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Considerations for conducting incubations to study the mechanisms of As release in reducing groundwater aquifers
Authors:Kathleen A Radloff  Anya R Manning  Brian Mailloux  Yan Zheng  M Moshiur Rahman  M Rezaul Huq  Kazi M Ahmed  Alexander van Geen
Institution:1. Department of Earth and Environmental Engineering, Columbia University, New York, NY 10027, USA;2. Barnard College, Columbia University, New York, NY 10027, USA;3. Queens College, City University of New York, Flushing, NY 11367, USA;4. Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA;5. Department of Geology, University of Dhaka, Dhaka, Bangladesh
Abstract:Microbial Fe reduction is widely believed to be the primary mechanism of As release from aquifer sands in Bangladesh, but alternative explanations have been proposed. Long-term incubation studies using natural aquifer material are one way to address such divergent views. This study addresses two issues related to this approach: (1) the need for suitable abiotic controls and (2) the spatial variability of the composition of aquifer sands. Four sterilization techniques were examined using orange-colored Pleistocene sediment from Bangladesh and artificial groundwater over 8 months. Acetate (10 mM) was added to sacrificial vials before sterilization using either (1) 25 kGy of gamma irradiation, (2) three 1-h autoclave cycles, (3) a single addition of an antibiotic mixture at 1× or (4) 10× the typical dose, and (5) a 10 mM addition of azide. The effectiveness of sterilization was evaluated using two indicators of microbial Fe reduction, changes in diffuse spectral reflectance and leachable Fe(II)/Fe ratios, as well as changes in P-extractable As concentrations in the solid phase. A low dose of antibiotics was ineffective after 70 days, whereas autoclaving significantly altered groundwater composition. Gamma irradiation, a high dose of antibiotics, and azide were effective for the duration of the experiment.
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