Unsteady flow to a large diameter well in a finite aquifers

dc.contributor.author	Mishra, G.C.
dc.contributor.author	Chachadi, A.G.
dc.date.accessioned	2015-06-03T06:47:03Z
dc.date.available	2015-06-03T06:47:03Z
dc.date.issued	1995
dc.identifier.citation	ISH Journal of Hydraulic Engineering. 1(2); 1995; 72-83.	en_US
dc.identifier.uri	http://dx.doi.org/10.1080/09715010.1995.10514575
dc.identifier.uri	http://irgu.unigoa.ac.in/drs/handle/unigoa/758
dc.description.abstract	Using the analytical solution derived by Muskat and Kuiper for unsteady flow to a well with negligible storage in a finite confined aquifer, an analytical solution for unsteady flow to a large-diameter well in a finite confined aquifer during pumping and recovery is obtained. Existence of a barrier boundary at a finite distance from the well has little influence on contribution of the well storage to pumping. The barrier boundary affects drawdown significantly. Well storage is not completely recovered in finite aquifer and there is a permanent drawdown in the initial piezometric surface consequent to an event of pumping.
dc.publisher	Taylor and Francis	en_US
dc.subject	Earth Science	en_US
dc.title	Unsteady flow to a large diameter well in a finite aquifers	en_US
dc.type	Journal article	en_US
dc.identifier.impf	y