmotic coupling coefficient
which is needed for practical calculations of fluid flow in clay-rocks subjected to temperature …

Three osmotic processes have been identified in clay-rich media. Electro-and chemo-
osmosis–flows of water caused by salinity and electrical potential gradients–have so far …

In this study, a new formulation for the thermo‐osmotic permeability of natural pore solutions
containing monovalent and divalent cations is proposed. The mathematical formulation …

In the framework of the studies dealing on ability to store radioactive wastes in argillaceous
formations, signification of interstitial pressures is an important point to understand water …

Fig. S4–Modeled surface speciation diagrams of TC, with different initial concentration,
adsorption onto kaolinite (KT, 0.023, 0.045 and 0.11 mM) and montmorillonite (MT, 0.11 and …