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Scordari, F. (1980) Structural considerations of some natural and artificial alkali iron hydrated sulphates. Mineralogical Magazine, 43 (329) 669-673 doi:10.1180/minmag.1980.043.329.18

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Reference TypeJournal (article/letter/editorial)
TitleStructural considerations of some natural and artificial alkali iron hydrated sulphates
JournalMineralogical MagazineISSN0026-461X
AuthorsScordari, F.Author
Year1980 (March)Volume43
Issue329
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_43/43-329-669.pdf+
DOIdoi:10.1180/minmag.1980.043.329.18Search in ResearchGate
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Mindat Ref. ID3112Long-form Identifiermindat:1:5:3112:1
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Full ReferenceScordari, F. (1980) Structural considerations of some natural and artificial alkali iron hydrated sulphates. Mineralogical Magazine, 43 (329) 669-673 doi:10.1180/minmag.1980.043.329.18
Plain TextScordari, F. (1980) Structural considerations of some natural and artificial alkali iron hydrated sulphates. Mineralogical Magazine, 43 (329) 669-673 doi:10.1180/minmag.1980.043.329.18
In(1980, March) Mineralogical Magazine Vol. 43 (329) Mineralogical Society
Abstract/NotesSynopsisTwo compounds are described which are structurally related to the three salts, metavoltine, Ξ±-Maus' salt, and an unnamed compound here termed β€˜salt X’: The last three salts have structures based on two sheets of composition [K Fe33+O(SO4)6(H2O)3]4βˆ’ which are essentially intercon-nected via Na atoms in metavoltine, K-atoms in Ξ±-Maus' salt and Na, K, H3O in salt X.Cell parameters and space groups of the new compounds have been determined: as in metavoltine, Ξ±-Maus' salt, and salt X they have a = b ≃ 9.6 Γ…, but the c parameters are ≃ 36 Γ… and ≃ 52 Γ…, i.e. about double and triple that of the other three salts (≃ 18 Γ…).The salt with c ≃ 36 Γ… was obtained using Van Tassel' recipe at about the same conditions which gave rise to salt X, i.e. from a solution containing Na2SO4Β·10H2O, K2SO4, Fe2(SO4)3Β·nH2O (n ≃ 7H2O) in the ratio 3.40:0.60:4.30. The salt with c ≃ 52 Γ… was formed spontaneously through a topotactic reaction of salt X.It is possible to deduce for these two new salts:(1) The presence of clusters of composition [Fe33+O(SO4)6(H2O)3]5βˆ’ interconnected via K atoms to build sheets like those found in meta-voltine, Ξ±-Maus' salt, and salt X.Some sheet sequences which may include the correct sequence.The position of Fe3+ atoms belonging to clusters, which are connected by K atoms to form sheets.The similar a and b lattice parameters, as well as the presence of the threefold axis in all the compounds mentioned, suggest strongly that in the two new compounds there are sheets of composition [K Fe33+O(SO4)6(H2O)3]4βˆ’ which are characterized by a = b ≃ 9.6 Γ… and threefold symmetry. As for the c parameters, examination of possible stacking sequences of the sheets shows which sequences are consistent with the known c parameters and symmetry. The two salts have a parameter and symmetry more similar to metavoltine and salt X than to Ξ±-Maus' salt; moreover, metavoltine and salt X, like the new salts, are more stable than Ξ±-Maus' salt. That is why probably in the two new salts there are two sheets interconnected by Na atoms as in metavoltine and salt X to form a sandwich sheet of composition [Na2K2Fe63+O2(SO4)12(H2O)6]6βˆ’. Then, taking into account the c parameters and space groups, possible sequences of these sandwich sheets are considered in order to establish the likely sequence in the new salts.Metavoltine and salt X contain clusters [Fe33+O(SO4)6(H2O)3]5βˆ’ which are differently oriented: the Fe3+ cation lies at x = 0.17, y = 0.22 or x = 0.22, y = 0.17. These two Fe3+ positions involve an angle rotation for the cluster of about 25Β°. Owing to the similarity in a, b parameters of metavoltine and the salt with c ≃ 52 Γ… on one hand, and of salt X and the salt with c ≃ 36 Γ… on the other, it seems quite probable that the xy coordinates of the Fe3+ cations belonging to the first pair of salts are similar, and similarly for the second pair.(Na, K) Ξ±-Maus' salt effloresces in air, the products being ferrinatrite and goldichite. The transformation (Na, K) Ξ±-Maus' salt β†’ ferrinatrite was clarified when the structure of ferrinatrite was solved. The transition (Na, K) Ξ±-Maus' salt β†’, goldichite is considered in order to understand how [Fe33+O(SO4)6(H2O)3]5βˆ’ clusters may be modified to build new structural units such as the corrugated sheets present in goldichite.


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