| Reference Type | Journal (article/letter/editorial) |
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| Title | Arsenopyrite: a spectroscopic investigation of altered surfaces |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Richardson, S. | Author |
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| Vaughan, D. J. | Author |
| Year | 1989 (April) | Volume | 53 |
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| Issue | 370 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_53/53-370-223.pdf+ |
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| DOI | doi:10.1180/minmag.1989.053.370.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 1495 | Long-form Identifier | mindat:1:5:1495:7 |
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| GUID | 0 |
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| Full Reference | Richardson, S., Vaughan, D. J. (1989) Arsenopyrite: a spectroscopic investigation of altered surfaces. Mineralogical Magazine, 53 (370) 223-229 doi:10.1180/minmag.1989.053.370.09 |
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| Plain Text | Richardson, S., Vaughan, D. J. (1989) Arsenopyrite: a spectroscopic investigation of altered surfaces. Mineralogical Magazine, 53 (370) 223-229 doi:10.1180/minmag.1989.053.370.09 |
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| In | (1989, April) Mineralogical Magazine Vol. 53 (370) Mineralogical Society |
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| Abstract/Notes | AbstractSurfaces of a natural sample of arsenopyrite (FeAsS) were oxidized by a range of inorganic oxidants, and the resultant surface alteration products studied using various spectroscopic techniques. The oxidants used were air during heating to relatively low temperatures (150°C), steam, ammonium hydroxide, hydrogen peroxide, and sulphuric acid. Electrochemical oxidation in water was also undertaken. X-ray photoelectron spectroscopy (XPS), Auger electron spectroscopy (AES), and spectral reflectance measurements, were used to characterize the surface compositions. New data are proposed for the binding energies of core electrons in arsenopyrite based on the fitted XPS spectra: 706.9 eV for the Fe 2p3/2 level, 161.2 eV for the S 2p level, and 40.7eV for the As 3d level. Spectroscopic analyses of the surfaces following oxidation indicated a range of iron oxides and hydroxides (Fe1−xO, Fe3O4, Fe2O3, FeOOH and Fe(OH)3), arsenic oxides (As2O3 and As2O5), sulphur and iron sulphates (FeSO4, Fe2(SO4)3). The relative proportions of the different phases present in the surface layer are related to the strength of the oxidant employed and, where relevant, the Eh/pH conditions prevalent during oxidation. The conclusions regarding the nature of the oxidation of arsenopyrite are discussed in relation to arsenopyrite extraction by flotation and leaching, and the breakdown of arsenopyrite in natural systems. |
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