The thermal decomposition and structural reconstruction of Mg-Fe-based
hydrotalcites (FIT) have been studied through thermogravimetric
analyses, X-ray powder diffraction (XRD), Fourier transform infrared
spectroscopy and Mossbauer spectroscopy. The destruction of the layered
structure took place at about 300degreesC. The broad peaks observed in
the X-ray diffractograms suggest that the resultant oxides constitute a
solid solution. For samples treated at temperatures higher than
500degreesC, the formation of the MgO and MgFe2O4 spinel phases is
observed. Fe-57 Mossbauer spectroscopy was employed to monitor the Fe
chemical environment for the samples annealed at different temperatures
(100-900degreesC). In situ XRD experiments revealed that the HTs start
an interlayer contraction at about 180degreesC. This phenomenon is
identified as being due to a grafting process for which the
interlamellar anions attach to the layers through a covalent bond. The
reconstruction of the HTs was also investigated and its efficiency
depends on the thermal annealing temperature and the Mg/Fe ratio. The
structure of the reconstructed samples was found to be exactly the same
as the parent structure. (C) 2004 Elsevier Inc. All rights reserved.
%0 Journal Article
%1 WOS:000223960700014
%A Ferreira, OP
%A Alves, OL
%A Gouveia, DX
%A Souza, AG
%A de Paiva, JAC
%A Mendes, J
%C 525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA
%D 2004
%I ACADEMIC PRESS INC ELSEVIER SCIENCE
%J JOURNAL OF SOLID STATE CHEMISTRY
%K Effect; Memory Mossbauer anionic clays; compounds; decomposition; double hydrotalcite-like hydroxides; iron} mixed oxides; pyroaurite; reconstruction; rehydration; spectroscopy; spinel; structural thermal {layered
%N 9
%P 3058-3069
%R 10.1016/j.jssc.2004.04.030
%T Thermal decomposition and structural reconstruction effect on
Mg-Fe-based hydrotalcite compounds
%V 177
%X The thermal decomposition and structural reconstruction of Mg-Fe-based
hydrotalcites (FIT) have been studied through thermogravimetric
analyses, X-ray powder diffraction (XRD), Fourier transform infrared
spectroscopy and Mossbauer spectroscopy. The destruction of the layered
structure took place at about 300degreesC. The broad peaks observed in
the X-ray diffractograms suggest that the resultant oxides constitute a
solid solution. For samples treated at temperatures higher than
500degreesC, the formation of the MgO and MgFe2O4 spinel phases is
observed. Fe-57 Mossbauer spectroscopy was employed to monitor the Fe
chemical environment for the samples annealed at different temperatures
(100-900degreesC). In situ XRD experiments revealed that the HTs start
an interlayer contraction at about 180degreesC. This phenomenon is
identified as being due to a grafting process for which the
interlamellar anions attach to the layers through a covalent bond. The
reconstruction of the HTs was also investigated and its efficiency
depends on the thermal annealing temperature and the Mg/Fe ratio. The
structure of the reconstructed samples was found to be exactly the same
as the parent structure. (C) 2004 Elsevier Inc. All rights reserved.
@article{WOS:000223960700014,
abstract = {The thermal decomposition and structural reconstruction of Mg-Fe-based
hydrotalcites (FIT) have been studied through thermogravimetric
analyses, X-ray powder diffraction (XRD), Fourier transform infrared
spectroscopy and Mossbauer spectroscopy. The destruction of the layered
structure took place at about 300degreesC. The broad peaks observed in
the X-ray diffractograms suggest that the resultant oxides constitute a
solid solution. For samples treated at temperatures higher than
500degreesC, the formation of the MgO and MgFe2O4 spinel phases is
observed. Fe-57 Mossbauer spectroscopy was employed to monitor the Fe
chemical environment for the samples annealed at different temperatures
(100-900degreesC). In situ XRD experiments revealed that the HTs start
an interlayer contraction at about 180degreesC. This phenomenon is
identified as being due to a grafting process for which the
interlamellar anions attach to the layers through a covalent bond. The
reconstruction of the HTs was also investigated and its efficiency
depends on the thermal annealing temperature and the Mg/Fe ratio. The
structure of the reconstructed samples was found to be exactly the same
as the parent structure. (C) 2004 Elsevier Inc. All rights reserved.},
added-at = {2022-05-23T20:00:14.000+0200},
address = {525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA},
author = {Ferreira, OP and Alves, OL and Gouveia, DX and Souza, AG and de Paiva, JAC and Mendes, J},
biburl = {https://www.bibsonomy.org/bibtex/2eaf95d02572d5a0bd4c001104a6f973f/ppgfis_ufc_br},
doi = {10.1016/j.jssc.2004.04.030},
interhash = {ef9fddbff47519ccfce545ddf1d2f0e3},
intrahash = {eaf95d02572d5a0bd4c001104a6f973f},
issn = {0022-4596},
journal = {JOURNAL OF SOLID STATE CHEMISTRY},
keywords = {Effect; Memory Mossbauer anionic clays; compounds; decomposition; double hydrotalcite-like hydroxides; iron} mixed oxides; pyroaurite; reconstruction; rehydration; spectroscopy; spinel; structural thermal {layered},
number = 9,
pages = {3058-3069},
publisher = {ACADEMIC PRESS INC ELSEVIER SCIENCE},
pubstate = {published},
timestamp = {2022-05-23T20:00:14.000+0200},
title = {Thermal decomposition and structural reconstruction effect on
Mg-Fe-based hydrotalcite compounds},
tppubtype = {article},
volume = 177,
year = 2004
}