Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3697
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dc.contributor.authorJacks, G.-
dc.contributor.authorBhattacharya, Prosun-
dc.contributor.authorAhmed, K. Matin-
dc.contributor.authorChatterjee, D.-
dc.date.accessioned2019-10-10T10:37:01Z-
dc.date.available2019-10-10T10:37:01Z-
dc.date.issued2000-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3697-
dc.description.abstractWidespread arsenic contamination in groundwater in the Bengal Delta seems to be largely natural depending on reducing conditions in the aquifers. Reduction of ferric hydroxides with adsorbed arsenic species occurs at intermediate depth. In situ remediation might be achieved by artificial recharge stabilising the ferric hydroxides. It might however be problematic to keep the aquifer oxic. Sulphate levels are generally low and sulphur deficiency for crops common. The low sulphate levels favour methane fermentation over sulphate reduction. Application of gypsum to the surface soils might favour immobilisation of the arsenic in the form of sulphides.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectArsenic in groundwateren_US
dc.subjectBengal Deltaen_US
dc.titleTheme 3-8-Arsenic in groundwater and redox conditions in the Bengal delta – Possible in situ remediationen_US
dc.typeTechnical Reporten_US
Appears in Collections:ICIWRM-2000, Proceedings of International Conference on Integrated Water Resources Management for Sustainable Development, 19-21 December, 2000, New Delhi, India Vol.-I



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