U.S. Department of Energy Office of Biological and Environmental Research

BER Research Highlights


Potential for Reoxidation of Iron-Chromium Precipitates by Manganese Oxide
Published: October 02, 2015
Posted: January 12, 2016

Abiotic reduction of Cr(VI) by FeS and reduced nontronite led to precipitates that released significant Cr(VI) when exposed to birnessite. Figure reproduced from Environ. Sci.: Processes Impacts 17 (2016), 1930–1940 (DOI: 10.1039/C5EM00286A) with permission from the Royal Society of Chemistry.

Reductive immobilization of hexavalent chromium (Cr(VI)), often forming Fe-Cr precipitates, is a frequent remediation alternative, yet the relationship between the conditions of precipitate formation, the structural and chemical properties of the precipitates, and the rate and extent of precipitate oxidation by Mn oxides is needed. This study provided a systematic investigation of the rates of Cr(VI) reduction by both abiotic minerals and a chromium reducing bacterium, the properties of the resulting Fe-Cr precipitates, and the susceptibility for reoxidation and remobilization of Cr(VI) upon precipitate exposure to the manganese oxide birnessite.

The properties of the resulting Fe-Cr solids and their behavior upon exposure to birnessite differed significantly. In microcosms where Cr(VI) was reduced by Desulfovibrio vulgaris strain RCH1, and where hematite or Al-goethite were present as iron sources, there was significant initial loss of Cr(VI) in a pattern consistent with adsorption, and significant Cr(VI) was found in the resulting solids. The solid formed when Cr(VI) was reduced by FeS contained a high proportion of Cr(III) and was poorly crystalline. Reaction between birnessite and the abiotically formed Cr(III) solids led to production of significant dissolved Cr(VI) compared to the no-birnessite controls. This pattern was not observed in the solids generated by microbial Cr(VI) reduction, and could be due to re-reduction of any Cr(VI) generated upon oxidation by birnessite via active bacteria or microbial enzymes.

The results of this study suggest that Fe-Cr precipitates formed in groundwater remediation may remain stable only in the presence of active anaerobic microbial reduction. If exposed to environmentally common Mn oxides such as birnessite in the absence of microbial activity, there is the potential for rapid (re)formation of dissolved Cr(VI) above regulatory levels.

Citation:
Butler, E. C., Chen, L., Hansel, C. M., Krumholz, L. R., Elwood Madden, A. S., Lan, Y. (2015), Biological versus mineralogical chromium reduction: Potential for reoxidation by manganese oxide, Environ. Sci.: Processes Impacts 17, 1930-1940, DOI: 10.1039/C5EM00286A.

Contact: Paul E. Bayer, SC-23.1, (301) 903-5324
Topic Areas:

  • Research Area: Subsurface Biogeochemical Research

Division: SC-23.1 Climate and Environmental Sciences Division, BER

 

BER supports basic research and scientific user facilities to advance DOE missions in energy and environment. More about BER

Recent Highlights

Aug 24, 2019
New Approach for Studying How Microbes Influence Their Environment
A diverse group of scientists suggests a common framework and targeting of known microbial processes [more...]

Aug 08, 2019
Nutrient-Hungry Peatland Microbes Reduce Carbon Loss Under Warmer Conditions
Enzyme production in peatlands reduces carbon lost to respiration under future high temperatures. [more...]

Aug 05, 2019
Amazon Forest Response to CO2 Fertilization Dependent on Plant Phosphorus Acquisition
AmazonFACE Model Intercomparison. The Science Plant growth is dependent on the availabi [more...]

Jul 29, 2019
A Slippery Slope: Soil Carbon Destabilization
Carbon gain or loss depends on the balance between competing biological, chemical, and physical reac [more...]

Jul 15, 2019
Field Evaluation of Gas Analyzers for Measuring Ecosystem Fluxes
How gas analyzer type and correction method impact measured fluxes. The Science A side- [more...]

List all highlights (possible long download time)