Abstract
57Fe Mössbauer spectroscopy and XRD have successfully been applied to show the incorporation of Fe ion into the interlayer space of montmorillonite via treatment with FeCl 3 in acetone. The 78K 57Fe Mössbauer spectra of montmorillonite samples reflected magnetically split spectrum part indicating the intercalation of iron into the interlayer of montmorillonite via the treatment with FeCl 3+acetone and washed with water until the initial pH=2.3 increased to pH=4.14. It was found that the occurrence of intercalated iron in the form of oxide-oxihydroxide in montmorillonite increases with the pH. Intercalation was confirmed by the gradual increase in the basal spacing d 001 with pH.
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The financial supports from the CAPES (No A127/2013) and OTKA (No K115913 and K115784) grants are acknowledged.
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This article is part of the Topical Collection on Proceedings of the 2nd Mediterranean Conference on the Applications of the Mssbauer Effect (MECAME 2016), Cavtat, Croatia, 31 May-3 June 2016.
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Kuzmann, E., Garg, V.K., Singh, H. et al. Mössbauer study of pH dependence of iron-intercalation in montmorillonite. Hyperfine Interact 237, 106 (2016). https://doi.org/10.1007/s10751-016-1314-5
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DOI: https://doi.org/10.1007/s10751-016-1314-5