We review theoretical and computational research, primarily from the past 10 years,
addressing the flow of reactive fluids in porous media. The focus is on systems where …

The transport of fluids through the Earth's crust controls the redistribution of elements to form
mineral and hydrocarbon deposits, the release and sequestration of greenhouse gases, and …

Fluid–rock interaction has profound effects on the dynamics of the lithosphere. This
Perspectives article describes the catalytic effects of water on the kinetics of mineral …

The equilibration of minerals in the presence of an aqueous fluid phase, with which it is out
of equilibrium, has been described in terms of a number of potential mechanisms …

Understanding the mechanism and kinetics of the replacement of carbonates by fluorite has
applications in Earth sciences and engineering. Samples of Carrara marble were reacted …

The zeta potential of a particle characterizes its motion in an electric field and is often
thought to be negligible at high ionic strength (several moles per liter) due to thinning of the …

Selective transport of water, salt, and ionic current across water-filled nanopores is a key
feature in a variety of natural and engineered systems including geologic media, biological …

We investigate the feedback between antigorite dehydration reactions and fluid extraction
mechanisms through the analysis of field-scale structures and microtextures formed by …

In this contribution, we use X-ray computed micro-tomography (X-CT) to observe and
quantify dynamic pattern and porosity formation in a fluid-mediated replacement reaction …

Existing theories can predict separately the effects of hydrodynamic slip and ion–ion
electrostatic correlations on diffusioosmosis. However, a predictive model for the coupled …