Skip to main content

Research Repository

Advanced Search

Behavior of aluminum, arsenic, and vanadium during the neutralization of red mud leachate by HCl, gypsum, or seawater

Burke, Ian T.; Peacock, Caroline L.; Lockwood, Cindy L.; Stewart, Douglas I.; Mortimer, Robert J. G.; Ward, Michael B.; Renforth, Philip; Gruiz, Katalin; Mayes, William M.

Authors

Ian T. Burke

Caroline L. Peacock

Cindy L. Lockwood

Douglas I. Stewart

Robert J. G. Mortimer

Michael B. Ward

Philip Renforth

Katalin Gruiz



Abstract

Red mud leachate (pH 13) collected from Ajka, Hungary is neutralized to < pH 10 by HCl, gypsum, or seawater addition. During acid neutralization >99% Al is removed from solution during the formation of an amorphous boehmite-like precipitate and dawsonite. Minor amounts of As (24%) are also removed from solution via surface adsorption of As onto the Al oxyhydroxides. Gypsum addition to red mud leachate results in the precipitation of calcite, both in experiments and in field samples recovered from rivers treated with gypsum after the October 2010 red mud spill. Calcite precipitation results in 86% Al and 81% As removal from solution, and both are nonexchangeable with 0.1 mol L–1 phosphate solution. Contrary to As associated with neoformed Al oxyhydroxides, EXAFS analysis of the calcite precipitates revealed only isolated arsenate tetrahedra with no evidence for surface adsorption or incorporation into the calcite structure, possibly as a result of very rapid As scavenging by the calcite precipitate. Seawater neutralization also resulted in carbonate precipitation, with >99% Al and 74% As removed from solution during the formation of a poorly ordered hydrotalcite phase and via surface adsorption to the neoformed precipitates, respectively. Half the bound As could be remobilized by phosphate addition, indicating that As was weakly bound, possibly in the hydrotalcite interlayer. Only 5–16% V was removed from solution during neutralization, demonstrating a lack of interaction with any of the neoformed precipitates. High V concentrations are therefore likely to be an intractable problem during the treatment of red mud leachates.

Citation

Burke, I. T., Peacock, C. L., Lockwood, C. L., Stewart, D. I., Mortimer, R. J. G., Ward, M. B., Renforth, P., Gruiz, K., & Mayes, W. M. (2013). Behavior of aluminum, arsenic, and vanadium during the neutralization of red mud leachate by HCl, gypsum, or seawater. Environmental Science and Technology, 47(12), 6527-6535. https://doi.org/10.1021/es4010834

Journal Article Type Article
Acceptance Date May 17, 2013
Online Publication Date Jun 5, 2013
Publication Date Jun 18, 2013
Deposit Date Apr 2, 2019
Journal Environmental Science and Technology
Print ISSN 0013-936X
Electronic ISSN 1520-5851
Publisher American Chemical Society
Peer Reviewed Peer Reviewed
Volume 47
Issue 12
Pages 6527-6535
DOI https://doi.org/10.1021/es4010834
Keywords Seawater; Anions; Calcite; Extended X-ray absorption fine structure; Inorganic carbon compounds
Public URL https://hull-repository.worktribe.com/output/1529665
Publisher URL https://pubs.acs.org/doi/10.1021/es4010834