Well hydraulics is a discipline to understand the process of flow to the well in an aquifer
which is regarded as a source of groundwater. A variety of analytical and numerical models …

In this paper, we investigated the tide-induced seawater–groundwater circulation in shallow
beach aquifers using the finite element model MARUN. The numerical solutions were …

The tidal influence on groundwater hydrodynamics, salt-water intrusion and submarine
groundwater discharge from coastal/estuarine aquifers is poorly quantified for systems with …

The responses of the fresh-saline water interface (FSI) and the groundwater level (GWL) to
the Mediterranean Sea tide were monitored in the coastal aquifer of Israel, modeled …

Above a shallow unconfined aquifer, a considerable amount of water is stored in the vadose
zone. Through water exchange with the underlying unconfined aquifer, the vadose zone …

Abstract Study region River Neretva coastal aquifer system located in the south eastern part
of Croatia. Study focus The study is focused to determination of the seasonal and non …

Intertidal zones are spatially complex and temporally dynamic environments. Coastal
groundwater discharge, including submarine groundwater discharge, may provide …

Observations of horizontal and vertical variations in piezometric head in a homogeneous,
laboratory aquifer are presented and discussed. The observed fluctuations are induced by a …

A comparative study concerning dynamic, local, and zero inertia variants of volume-
averaged depth-integrated porous shallow water equations has been presented. The first …

This study examines effects of tides on fluctuations of the fresh-saline water interface and the
groundwater level in unconfined coastal aquifers using a two-dimensional numerical model …