Interactions between Microbial Iron Reduction and Metal Geochemistry:  Effect of Redox Cycling on Transition Metal Speciation in Iron Bearing Sediments

• Published in: Environmental science & technology Vol. 40; no. 6; pp. 1884 - 1891
• Main Authors: Cooper, D. Craig, Picardal, Flynn F, Coby, Aaron J
• Format: Journal Article
• Language: English
• Published: Washington, DC American Chemical Society 15-03-2006
• Subjects: AIR; Bacteria; BEARINGS; Contaminated sediments; CONTAMINATION; COORDINATION NUMBER; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Exact sciences and technology; Ferric Compounds - chemistry; GEOCHEMISTRY; Geologic Sediments - analysis; Geologic Sediments - chemistry; GOETHITE; Hydrochloric Acid - chemistry; IRON; Iron - chemistry; Iron - metabolism; Iron Compounds - chemistry; MATERIALS SCIENCE, 58 - GEOSCIENCES; metal; Metals; Metals, Heavy - analysis; Metals, Heavy - chemistry; microbial; Minerals; MIXTURES; OXIDATION; Oxidation-Reduction; Pollution, environment geology; redox cycling; SEDIMENTS; Soil Microbiology; Solubility; TRANSITION ELEMENTS; Zinc - analysis; Zinc - chemistry; experimental studies; trace metals; oxides; ferric iron; heavy metals; ferrous iron; metals; pollution; speciation; goethite; hydroxides; chemical reduction; ferrihydrite; microorganisms; iron; biogenic effects; sediments
• ISSN: 0013-936X; 1520-5851
• DOI: 10.1021/es051778t

Microbial iron reduction is an important biogeochemical process that can affect metal geochemistry in sediments through direct and indirect mechanisms. With respect to Fe(III) (hydr)oxides bearing sorbed divalent metals, recent reports have indicated that (1) microbial reduction of goethite/ferrihydrite mixtures preferentially removes ferrihydrite, (2) this process can incorporate previously sorbed Zn(II) into an authigenic crystalline phase that is insoluble in 0.5 M HCl, (3) this new phase is probably goethite, and (4) the presence of nonreducible minerals can inhibit this transformation. This study demonstrates that a range of sorbed transition metals can be selectively sequestered into a 0.5 M HCl insoluble phase and that the process can be stimulated through sequential steps of microbial iron reduction and air oxidation. Microbial reduction experiments with divalent Cd, Co, Mn, Ni, Pb, and Zn indicate that all metals save Mn experienced some sequestration, with the degree of metal incorporation into the 0.5 M HCl insoluble phase correlating positively with crystalline ionic radius at coordination number = 6. Redox cycling experiments with Zn adsorbed to synthetic goethite/ferrihydrite or iron-bearing natural sediments indicate that redox cycling from iron reducing to iron oxidizing conditions sequesters more Zn within authigenic minerals than microbial iron reduction alone. In addition, the process is more effective in goethite/ferrihydrite mixtures than in iron-bearing natural sediments. Microbial reduction alone resulted in a ∼3× increase in 0.5 M HCl insoluble Zn and increased aqueous Zn (Zn-aq) in goethite/ferrihydrite, but did not significantly affect Zn speciation in natural sediments. Redox cycling enhanced the Zn sequestration by ∼12% in both goethite/ferrihydrite and natural sediments and reduced Zn-aq to levels equal to the uninoculated control in goethite/ferrihydrite and less than the uninoculated control in natural sediments. These data suggest that in situ redox cycling may serve as an effective method for mitigating divalent metal contamination in subsurface environments.