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The characteristics of the groundwater circulation were evaluated from variations in electrical resistivity and groundwater level.
Dual-screened groundwater circulation wells (GCWs) can be used to remove contaminant mass and to mix reagents in situ.
Continuous lowering of the level of groundwater circulation often produces tiers of passages stacked one on top of the other, and these need not be interconnected by an explorable cave.
Groundwater circulation in karst aquifers is characterized by short residence time and low water-rock interaction caused by high karstification processes in the study area.
Significant climate driven, periodic fluctuations in the power of runoff, stream flows and groundwater circulation were revealed that have not previously been documented.
The ratio rGW-LOCAL is sensitive to recharge conditions as well as topography and it could be used to compare controls on groundwater circulation within or between catchments.
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In order to investigate the origin of groundwater, its circulation patterns, and to understand the connectivity and compartmentalization of a karst system, a multi-tracer approach was used to describe the hydrogeology of the Lez karst system.
Chemical composition of geologic formations affects the hydrochemical characteristics of groundwater during their circulation in the subsurface (Elango et al. 2003).
This may be due to the enhanced circulation of groundwater in the shallow local groundwater system.
This may be due to the enhanced circulation of groundwater in the shallow, local groundwater system, relatively deficient in silica.
Hence, to capture the important mass and energy transfers correctly, which may affect regional precipitation and temperature dynamics5,6, lateral flow circulation of groundwater must be incorporated into the next generation of global models rather than assuming within-grid-cell hydrological closure of the water budget as is currently often assumed20,21,22.
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