dc.contributorUniversidade Estadual Paulista (UNESP)
dc.creatorGarcia, O.
dc.creatorBigham, J. M.
dc.creatorTuovinen, O. H.
dc.date2014-05-20T15:25:26Z
dc.date2016-10-25T17:59:54Z
dc.date2014-05-20T15:25:26Z
dc.date2016-10-25T17:59:54Z
dc.date1997-01-01
dc.date.accessioned2017-04-05T23:52:20Z
dc.date.available2017-04-05T23:52:20Z
dc.identifierRevista de Microbiologia. São Paulo: Soc Brasileira Microbiologia, v. 28, p. 95-100, 1997.
dc.identifier0001-3714
dc.identifierhttp://hdl.handle.net/11449/35858
dc.identifierhttp://acervodigital.unesp.br/handle/11449/35858
dc.identifierWOS:000168676300016
dc.identifierhttp://www.scielo.br/scielo.php?script=sci_issues&pid=0001-3714&lng=en&nrm=iso
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/879489
dc.descriptionSolution- and solid-phase changes associated with galena (PbS) and sphalerite (ZnS) oxidation by T. ferrooxidans and T. thiooxidans, were determined. In experiments with galena, anglesite (PbSO4) was detected as a solid-phase product in biotic and abiotic experiments. In T. ferrooxidans cultures supplemented with FeSO4, jarosite [MFe3 (SO4)(2) (OH)(6)] was also detected as a new solid phase product, whereas SO was not detected in the residues. In sphalerite experiments, minor amounts of SO accumulated in FeSO4-amended sphalerite media with or without T. ferrooxidans or T. thiooxidans. Jarosite was only detected in T. ferrooxidans culture with FeSO4. By comparison with T. thiooxidans, T. ferrooxidans was more efficient in the oxidation of galena and sphalerite.
dc.languageeng
dc.publisherSoc Brasileira Microbiologia
dc.relationRevista de Microbiologia
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectThiobacillus ferrooxidans
dc.subjectThiobacillus thiooxidans
dc.subjectmineral sulfides
dc.titleOxidative dissolution of research-grade minerals by Thiobacillus ferrooxidans and Thiobacillus thiooxidans
dc.typeOtro


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