H13L-1745
Biogeochemical Processes leading to release of As and Mn in the groundwaters of Murshidabad District of West Bengal, India

Monday, 14 December 2015
Poster Hall (Moscone South)
Saugata Datta, Kansas State University, Department of Geology, Manhattan, KS, United States
Abstract:
Elevated concentrations of both manganese (Mn) and arsenic (As) have been observed in the groundwaters of Murshidabad, in eastern India. Mn, a postulated neurotoxin is known to cause neuromuscular problems, inhibition of neurological development particularly in children. The health impacts from higher bioavailable proportions of As is well known in being a Class I carcinogen. The discovery of this additional contaminant in the already As afflicted regions of SE Asia poses serious implications for millions of inhabitants. The current study aims to address three objectives in understanding biogeochemical cycling of Mn and As in groundwaters: i) the occurrence and overall distribution (lateral and temporal) of groundwater Mn and As; ii) characterization of the dissolved organic matter and microbial content and the resultant effects that are imposed on dissolved As and Mn; and iii) the relationship between Mn, As, and various other inorganic constituents and their impact on the subsequent release of Mn, on top of As. A three year time series of chemical data for the dissolved constituents from six villages in Murshidabad will be presented. Hariharpara, Beldanga, Naoda villages contain reducing groundwaters (mean Mn: 0.93mg/L); Nabagram, Kandi, Khidirpore demonstrate oxidizing aquifers (Mn: 0.74mg/L). Eighty-three percent of the wells surveyed contain Mn levels that exceed the recommended WHO limit of 0.4 mg/L. Dissolved As within the same locations show a range from <10µg/L to ~4000 µg/L. DOC values demonstrate a positive correlation with Mn in reducing and a negative correlation in oxidizing environments. The reducing aquifers are also high in As and DOC, indicating that the microbially mediated reductive dissolution of As-sorbed onto Fe-Mn mineral phases is probable. Fluorescence analyses of dissolved OM, solidphase modeling of Mn speciation are being combined in this study for more insight into the mechanisms of Mn release and its relation if any to As release.