Groundwater with high geogenic arsenic (As) is extensively present in the Holocene alluvial aquifers of Ghazipur District in the middle Gangetic Plain, India. A shift in the climatic conditions, weathering of carbonate and silicate minerals, surface water interactions, ion exchange, redox processes, and anthropogenic activities are responsible for high concentrations of cations, anions and As in the groundwater.
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/arsenic-enrichment-groundwater-middle-gangetic-plain-ghazipur-district-uttar-pradesh
[2] http://admin.indiaenvironmentportal.org.in/category/author/manish-kumar
[3] http://admin.indiaenvironmentportal.org.in/category/author/pankaj-kumarb
[4] http://admin.indiaenvironmentportal.org.in/category/author/al-ramanathan-et-al
[5] http://admin.indiaenvironmentportal.org.in/category/journal/journal-geochemical-exploration
[6] http://admin.indiaenvironmentportal.org.in/category/thesaurus/groundwater-quality
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/arsenic
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/indo-gangetic-plains
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/ghazipur-d
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/uttar-pradesh
