Surface wettability is one of the major factors that regulate immiscible fluid displacement in
porous media. However, the role of pore-scale wettability heterogeneity on dynamic …

This study characterized and modeled heterogeneous surface wettability in sandstone and
investigated the role of spatial heterogeneity and correlation length of surface wettability on …

The objective of this study was to investigate the effect of wettability heterogeneity on pore–
scale characteristics of Supercritical (sc) CO 2 displacement dynamics and its capillary …

Wettability is an important factor controlling the displacement of immiscible fluids in porous
media and therefore affects the flow and transport of supercritical (sc) CO 2 in geologic …

Geological carbon storage (GCS) involves unstable drainage processes, the formation of
patterns in a morphologically unstable interface between two fluids in a porous medium …

Wetting properties of reservoir rocks and caprocks can vary significantly, and they strongly
influence geological storage of carbon dioxide in deep saline aquifers, during which CO 2 is …

Most numerical simulation studies have focused on the effect of homogenous wettability on
fluid flow dynamics; however, most rocks display spatially heterogeneous wettability …

To characterize the influence of reservoir conditions upon multiphase flow, we calculated
fluid displacements (drainage processes) in 3D pore spaces of Berea sandstone using two …

Abstract Changes in pore (throat) size, surface roughness, and mineralogy induced by
supercritical CO 2‐water‐rock reactions impact petrophysical properties such as porosity …

Geological carbon storage in deep aquifers involves displacement of resident brine by
supercritical CO 2 (scCO 2), which is an unstable drainage process caused by the invasion …