7-Determination of aquifer recharge for varying river stages.

dc.contributor.author	Mishra, G. C.
dc.date.accessioned	2019-08-07T11:30:39Z
dc.date.available	2019-08-07T11:30:39Z
dc.date.issued	1987
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/3318
dc.description.abstract	A mathematical model has been developed for finding the exchange flow rate between a river and a multiaquifer system for varying river stages. The solution has been obtained by discretising the time parameter and using unit response function coefficients. The analytical solution is tractable for numerical calculation. It is found that the storage coefficient of the lower aquifer controls the recharge from the upper aquifer, besides the aquitard resistance.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Determination of aquifer recharge	en_US
dc.title	7-Determination of aquifer recharge for varying river stages.	en_US
dc.type	Technical Report	en_US