Determination of unsteady radius of influence during pumping from confined aquifers
Authors:
Abstract
In case of pumping from a confined aquifer at a dynamic water level located above its roof, during the period of unsteady water inflow to the borehole, the pumped water is obtained at the expense of “elastic storage” (an aquifer not communicating with other aquifers or surface water bodies within the area of the cone of depression). “Elastic storage”, according to V.N. Shchelkachev, is the volume of water displaced into the well during elastic expansion of water and water-bearing rocks due to pressure drop in the area of the cone of depression.
Область исследования:
(Archived) Hydrogeology, engineering geology
Funding:
None
References
- Shchelkachev V. N. Development of oil-water-bearing strata under elastic mode. Gostoptekhizdat, 1959.
- Shchelkachev V. N., Lapuk B. B. Underground Hydraulics. Gostoptekhizdat, 1949.
- Kerkis E. E. Determination of the Radius of Influence in the Calculation of Water Inflows. Ugletekhizdat, 1955.
Similar articles
On the porosity of rocks of the Rhaetian-Liassic sequence of the Chelyabinsk Basin
1962 N. P. Krasilnikov
Physical and mechanical properties of clayey rocks of the Upper Pestrotsvetnaya Formation of the main Devonian field of the Russian Platform
1962 V. D. Lomtazde