PREPARATION, CHARACTERIZATION AND CATALYTIC ACTIVITY OF Co-Zn-BASED MANGANITES OBTAINED FROM CARBONATE PRECURSORS
Articolo
Data di Pubblicazione:
2001
Abstract:
Cobalt-zinc manganites at rather low Co content (x = Co/(Co+Zn) = 0, 0.01, 0.05, 0.10) were prepared by thermal
decomposition of carbonate precursors obtained by coprecipitation at constant pH. Precursors were characterized by X-ray
diffraction (XRD), diffuse reflectance spectroscopy (DRS), thermogravimetric analysis (TGA-DTA) and magnetic susceptibility
measurements. For all samples, a single rhodochrosite-like phase, CoxZnyMn(1-x-y)CO3, was formed, as detected by
XRD. Magnetic analysis confirmed that cobalt and manganese were present as Co2+ and Mn2+ in the rhodochrosite crystal
lattice. The carbonate monophasic precursors were decomposed at 723 and 973 K in air and Co-Zn-Mn based spinel-like
solid solutions were obtained at both temperatures. The DRS and magnetic susceptibility data suggested that after calcination
cobalt was mainly present as Co3+ ions in the octahedral sites of the spinel together with Mn3+ ions. The catalyst reducibility
in H2 was studied by temperature-programmed reduction (TPR). The cobalt containing catalysts reduced almost as the pure
ZnMn2O4 suggesting that cobalt does not show a detectable influence on the spinel reducibility. Preliminary results of the
catalytic activity for the reduction of NO by hydrocarbons in absence of oxygen are presented.
decomposition of carbonate precursors obtained by coprecipitation at constant pH. Precursors were characterized by X-ray
diffraction (XRD), diffuse reflectance spectroscopy (DRS), thermogravimetric analysis (TGA-DTA) and magnetic susceptibility
measurements. For all samples, a single rhodochrosite-like phase, CoxZnyMn(1-x-y)CO3, was formed, as detected by
XRD. Magnetic analysis confirmed that cobalt and manganese were present as Co2+ and Mn2+ in the rhodochrosite crystal
lattice. The carbonate monophasic precursors were decomposed at 723 and 973 K in air and Co-Zn-Mn based spinel-like
solid solutions were obtained at both temperatures. The DRS and magnetic susceptibility data suggested that after calcination
cobalt was mainly present as Co3+ ions in the octahedral sites of the spinel together with Mn3+ ions. The catalyst reducibility
in H2 was studied by temperature-programmed reduction (TPR). The cobalt containing catalysts reduced almost as the pure
ZnMn2O4 suggesting that cobalt does not show a detectable influence on the spinel reducibility. Preliminary results of the
catalytic activity for the reduction of NO by hydrocarbons in absence of oxygen are presented.
Tipologia CRIS:
01.01 Articolo in rivista
Elenco autori:
Dragone, Roberto; Ferraris, Giovanni; Fierro, Giuseppe; Inversi, Marcello
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