Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18
Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 , is a complex hydrated sulphate of the voltaite group that has been recently discovered on the surface of the Severo-Kambalny geothermal field (Kamchatka, Russia). Vibrational spectroscopy has been applied for characterization of th...
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ftdoajarticles:oai:doaj.org/article:4c5a5caadf524a87a85a2826d45d1d76 2023-05-15T16:59:26+02:00 Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 Anastasia V. Sergeeva Elena S. Zhitova Anton A. Nuzhdaev Andrey A. Zolotarev Vladimir N. Bocharov Rezeda M. Ismagilova 2020-09-01T00:00:00Z https://doi.org/10.3390/min10090781 https://doaj.org/article/4c5a5caadf524a87a85a2826d45d1d76 EN eng MDPI AG https://www.mdpi.com/2075-163X/10/9/781 https://doaj.org/toc/2075-163X doi:10.3390/min10090781 2075-163X https://doaj.org/article/4c5a5caadf524a87a85a2826d45d1d76 Minerals, Vol 10, Iss 781, p 781 (2020) ammoniovoltaite voltaite sulphate iron ammonium water Mineralogy QE351-399.2 article 2020 ftdoajarticles https://doi.org/10.3390/min10090781 2022-12-31T01:49:36Z Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 , is a complex hydrated sulphate of the voltaite group that has been recently discovered on the surface of the Severo-Kambalny geothermal field (Kamchatka, Russia). Vibrational spectroscopy has been applied for characterization of the mineral. Both infrared and Raman spectra of ammoniovoltaite are characterized by an abundance of bands, which corresponds to the diversity of structural fragments and variations of their local symmetry. The infrared spectrum of ammoniovoltaite is similar to that of other voltaite-related compounds. The specific feature related to the dominance of the NH 4 group is its ν 4 mode observed at 1432 cm −1 with a shoulder at 1510 cm −1 appearing due to NH 4 disorder. The Raman spectrum of ammoniovoltaite is basically different from that of voltaite by the appearance of an intensive band centered at 3194 cm −1 and attributed to the ν 3 mode of NH 4 . The latter can serve as a distinctive feature of ammonium in voltaite-group minerals in resemblance to recently reported results for another NH 4 -mineral—tschermigite, where ν 3 of NH 4 occurs at 3163 cm −1 . The values calculated from wavenumbers of infrared bands at 3585 cm −1 , 3467 cm −1 and 3400 cm −1 for hydrogen bond distances: d (O···H) and d (O···O) correspond to bonding involving H1 and H2 atoms of Fe 2+ X 6 ( X = O, OH) octahedra. The infrared bands observed at 3242 cm −1 and 2483 cm −1 are due to stronger hydrogen bonding, that may refer to non-localized H atoms of Al(H 2 O) 6 or NH 4 . Article in Journal/Newspaper Kamchatka Directory of Open Access Journals: DOAJ Articles Minerals 10 9 781 |
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ftdoajarticles |
language |
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topic |
ammoniovoltaite voltaite sulphate iron ammonium water Mineralogy QE351-399.2 |
spellingShingle |
ammoniovoltaite voltaite sulphate iron ammonium water Mineralogy QE351-399.2 Anastasia V. Sergeeva Elena S. Zhitova Anton A. Nuzhdaev Andrey A. Zolotarev Vladimir N. Bocharov Rezeda M. Ismagilova Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
topic_facet |
ammoniovoltaite voltaite sulphate iron ammonium water Mineralogy QE351-399.2 |
description |
Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 , is a complex hydrated sulphate of the voltaite group that has been recently discovered on the surface of the Severo-Kambalny geothermal field (Kamchatka, Russia). Vibrational spectroscopy has been applied for characterization of the mineral. Both infrared and Raman spectra of ammoniovoltaite are characterized by an abundance of bands, which corresponds to the diversity of structural fragments and variations of their local symmetry. The infrared spectrum of ammoniovoltaite is similar to that of other voltaite-related compounds. The specific feature related to the dominance of the NH 4 group is its ν 4 mode observed at 1432 cm −1 with a shoulder at 1510 cm −1 appearing due to NH 4 disorder. The Raman spectrum of ammoniovoltaite is basically different from that of voltaite by the appearance of an intensive band centered at 3194 cm −1 and attributed to the ν 3 mode of NH 4 . The latter can serve as a distinctive feature of ammonium in voltaite-group minerals in resemblance to recently reported results for another NH 4 -mineral—tschermigite, where ν 3 of NH 4 occurs at 3163 cm −1 . The values calculated from wavenumbers of infrared bands at 3585 cm −1 , 3467 cm −1 and 3400 cm −1 for hydrogen bond distances: d (O···H) and d (O···O) correspond to bonding involving H1 and H2 atoms of Fe 2+ X 6 ( X = O, OH) octahedra. The infrared bands observed at 3242 cm −1 and 2483 cm −1 are due to stronger hydrogen bonding, that may refer to non-localized H atoms of Al(H 2 O) 6 or NH 4 . |
format |
Article in Journal/Newspaper |
author |
Anastasia V. Sergeeva Elena S. Zhitova Anton A. Nuzhdaev Andrey A. Zolotarev Vladimir N. Bocharov Rezeda M. Ismagilova |
author_facet |
Anastasia V. Sergeeva Elena S. Zhitova Anton A. Nuzhdaev Andrey A. Zolotarev Vladimir N. Bocharov Rezeda M. Ismagilova |
author_sort |
Anastasia V. Sergeeva |
title |
Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
title_short |
Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
title_full |
Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
title_fullStr |
Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
title_full_unstemmed |
Infrared and Raman Spectroscopy of Ammoniovoltaite, (NH 4 ) 2 Fe 2+ 5 Fe 3+ 3 Al(SO 4 ) 12 (H 2 O) 18 |
title_sort |
infrared and raman spectroscopy of ammoniovoltaite, (nh 4 ) 2 fe 2+ 5 fe 3+ 3 al(so 4 ) 12 (h 2 o) 18 |
publisher |
MDPI AG |
publishDate |
2020 |
url |
https://doi.org/10.3390/min10090781 https://doaj.org/article/4c5a5caadf524a87a85a2826d45d1d76 |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Minerals, Vol 10, Iss 781, p 781 (2020) |
op_relation |
https://www.mdpi.com/2075-163X/10/9/781 https://doaj.org/toc/2075-163X doi:10.3390/min10090781 2075-163X https://doaj.org/article/4c5a5caadf524a87a85a2826d45d1d76 |
op_doi |
https://doi.org/10.3390/min10090781 |
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Minerals |
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10 |
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9 |
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781 |
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