7-Flowing Wells.

dc.contributor.author	Chandra, Satish
dc.contributor.author	Mishra, G. C.
dc.date.accessioned	2021-01-22T20:22:45Z
dc.date.available	2021-01-22T20:22:45Z
dc.date.issued	1992
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/5666
dc.description.abstract	Using discrete kernel approach an analytical solution has been obtained to determine temporal variation of discharge of a flowing well in a confined aquifer of finite areal extent. The quant ifi es of water that remain in the aquifer storage at any time after the onset of flow, which will be subsequently drained by the flowing well, have been quantified. Type curves have been prepared to enable determination of aquifer parameters. such- as: storage coefficient, transmissivity ,distance of the no flow boundary from the flowing well, and the initial hydraulic head.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Ground Water Quality	en_US
dc.subject	Wells	en_US
dc.title	7-Flowing Wells.	en_US
dc.type	Technical Report	en_US