The pumping has created what hydrologists call a " cone of depression " in the aquifer, which is much like the vortex in a drain.
12.
As a well is pumped, the cone of depression will extend out and will continue to expand in a radial fashion until a point of equilibrium occurs.
13.
In such cases, water from the lake or stream supplies water to the cone of depression and therefore the cone will not expand as far in this direction.
14.
A "'cone of depression "'occurs in an aquifer when groundwater is pumped from a artesian ), the cone of depression is a reduction in the pressure head surrounding the pumped well.
15.
A "'cone of depression "'occurs in an aquifer when groundwater is pumped from a artesian ), the cone of depression is a reduction in the pressure head surrounding the pumped well.
16.
Instead, a " cone of depression " forms : The water disappears across a wide area near the surface, tapering down to a small point by the base of the well.
17.
Conversely, if the cone of depression contacts a barrier, such as massive bedrock ridge, a clay body, or the edge of the aquifer, the cone of depression will decline to greater depths in order to supply water to the well.
18.
Conversely, if the cone of depression contacts a barrier, such as massive bedrock ridge, a clay body, or the edge of the aquifer, the cone of depression will decline to greater depths in order to supply water to the well.
19.
As water is pumped from a deep well, a hydraulic gradient is formed and water flows into the well forming a cone of depression around the well in which there is little or no water remaining in the pore spaces of the surrounding soil.
20.
When two cones of depression intersect one another, they tend to have a combined effect on mines and landfills where the goal is to lower water levels and pressures, wells often are placed close together in order to reduce head in the aquifer to the maximum amount.
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