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Ventruti, Gennaro; Della Ventura, Giancarlo; Gomez, Mario Alberto; Capitani, Giancarlo; Sbroscia, Marco; Sodo, Armida (2020) High-temperature study of basic ferric sulfate, FeOHSO4. Physics and Chemistry of Minerals, 47 (10). 43 doi:10.1007/s00269-020-01113-7

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Reference TypeJournal (article/letter/editorial)
TitleHigh-temperature study of basic ferric sulfate, FeOHSO4
JournalPhysics and Chemistry of Minerals
AuthorsVentruti, GennaroAuthor
Della Ventura, GiancarloAuthor
Gomez, Mario AlbertoAuthor
Capitani, GiancarloAuthor
Sbroscia, MarcoAuthor
Sodo, ArmidaAuthor
Year2020 (October)Volume47
Page(s)43Issue10
PublisherSpringer Science and Business Media LLC
URL
DOIdoi:10.1007/s00269-020-01113-7Search in ResearchGate
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Mindat Ref. ID4570422Long-form Identifiermindat:1:5:4570422:6
GUID0
Full ReferenceVentruti, Gennaro; Della Ventura, Giancarlo; Gomez, Mario Alberto; Capitani, Giancarlo; Sbroscia, Marco; Sodo, Armida (2020) High-temperature study of basic ferric sulfate, FeOHSO4. Physics and Chemistry of Minerals, 47 (10). 43 doi:10.1007/s00269-020-01113-7
Plain TextVentruti, Gennaro; Della Ventura, Giancarlo; Gomez, Mario Alberto; Capitani, Giancarlo; Sbroscia, Marco; Sodo, Armida (2020) High-temperature study of basic ferric sulfate, FeOHSO4. Physics and Chemistry of Minerals, 47 (10). 43 doi:10.1007/s00269-020-01113-7
In(2020, October) Physics and Chemistry of Minerals Vol. 47 (10) Springer Science and Business Media LLC
Abstract/NotesAbstractWe report in this paper a new crystal-chemical study of synthetic basic ferric sulfate FeOHSO4. The structure solution performed by the Endeavour program, from new X-ray powder diffraction (XRPD) data, indicated that the correct space group of the monoclinic polytype of FeOHSO4 is C2/c. Selected Area Electron Diffraction (SAED) patterns are also consistent with this structure solution. The arrangement of Fe and S atoms, based on linear chains of Fe3+ octahedra cross-linked by SO4 tetrahedra, corresponds to that of the order/disorder (OD) family. The positions of the hydrogen atoms were located based on DFT calculations. IR and Raman spectra are presented and discussed according to this new structure model. The decomposition of FeOHSO4 during heating was further investigated by means of variable temperature XRPD, thermogravimetry, and differential thermal analysis as well as IR and Raman spectroscopies.

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MineralCitation Details
Unnamed (Fe Sulphate Hydroxide)


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