4.4 Article

Influence of Fe2+-catalysed iron oxide recrystallization on metal cycling

Journal

BIOCHEMICAL SOCIETY TRANSACTIONS
Volume 40, Issue -, Pages 1191-1197

Publisher

PORTLAND PRESS LTD
DOI: 10.1042/BST20120161

Keywords

goethite; haematite; iron oxide; magnetite; metal cycling; recrystallization

Funding

  1. National Science Foundation (NSF) [EAR-1012037]
  2. Subsurface Science Scientific Focus Area (SFA) at Argonne National Laboratory (ANL) by the Subsurface Biogeochemical Research Program, Office of Biological and Environmental Research, Office of Science, U.S. Department of Energy (DOE) [DE-AC02-06CH11357]
  3. Division Of Chemistry
  4. Direct For Mathematical & Physical Scien [1012037] Funding Source: National Science Foundation

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Recent work has indicated that iron (oxyhydr-)oxides are capable of structurally incorporating and releasing metals and nutrients as a result of Fe2+-induced iron oxide recrystallization. In the present paper, we briefly review the current literature examining the mechanisms by which iron oxides recrystallize and summarize how recrystallization affects metal incorporation and release. We also provide new experimental evidence for the Fe2+-induced release of structural manganese from manganese-doped goethite. Currently, the exact mechanism(s) for Fe2+-induced recrystallization remain elusive, although they are likely to be both oxide- and metal-dependent. We conclude by discussing some future research directions for Fe2+-catalysed iron oxide recrystallization.

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