Geomicrobiology Journal · 2007 · 32 citations · 14 references
Natural SciencesChemistryMicrobiologyElemental AnalysisInorganic ChemistryMineralogyMetal SulfidesMicrobial Sulfur CyclingSulfide MineralogySulfide MineralsSulfur ChemistrySulfur CycleMetal Sulfide FormationMicrobial Sulfate ReductionNickel SulfidesSulfate ReductionSulfate-reducing BacteriaSulfate-reducing MicroorganismsSulfide PrecipitationX-ray Diffraction Analysis
The purpose of this study was to characterize Ni- and Zn-sulfides precipitated in sulfate-reducing bacterial cultures. Fe-free media containing 58 mM SO 4 2− were amended with Ni and Zn chloride followed by inoculation. Precipitates were sampled from cultures after two weeks of incubation at 22, 45, and 60 ° C. Abiotic controls were prepared by reacting bacteria-free liquid media with Na 2 S solutions under otherwise identical conditions. Precipitates were collected anaerobically, freeze-dried and analyzed by x-ray diffraction (XRD), scanning electron microscopy, and for total Ni, Zn, and S. In Ni-containing media, biogenic sulfide precipitates were mostly heazelwoodite (Ni 3 S 2 ), whereas abiotic precipitates were mixed heazelwoodite and vaesite (NiS 2 ). The biogenic Ni-precipitates were better crystalline than the corresponding abiotic samples. Sphalerite (ZnS) was identified by XRD in precipitates sampled from Zn-containing media. Scanning electron microscopy revealed disordered morphological features for the sulfides, which occurred mostly as aggregates of fine particles in biogenic samples, whereas abiotic precipitates contained more plate- and needle-like structures.
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