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Radon variability in groundwater from the lesser Himalayas to the gangetic alluvial plain, with hydrogeochemical and isotopic insights from Tehri Garhwal

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dc.contributor.author Krishan, Gopal
dc.contributor.author Sakthivel, V.
dc.contributor.author Rao, M.S.
dc.contributor.author Khobragade, S.D.
dc.date.accessioned 2026-11-11T07:18:26Z
dc.date.available 2026-11-11T07:18:26Z
dc.date.issued 2026
dc.identifier.citation Journal of Radioanalytical and nuclear chemistry en_US
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/8063
dc.description.abstract Groundwater radon (222Rn) poses radiological risks in Himalayan regions dominated by fractured crystalline aquifers. This study evaluates radon variability in groundwater from Tehri Garhwal (Lesser Himalayas) and compares it with previously published groundwater data from 27 sites (post-monsoon 2022) in the Siwalik foothills (Dehradun) and Gangetic alluvial plains (Haridwar). In the present study, ten groundwater samples from Tehri Garhwal were analyzed for radon, while hydro chemical and stable isotope (δ18O and δD) analyses were conducted on 13 water samples, including the ten analyzed for radon. Radon concentrations ranged from 2 to 43 Bq L⁻1, with 70% exceeding the recommended drinking-water guideline . en_US
dc.language.iso en en_US
dc.publisher Springer en_US
dc.subject Radon en_US
dc.subject Lesser Himalayas en_US
dc.subject Public health implications en_US
dc.subject Post-monsoon en_US
dc.subject Hydrogeochemistry en_US
dc.subject Groundwater recharge sources en_US
dc.title Radon variability in groundwater from the lesser Himalayas to the gangetic alluvial plain, with hydrogeochemical and isotopic insights from Tehri Garhwal en_US
dc.type Article en_US


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