Evaluation of groundwater quality with emphasis on fluoride concentration in Nalbari district, Assam, Northeast India

• Published in: Environmental earth sciences 2012-04, Vol.65 (7), p.2147-2159
• Main Authors: Sharma, Pallavi, Sarma, Hari Prasad, Mahanta, Chandan
• Format: Article
• Language: English
• Subjects: Anions; Biogeosciences; Cations; Chemical analysis; Drinking water; Earth and Environmental Science; Earth Sciences; Environmental Science and Engineering; Fluorides; Geochemistry; Geology; Groundwater; Groundwater irrigation; Hydrology/Water Resources; Irrigation water; Original Article; Salinity; Sodium; Soil types; Terrestrial Pollution; Water analysis; Water quality; Water sampling
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-011-1195-5

This study was carried out to analyze groundwater quality in selected villages of Nalbari district, Assam, India, where groundwater is the main source of drinking water. 40 groundwater samples collected from hand pumps and analyzed for pH, EC, TDS, Ca 2+ , Mg 2+ , Na + , K + , HCO 3 − , SO 4 2− , Cl − and F − . Chemical analysis of the groundwater showed that mean concentration of cations in (mg/L) is in the order Ca 2+  > Mg 2+  > Na +  > K + while for anions it is HCO 3 −  > Cl −  > SO 4 2−  > F − . Fluoride concentration was recorded in the range of 0.02–1.56 mg/L. As per the desirable and maximum permissible limits for fluoride in drinking water recommended by WHO and by Bureau of Indian Standards (BIS), which is 1.5 mg/L, the groundwater of about 97% of the samples were found to be suitable for drinking purpose. The suitability of the groundwater for irrigation purpose was investigated by some determining factors such as sodium adsorption ratio, soluble sodium percentage, Kelly’s ratio and electrical conductivity. The value of the sodium absorption ratio and electrical conductivity of the groundwater samples were plotted in the US Salinity laboratory diagram for irrigation water. Most of the groundwater samples fall in the field of C2S1 and C3S1 indicating medium to high salinity and low sodium water, which can be used for irrigation on almost all types of soil with little doubt of exchangeable sodium. The hydrochemical facies shows that the groundwater is Ca-HCO 3 type.