Search results
A confined aquifer is an aquifer below the land surface that is saturated with water. Layers of impermeable material are both above and below the aquifer, causing it to be under pressure so that when the aquifer is penetrated by a well, the water will rise above the top of the aquifer.
A confined aquifer is an aquifer that occurs beneath an aquitard which is often referred to as a confining bed. In a confined aquifer, the water level in tightly cased wells rises above the top elevation of the aquifer.
1. Confined aquifers with upper impermeable layers where recharge only occurs from precipitation where the water-bearing formations outcrop at land surface. 2. Unconfined (phreatic) aquifers in wet regions where rainfall is high and evapotranspiration is low.
Confined aquifers are aquifers that are overlain by a confining layer, often made up of clay. The confining layer might offer some protection from surface contamination.
Oct 16, 2019 · Groundwater in aquifers between layers of poorly permeable rock, such as clay or shale, may be confined under pressure. If such a confined aquifer is tapped by a well, water will rise above the top of the aquifer and may even flow from the well onto the land surface.
Apr 24, 2024 · An aquifer where there is a lower permeability material between the aquifer and the ground surface is known as a confined aquifer, and the aquitard separating ground surface and the aquifer is known as the confining layer.
Confined Aquifer Storativity The storativity of a confined aquifer is defined as the volume of water released from, or added to, storage per unit change in head normal to the surface, per unit area. This is the same definition as for unconfined aquifers.
