Spatial and temporal distribution of arsenic in groundwater of the Brahmaputra River floodplains in Assam, India

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[1] Medhi, Smitakshi
[2] Choudhury, Runti
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Biogeochemistry - Chemical detection - Chlorine compounds - Groundwater geochemistry - Hydrochemistry - Magnesium alloys - Precipitation (chemical) - Recharging (underground waters) - Surface tension;
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10.1016/j.gsd.2024.101400
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摘要
The present study focuses on spatial and seasonal distribution of arsenic (As) along with the solute chemistry and hydrochemical evolution of groundwater in the southern bank of Brahmaputra floodplains in Assam, India. A total of 100 groundwater samples were collected from shallow aquifers (2+, Na+, K+, Mg2+ Cl−, HCO3−, NO3−, SO42−, Fe, Mn and As to interpret the hydrochemistry and groundwater evolution in the study area. Broadly three zones were delineated based on As distribution in the region viz; zone 1 as high As zone, areas adjacent to the foothills of Naga hills,(ranged from below detection level (bdl) to 531 μg/l, mean:93.91 μg/l). Zone 2 is demarcated as low arsenic zone, near the Brahmaputra River, where As concentration was mostly 3 as a primary water type during pre-monsoon, while Ca-Mg-HCO3 type during post monsoon.Groundwater is undersaturated with respect to As phases such as Arsenolite and As2O5 specifying that As is in dissolved form in the groundwater. The groundwater is supersaturated with calcite (CaCO3) and Dolomite (MgCa(CO3)2and Fe(III) (Oxyhyroxide). The stable isotopes (δ18O and δ2H) of groundwater suggest that precipitation is primarily recharging the groundwater with some influence of evaporation. The results of the study will contribute to a deeper understanding of the arsenic distribution dynamics in the Brahmaputra Floodplains along with facilitating evidence-based decision making aimed at providing arsenic safe drinking water to the affected communities. © 2024 Elsevier B.V.
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