Aquifer Management using Isotopes

dc.contributor.author	Krishan, Gopal
dc.date.accessioned	2020-05-08T10:02:23Z
dc.date.available	2020-05-08T10:02:23Z
dc.date.issued	2019
dc.identifier.citation	Current World Environment,Vol. 14, No. (3) 2019, Pg. 349-350	en_US
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/4223
dc.description.abstract	Groundwater occurs in the saturated soil and rock below the water table in aquifers. Aquifer is a sub surface layer where pore spaces of water-bearing permeable rock, rock fractures, unconsolidated materials such as gravel, sand, or silt are completely filled with water under saturated conditions.	en_US
dc.language.iso	en	en_US
dc.publisher	Enviro Research Publishers	en_US
dc.subject	Isotopes	en_US
dc.subject	Aquifer management	en_US
dc.subject	Aquifer	en_US
dc.subject	Aquifer quality	en_US
dc.title	Aquifer Management using Isotopes	en_US
dc.type	Article	en_US