A riparian zone is an important element in a river-aquifer system, controlling water exchange
and other chemical and biological processes between a river and an aquifer. Complex …

A coupled unsaturated–saturated model for groundwater flow in a riparian zone is
established to evaluate the impacts of unsaturated zone on groundwater flow and aquifer …

Low-permeability aquitards are important sedimentary units that protect the underlying
confined aquifers from contamination by seawater and anthropogenic sources in coastal …

Rapidly rising river stages induced by flood events lead to considerable river water
infiltration into aquifers and carry surface‐borne solutes into hyporheic zones which are …

Deep learning models exhibit good interpolating ability, but their performance is often
hindered by the scarcity of data in groundwater problems. Analytical models (solutions) …

Hyporheic zone is an essential landscape element controlling the biogeochemical
processes and water exchange in river-aquifer system. Complex hyporheic flow patterns …

Natural hydrogeological settings may delineate wedge-shaped aquifers that are
sandwiched between streams, lakes or sea water bodies along arbitrary-oriented boundary …

In this study, new analytical solutions were developed for 2D and 3D steady-state water
seepage through dams with nonsymmetric boundary conditions. The nonsymmetric …

Different aspects of groundwater mound dynamics in triangular-shaped aquifers are
investigated analytically under spatially uniform recharge of time-varying rate. The aquifer …

Analytical solutions were derived for the variance, covariance, and spectrum of groundwater
level, h (x, t), in an unconfined aquifer described by a linearized Boussinesq equation, with …