1. NIH Digital Repository
  2. Conference Proceedings
  3. National Seminar/Workshop
  4. Proceedings of the Seminar on Ground Water Hydrology, 17-18 July 1992 at New Delhi, Vol-I
Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/5666
Full metadata record
DC FieldValueLanguage
dc.contributor.authorChandra, Satish-
dc.contributor.authorMishra, G. C.-
dc.date.accessioned2021-01-22T20:22:45Z-
dc.date.available2021-01-22T20:22:45Z-
dc.date.issued1992-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/5666-
dc.description.abstractUsing 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.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectGround Water Qualityen_US
dc.subjectWellsen_US
dc.title7-Flowing Wells.en_US
dc.typeTechnical Reporten_US
Appears in Collections:Proceedings of the Seminar on Ground Water Hydrology, 17-18 July 1992 at New Delhi, Vol-I

Files in This Item:
File Description SizeFormat 
7-Flowing Wells..pdf2.33 MBAdobe PDFView/Open
Show simple item record


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.