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Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/7413
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dc.contributor.authorKrishan, Gopal-
dc.contributor.authorLapworth, D.J.-
dc.contributor.authorMacDonald, A.M.-
dc.contributor.authorRao, M.S.-
dc.date.accessioned2023-12-01T14:49:56Z-
dc.date.available2023-12-01T14:49:56Z-
dc.date.issued2023-
dc.identifier.citationJournal of Hydrology: Regional Studies Volume 50, December 2023en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/7413-
dc.description.abstractWater isotopes and specific electrical conductivity (SEC) are used in this paper to investigate groundwater recharge sources and processes in a catchment with a history of high groundwater abstraction for irrigation and canal irrigation. High frequency (every 10 days) samples for water stable isotope analysis (δ18O and δ2H) were sampled from a dense network of shallow (<50 m) and deep (>100 m) hand pumps and tube wells in Bist-Doab, northern Punjab between 2009 and 2014.en_US
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.subjectGroundwateren_US
dc.subjectRechargeen_US
dc.subjectSalinityen_US
dc.subjectNorth-west Indiaen_US
dc.subjectSecurityen_US
dc.titleGroundwater recharge sources and processes in northwest India: Evidence from high frequency water isotope observationsen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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