TR-19 : Recharge from large depression storage

dc.contributor.author	Chachadi, A. G.
dc.contributor.author	Mishra, G. C.
dc.date.accessioned	2019-02-28T06:47:15Z
dc.date.available	2019-02-28T06:47:15Z
dc.date.issued	1985
dc.identifier.uri	http://117.252.14.250:8080/xmlui/handle/123456789/440
dc.description.abstract	The duration of the pumping test is largely influenced by the discharge rate, radial distances of the observation points, aquifer parameters and boundary conditions. Plots have been presented for determining the time during which the initial disturbances persist during a pumping test. An equation has been suggested to compute the travel time of the radius of influence when a pumping test is conducted near a recharge boundary. Based on the actual pumping test data certain guidelines and index drawdowns have been provided which would help in deciding the maximum duration of pumping in a confined aquifer for reliable estimation of aquifer properties.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.relation.ispartofseries	;TN-19
dc.subject	Test pumping	en_US
dc.subject	Test pumping- duration	en_US
dc.title	TR-19 : Recharge from large depression storage	en_US
dc.type	Technical Report	en_US