Assessment of arsenic exposure from groundwater and rice in Bengal Delta Region, West Bengal, India

• Published in: Water research (Oxford) 2010-11, Vol.44 (19), p.5803-5812
• Main Authors: Chatterjee, Debashis, Halder, Dipti, Majumder, Santanu, Biswas, Ashis, Nath, Bibhash, Bhattacharya, Prosun, Bhowmick, Subhamoy, Mukherjee-Goswami, Aishwarya, Saha, Debasree, Hazra, Rasmani, Maity, Palash B., Chatterjee, Debankur, Mukherjee, Abhijit, Bundschuh, Jochen
• Format: Article
• Language: English
• Subjects: Aquifers; Arsenic; Arsenic - analysis; Arsenic - toxicity; Arsenic exposure; Assessments; Body Mass Index; Brackish; Chromatography, Ion Exchange; Civil engineering and architecture; Environmental engineering; Environmental Exposure - statistics & numerical data; Environmental Monitoring - statistics & numerical data; Fe Cycling; Fresh Water - chemistry; Groundwater; Habits; Health; Health Knowledge, Attitudes, Practice; Human body; Humans; Hydrochemistry; India; Interviews as Topic; Miljöteknik; Oryza - chemistry; Oryza sativa; Other technology; Redox chemistry; Rice; Risk assessment; Samhällsbyggnadsteknik och arkitektur; Spectrophotometry, Atomic; Surveys and Questionnaires; TECHNOLOGY; TEKNIKVETENSKAP; Vattenteknik; Water engineering; Water Pollutants, Chemical - analysis; Water Pollutants, Chemical - toxicity; Water quality; Övriga teknikvetenskaper
• ISSN: 0043-1354; 1879-2448; 1879-2448
• DOI: 10.1016/j.watres.2010.04.007

Arsenic (As) induced identifiable health outcomes are now spreading across Indian subcontinent with continuous discovery of high As concentrations in groundwater. This study deals with groundwater hydrochemistry vis-à-vis As exposure assessment among rural population in Chakdaha block, West Bengal, India. The water quality survey reveals that 96% of the tubewells exceed WHO guideline value (10 μg/L of As). The groundwaters are generally anoxic (−283 to −22 mV) with circum-neutral pH (6.3 to 7.8). The hydrochemistry is dominated by HCO 3 − (208 to 440 mg/L), Ca 2+ (79 to 178 mg/L) and Mg 2+ (17 to 45 mg/L) ions along with high concentrations of As T (As total, below detection limit to 0.29 mg/L), Fe T (Fe total, 1.2 to 16 mg/L), and Fe(II) (0.74 to 16 mg/L). The result demonstrates that Fe(II)–Fe(III) cycling is the dominant process for the release of As from aquifer sediments to groundwater (and vice versa), which is mainly controlled by the local biogeochemical conditions. The exposure scenario reveals that the consumption of groundwater and rice are the major pathways of As accumulation in human body, which is explained by the dietary habit of the surveyed population. Finally, regular awareness campaign is essential as part of the management and prevention of health outcomes.