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Applied and Environmental Microbiology, October 2005, p. 6308-6318, Vol. 71, No. 10
0099-2240/05/$08.00+0     doi:10.1128/AEM.71.10.6308-6318.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.

Microbiological and Geochemical Heterogeneity in an In Situ Uranium Bioremediation Field Site

Helen A. Vrionis,1* Robert T. Anderson,1 Irene Ortiz-Bernad,1 Kathleen R. O'Neill,1 Charles T. Resch,2 Aaron D. Peacock,3 Richard Dayvault,4 David C. White,3 Philip E. Long,2 and Derek R. Lovley1

Department of Microbiology, University of Massachusetts, Amherst, Massachusetts 01003,1 Pacific Northwest National Laboratory, Richland, Washington 99352,2 S. M. Stoller Corporation, Lafayette, Colorado 80026,4 Center for Biomarker Analysis, University of Tennessee, Knoxville, Tennessee 379323

Received 15 March 2005/ Accepted 30 April 2005

The geochemistry and microbiology of a uranium-contaminated subsurface environment that had undergone two seasons of acetate addition to stimulate microbial U(VI) reduction was examined. There were distinct horizontal and vertical geochemical gradients that could be attributed in large part to the manner in which acetate was distributed in the aquifer, with more reduction of Fe(III) and sulfate occurring at greater depths and closer to the point of acetate injection. Clone libraries of 16S rRNA genes derived from sediments and groundwater indicated an enrichment of sulfate-reducing bacteria in the order Desulfobacterales in sediment and groundwater samples. These samples were collected nearest the injection gallery where microbially reducible Fe(III) oxides were highly depleted, groundwater sulfate concentrations were low, and increases in acid volatile sulfide were observed in the sediment. Further down-gradient, metal-reducing conditions were present as indicated by intermediate Fe(II)/Fe(total) ratios, lower acid volatile sulfide values, and increased abundance of 16S rRNA gene sequences belonging to the dissimilatory Fe(III)- and U(VI)-reducing family Geobacteraceae. Maximal Fe(III) and U(VI) reduction correlated with maximal recovery of Geobacteraceae 16S rRNA gene sequences in both groundwater and sediment; however, the sites at which these maxima occurred were spatially separated within the aquifer. The substantial microbial and geochemical heterogeneity at this site demonstrates that attempts should be made to deliver acetate in a more uniform manner and that closely spaced sampling intervals, horizontally and vertically, in both sediment and groundwater are necessary in order to obtain a more in-depth understanding of microbial processes and the relative contribution of attached and planktonic populations to in situ uranium bioremediation.


* Corresponding author. Mailing address: Department of Microbiology, Morrill Science IVN, University of Massachusetts, Amherst, MA 01003. Phone: (413) 577-0217. Fax: (413) 545-1578. E-mail: vrionis{at}microbio.umass.edu.


Applied and Environmental Microbiology, October 2005, p. 6308-6318, Vol. 71, No. 10
0099-2240/05/$08.00+0     doi:10.1128/AEM.71.10.6308-6318.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.




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