Dissolution trap** is one of the crucial trap** mechanisms for geological carbon storage
in deep saline aquifers. The injected supercritical CO2 (scCO2) flow and dissolution …

A 3–4D soil model represents a logical step forward from one‐dimensional soil columns
(1D), two‐dimensional soil maps (2D), and three‐dimensional soil volumes (3D) toward …

Natural porous media are generally heterogeneous and anisotropic. The structure of porous
media plays a vital role and is often the source of their heterogeneity and anisotropy. In …

Available methods to quantify the recharge of karst aquifers usually rely on spatially and
temporally aggregated precipitation measurements and simplified recharge models …

The unsaturated seepage field coupled with heavy rainfall-induced surface flow mainly
accounts for the slope instability. If the slope contains macropores, the coupled model and …

Fractures provide pathways for preferential flow, whereas porous rock acts as storage that
delays fluid propagation through matrix imbibition. These dual‐porosity mechanisms are …

A popular equation that is often employed to represent the relationship between the
pressure loss and the fluid flow in fluidized or packed granular beds is the Ergun equation …

The flow of water through a channel with a heterogeneous porous layer in its central core is
simulated using the method of Smoothed-Particle Hydrodynamics (SPH). Three different …

Many studies have shown that fracture networks can provide rapid pathways for water
infiltration and time‐dependent recharge in the vadose zone of consolidated fractured rock …