Ewa M.
Serwicka
*a,
Krzysztof
Bahranowski
b,
Maciej
Sitarz
c,
Małgorzata
Zimowska
a and
Alicja
Michalik-Zym
a
aJerzy Haber Institute of Catalysis and Surface Chemistry, Polish Academy of Sciences, Niezapominajek 8, 30-239 Krakow, Poland
bFaculty of Geology, Geophysics and Environmental Protection, AGH-University of Science and Technology, al. Mickiewicza 30, 30-059 Krakow, Poland
cFaculty of Materials Science and Ceramics, AGH-University of Science and Technology, al. Mickiewicza 30, 30-059 Krakow, Poland
First published on 16th September 2016
Retraction of ‘Vibrational evidence for the “missing link” in structural kinship between kanemite and FSM-16 mesoporous silica’ by Ewa M. Serwicka, et al., Dalton Trans., 2016, DOI: 10.1039/C6DT01600F.
However, recent further investigations have established that the kanemite samples investigated in this study contain trace amount of cristobalite, whose low temperature modification displays a strong band at 620 cm−1. In view of this, the FTIR spectrum feature at 620 cm−1, which was taken for a link between the kanemite and the FSM-16 structures, may not be wholly conclusive of the structural kinship but originate instead from traces of cristobalite transferred from kanemite to FSM-16 during synthesis.
We are currently trying to synthesize kanemite samples free of impurities, in order to be able to re-examine its vibrational spectra and continue our research as to the possible structural links with the mesoporous silicas derived from this material.
Signed: Ewa M. Serwicka, Krzysztof Bahranowski, Maciej Sitarz, Małgorzata Zimowska and Alicja Michalik-Zym, 6th September 2016.
Retraction endorsed by Andrew Shore, Executive Editor, Dalton Transactions.
This journal is © The Royal Society of Chemistry 2016 |