Applied and Environmental Microbiology, January 1999, p. 175-180, Vol. 65, No. 1
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
School of Civil and Environmental Engineering,1 Section of Microbiology,2 and School of Chemical Engineering,3 Cornell University, Ithaca, New York 14853
Received 21 May 1998/Accepted 15 October 1998
Biogenic Mn oxides were produced by the bacterium Leptothrix
discophora SS-1 (= ATCC 3182) in a chemically defined
mineral salts medium, and the Pb binding and specific surface area of these oxides were characterized. Growth of SS-1 in the defined medium with pyruvate as a carbon and energy source required the addition of vitamin B12. Complete oxidation of Mn(II)
within 60 h required the addition of
0.1 µM FeSO4.
Pb adsorption isotherms were determined for the biogenic Mn oxides (and
associated cells with their extracellular polymer) and compared to the
Pb adsorption isotherms of cells and exopolymer alone, as well as to
abiotic Mn oxides. The Pb adsorption to cells and exopolymer with
biogenic Mn oxides (0.8 mmol of Mn per g) at pH 6.0 and 25°C was 2 orders of magnitude greater than the Pb adsorption to cells and
exopolymer alone (on a dry weight basis). The Pb adsorption to the
biogenic Mn oxide was two to five times greater than the Pb adsorption to a chemically precipitated abiotic Mn oxide and several orders of
magnitude greater than the Pb adsorption to two commercially available
crystalline MnO2 minerals. The N2
Brunauer-Emmet-Teller specific surface areas of the biogenic Mn oxide
and fresh Mn oxide precipitate (224 and 58 m2/g,
respectively) were significantly greater than those of the commercial
Mn oxide minerals (0.048 and 4.7 m2/g). The Pb adsorption
capacity of the biogenic Mn oxide also exceeded that of a chemically
precipitated colloidal hydrous Fe oxide under similar solution
conditions. These results show that amorphous biogenic Mn oxides
similar to those produced by SS-1 may play a significant role in the
control of trace metal phase distribution in aquatic systems.
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