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In Situ Magnetite Formation and Long-Term Arsenic Immobilization under Advective Flow Conditions Jing Sun, Steven N Chillrud, Brian J. Mailloux, and Benjamin C. Bostick Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.6b02362 • Publication Date (Web): 17 Aug 2016 Downloaded from http://pubs.acs.org on August 17, 2016
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Environmental Science & Technology
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In Situ Magnetite Formation and Long-Term Arsenic Immobilization under
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Advective Flow Conditions.
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Jing Sun 1,2, Steven N. Chillrud 2, Brian J. Mailloux 3, and Benjamin C. Bostick *,2
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10027, USA
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Lamont-Doherty Earth Observatory, PO Box 1000, 61 Route 9W, Palisades, NY 10964, USA
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Department of Environmental Sciences, Barnard College, 3009 Broadway, New York, NY 10027, USA
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Corresponding author: Benjamin C. Bostick
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Phone: (+1) 845-365-8659; Fax: (+1) 845-365-8155; E-mail:
[email protected] Department of Earth and Environmental Sciences, Columbia University, Mail Code 5505, New York, NY
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1 ACS Paragon Plus Environment
Environmental Science & Technology
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ABSTRACT
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In situ precipitation of magnetite and other minerals potentially sequesters dissolved arsenic (As)
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in contaminated aquifers. This study examines As retention and transport in aquifer sediments
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using a multi-stage column experiment in which magnetite and other minerals formed from
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added nitrate and ferrous iron (Fe). Sediments were collected from the Dover Municipal Landfill
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Superfund site. Prior to nitrate-Fe(II) addition, As was not effectively retained within the
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sediments in the column. The combination of nitrate (10 mM) and Fe(II) (4 mM), resulted in
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mineral precipitation and rapidly decreased effluent As concentrations to
