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Plášil, J., Škoda, R., Fejfarová, K., Čejka, J., Kasatkin, A. V., Dušek, M., Talla, D., Lapčák, L., Machovič, V., Dini, M. (2014) Hydroniumjarosite, (H3O)+Fe3(SO4)2(OH)6, from Cerros Pintados, Chile: Single-crystal X-ray diffraction and vibrational spectroscopic study. Mineralogical Magazine, 78 (3) 535-547 doi:10.1180/minmag.2014.078.3.04

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Reference TypeJournal (article/letter/editorial)
TitleHydroniumjarosite, (H3O)+Fe3(SO4)2(OH)6, from Cerros Pintados, Chile: Single-crystal X-ray diffraction and vibrational spectroscopic study
JournalMineralogical Magazine
AuthorsPlášil, J.Author
Škoda, R.Author
Fejfarová, K.Author
Čejka, J.Author
Kasatkin, A. V.Author
Dušek, M.Author
Talla, D.Author
Lapčák, L.Author
Machovič, V.Author
Dini, M.Author
Year2014 (June)Volume78
Issue3
PublisherMineralogical Society
Download URLhttps://rruff.info/rruff_1.0/uploads/MM78_535.pdf+
DOIdoi:10.1180/minmag.2014.078.3.04Search in ResearchGate
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Mindat Ref. ID244517Long-form Identifiermindat:1:5:244517:9
GUID0
Full ReferencePlášil, J., Škoda, R., Fejfarová, K., Čejka, J., Kasatkin, A. V., Dušek, M., Talla, D., Lapčák, L., Machovič, V., Dini, M. (2014) Hydroniumjarosite, (H3O)+Fe3(SO4)2(OH)6, from Cerros Pintados, Chile: Single-crystal X-ray diffraction and vibrational spectroscopic study. Mineralogical Magazine, 78 (3) 535-547 doi:10.1180/minmag.2014.078.3.04
Plain TextPlášil, J., Škoda, R., Fejfarová, K., Čejka, J., Kasatkin, A. V., Dušek, M., Talla, D., Lapčák, L., Machovič, V., Dini, M. (2014) Hydroniumjarosite, (H3O)+Fe3(SO4)2(OH)6, from Cerros Pintados, Chile: Single-crystal X-ray diffraction and vibrational spectroscopic study. Mineralogical Magazine, 78 (3) 535-547 doi:10.1180/minmag.2014.078.3.04
Abstract/NotesThe natural hydroniumjarosite sample from Cerros Pintados (Chile) was investigated by electron microprobe, single-crystal X-ray diffraction and vibrational spectroscopy (Infrared and Raman). The chemical composition of studied specimens (wt.%, mean of seven analyses) obtained from electron microprobe (in wt.%): Na2O 1.30, K2O 0.23, CaO 0.04, Fe2O350.49, Al2O30.37, SiO20.33, SO333.88, H2O (calculated on the basis of Σ(OH–+H3O+) deduced from the charge balance) 13.32, total 99.98, corresponds to the empirical formula (H3O)0.77+(Na0.20K0.02)∑0.22(Fe2.95Al0.03)∑2.98(OH)6.12[(SO4)1.97(SiO4)0.03]∑2.00(calculated on the basis of S + Si = 2 a.p.f.u. (atoms per formula unit)). The studied hydroniumjarosite is trigonal, with space groupRm, witha= 7.3408(2),c= 17.0451(6) Å andV= 795.46(4) Å3. The refined structure architecture is consistent with known jarosite-series minerals, including synthetic hydroniumjarosite. However, in the current study the presence of H3O+is well documented in difference Fourier maps, where characteristic positive difference Fourier maxima, with apparent trigonal symmetry, were localized in the vicinity of the O4 atom in the channel-voids of the structure. The structure of natural hydroniumjarosite, including the H atoms, was refined toR1= 0.0166 for 2113 unique observed reflections, withIobs>3σ(I). The present structure model, which includes the position of the H atom within the hydronium ion, is discussed with regard to the vibration spectroscopy results and earlier published density-functional theory (DFT) calculations for the alunite-like structure containing H3O+.


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