Published June 2019 | Version v1
Journal article

Microbial reductive transformation of iron-rich tailings in a column reactor and its environmental implications to arsenic reactive transport in mining tailings

  • 1. Key Laboratory of Surficial Geochemistry of Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210046 (China)
  • 2. Earth Sciences Department, Dartmouth College, HB6105 Fairchild Hall, Hanover, NH 03755 (United States)
  • 3. State Key Laboratory for Deposits research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210046 (China)

Description

Highlights: • Advective flow with reductive bacteria in tailings induces Fe-minerals transformation and As transport. • Microbial iron reduction decomposes Fe3+ minerals in oxidized tailings and releases Fe2+ ions. • Jarosite is decomposed while other iron oxides are newly formed in reaction column. • Reactive transport model agrees with lab results of As release, transport and immobilization. -- Abstract: The evolution of iron minerals under buried conditions is one of the most important processes controlling the mineral composition and heavy metal transportation in sediments. Microbial-mediated reduction plays a critical role in iron mineral transformation in natural environment. This study examined the transformation pathways of iron minerals mediated by bacteria and the changes of associated arsenic species in iron-rich mine tailings. Static and column reactions were designed to monitor variations of minerals and released iron and arsenic, a reactive transport model was simulated to support laboratory results. Laboratory experiments showed that major ferric minerals were preferentially dissolved and reduced by dissimilatory iron-reducing bacteria. The released Fe3+ in fluid promoted oxidative dissolution of pyrite and arsenopyrite, and precipitation of oxides and carbonates. The arsenic released to fluid was inferred to be immobilized by both pristine ferrihydrite and newly formed hydrous ferric oxides via surface complexation. The reaction system maintained a steady-state of iron mineral transformation and arsenic (im)mobilization. In the latter stage of column reactor experiments, continuous reaction and removal of dissolved Fe3+ and Fe2+ destabilized the state, leading to arsenic re-location and eventually rising concentration in fluid. The findings implicate that microbial-mediated iron mineral evolution remarkably influence the natural mineral assemblages and the fate of contaminant transport in the environment, and that deposition of iron oxides is essential in environmental protection and pollution recovery.

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2019.03.285;
PII
S004896971931277X;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
670
Journal Page Range
p. 1008-1018
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2019 Published by Elsevier B.V.