Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6344671 | Journal of Geochemical Exploration | 2014 | 17 Pages |
â¢Fluoride concentration occurs up to 13 mg/l in shallow alluvial aquifer.â¢Ion-exchange is the dominant in hydrogeochemical process.â¢Intercalated zeolitic clay within aquifer sand is the main source of Fâ.â¢Sorption and de-sorption mechanism of clay leads to mobilization of Fâ.
Groundwaters with high fluoride (Fâ) concentration up to 13.61 mg/L occur in some parts of the Quaternary alluvial aquifer of Birbhum district, West Bengal, India. The high Fâ groundwater zones are mainly located in the discharge areas of Dwarka river basin, especially in places where groundwater occurs at a depth of 24-30 m within alluvial sediments, consisting of micaceous sand, silt and clay. Soil depth samples were collected from the 3 bore holes drilled up to about 30 m depth for geochemical analysis. Total Fâ in the sedimentary material from the drilled holes measured about 400 to 450 mg/kg at deeper depth in CS1 and CS3 but no abnormal values found in CS2. XRD, XRF and total Fâ analyses of sediments from aquifer zone reveal that, the presence of intercalated zeolitic clay within the aquifer sand is the major source of Fâ in groundwater. Furthermore, geochemical investigations and laboratory analysis emphasize that sorption and de-sorption of intercalated zeolitic clay at different pH levels along with ion-exchange are the major mobilising factors for Fâ in pre- and post-monsoon seasons. Most of the groundwater having fast recharge component either from flowing canals or rainfall, contains relatively depleted δ18O content (â 5 to â 4â°). However, δ18O content has no correlation either with Clâ or Fâ that shows more than one contaminant sources.