Abstract
Mössbauer spectroscopy, x-ray powder diffraction, thermal analysis and elemental analysis were used for the study of the mechanism of reaction between NaCI and Fe2(SO4)3 in the oxidizing atmosphere (air). It was found that the reaction starts at 400°C in isothermal conditions and is accompanied by the liberation of Cl2. The initial reaction proceeds in the molar ratio of NaCl:Fe2(SO4)3=3:1. β-Fe2O3, NaFe(SO4)2, Na3Fe(SO4)3 and Na2SO4 were identified as solid products of the initial reaction. At the second stage both the double sulfates were transformed into β-Fe2O3 and Na2SO4, the gaseous SO3 was liberated simultaneously. Thermally less stable NaFe(SO4)2 decomposes before Na3Fe(SO4)3. The hexagonal α-Fe2O3 is formed in this process only as the product of the structural transformation of β-Fe2O3. This beta-alpha transformation accompanies both the initial reaction and the secondary conversions of the intermediates. The Mössbauer parameters of the reaction products are enlisted.
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© 1999 Springer Science+Business Media Dordrecht
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Zboril, R., Mashlan, M., Krausova, D. (1999). The Mechanism of β-Fe2O3 Formation by Solid-State Reaction between NaCl and Fe2(SO4)3 . In: Miglierini, M., Petridis, D. (eds) Mössbauer Spectroscopy in Materials Science. NATO Science Series, vol 66. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4548-0_5
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DOI: https://doi.org/10.1007/978-94-011-4548-0_5
Publisher Name: Springer, Dordrecht
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