Bei**g is an international metropolis, where over-exploration of water resource makes land
subsidence becoming more and more serious. The related problems cannot be avoided in …

In the mid-seventies, a new area of research has emerged in subsurface hydrology, namely
sto chastic modeling of flow and transport. This development has been motivated by the …

Most large‐scale flow and transport simulations for geologic carbon sequestration (GCS)
applications are carried out using simulators that solve flow equations arising from Darcy's …

Subsurface flow from a hillslope can be described by hydraulic groundwater theory, as
formulated by the Boussinesq equation. Solution of its linear version brings out some of the …

The relationship between base flow recession characteristics in steep watersheds and
geomorphologic and soil parameters is investigated. The formulation for the groundwater …

Modeling hydrological processes in certain peats requires a detailed understanding of short-
term changes in soil volume and it's influence on the system's hydraulic properties. A study …

A Laplace transform solution is presented for flow to a well in a homogeneous, water‐table
aquifer with noninstanta‐neous drainage of water from the zone above the water table. The …

The Boussinesq equation describes aquifer movement when capillarity effects are
unimportant. A simple correction term to the equation is proposed here to take those effects …

Macroscopic differential equations of mass and momentum balance for two immiscible fluids
in a deformable porous medium are derived in an Eulerian framework using the continuum …

The pressure field inside a porous bed induced by the passage of an Internal Solitary Wave
(ISW) of depression is examined using high‐accuracy numerical simulations. The velocity …