TY - JOUR AU - Kuzmann, Ernő AU - Garg, VK AU - Singh, H AU - de Oliveira, AC AU - Pati, SS AU - Homonnay, Zoltán AU - Rudolf, M AU - Molnár, ÁM AU - Kovács, Eszter Mária AU - Baranyai, Edina AU - Kubuki, S AU - M. Nagy, Noémi AU - Kónya, József TI - Mössbauer study of pH dependence of iron-intercalation in montmorillonite JF - HYPERFINE INTERACTIONS J2 - HYPERFINE INTERACT VL - 237 PY - 2016 IS - 1 PG - 6 SN - 0304-3843 DO - 10.1007/s10751-016-1314-5 UR - https://m2.mtmt.hu/api/publication/3097530 ID - 3097530 N1 - WoS:hiba:000379534100001 2020-12-06 01:42 cikkazonosító nem egyezik Institute of Chemistry, Eötvös Loránd University, Budapest, Hungary Institute of Physics, University of Brasília, Brasília, DF, Brazil Imre Lajos Isotope Laboratory, Department of Colloid and Environmental Chemistry, University of Debrecen, Debrecen, Hungary Department of Inorganic and Analytical Chemistry, University of Debrecen, Debrecen, Hungary Department of Chemistry, Tokyo Metropolitan University, Tokyo, 192-0397, Japan Cited By :4 Export Date: 5 February 2021 CODEN: HYIND Correspondence Address: Kuzmann, E.; Institute of Physics, Brazil; email: kuzmann@caesar.elte.hu AB - 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 d001 with pH. © 2016, Springer International Publishing Switzerland. LA - English DB - MTMT ER -