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Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/4223
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dc.contributor.authorKrishan, Gopal-
dc.date.accessioned2020-05-08T10:02:23Z-
dc.date.available2020-05-08T10:02:23Z-
dc.date.issued2019-
dc.identifier.citationCurrent World Environment,Vol. 14, No. (3) 2019, Pg. 349-350en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/4223-
dc.description.abstractGroundwater 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.isoenen_US
dc.publisherEnviro Research Publishersen_US
dc.subjectIsotopesen_US
dc.subjectAquifer managementen_US
dc.subjectAquiferen_US
dc.subjectAquifer qualityen_US
dc.titleAquifer Management using Isotopesen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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