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Colloids and Surfaces A: Physicochem. Eng. Aspects 320 (2008) 123–129
Schiff base complex sol–gel method for LaCoO
3
perovskite
preparation with high-adsorbed oxygen
Attera Worayingyong
∗
, Praewpilin Kangvansura, Sutasinee Kityakarn
Department of Chemistry, Faculty of Science, Kasetsart University, Bangkok 10900, Thailand
Received 14 July 2007; received in revised form 30 December 2007; accepted 29 January 2008
Available online 7 February 2008
Abstract
A novel Schiff base complex sol–gel method has been used to prepare LaCoO
3
producing high ratios of adsorbed (or surface) oxygen ()
to lattice oxygen (). The as-prepared gels, characterized by Fourier transform infrared spectroscopy (FTIR), showed that both lanthanum and
cobalt ions were complexed before calcinations. IR spectra revealed that CO
3
2-
and NO
3
-
presented on the sample surfaces during heat treatment.
High-resolution transmission electron microscopic (HRTEM) images of all samples showed resolved lattice fringes with the inter-planar spacing
0.37–0.39 nm of the (0 1 2) plane in hexagonal perovskite. BET surface areas of LaCoO
3
nano-crystals were 11.7–18.6 m
2
/g. Ratios of adsorbed (or
surface) oxygen () to lattice oxygen () quantified by X-ray photoemission spectroscopy showed that LaCoO
3
prepared by the Schiff base complex
method produced higher ratios when bases had higher nitrogen content in molecules. Carbonate and nitrate which were resulting from the oxidation
of functional groups in the Schiff base complex, can produce gaseous compounds and leave vacant sites for oxygen in the gas phase to adsorb.
© 2008 Elsevier B.V. All rights reserved.
Keywords: Schiff base; LaCoO
3
perovskite; Adsorbed oxygen; Lattice oxygen
1. Introduction
Perovskite type oxide was found comparable to Pt/Al
2
O
3
[1,2] as an effective catalyst in catalytic oxidations, including
total oxidation of hydrocarbons. Perovskite can be used as a
gas sensor and in dry cell electrode materials for high tempera-
ture solid oxide fuel cells [3,4]. The most important contribution
to the high activity of mixed oxides such as the perovskite type
oxide, represented by ABO
3
(A: the large ion in the dodecahedral
hole and B: the transition metal ion), is distortion in the individ-
ual BO
6
octahedra [5,6]. The transition metal B in the perovskite
can be particularly active in oxidation catalysis if it can fluctuate
between two stable oxidation states [8] to balance electrically:
(1) the insertion of O
2
-
ion into a lattice from gas phase O
2
, and
(2) the formation of oxygen radicals. Two types of oxygen are
considered to involve in oxidation reaction, adsorbed (or surface)
oxygen () and lattice oxygen () [7]. The adsorbed oxygen ()
is oxygen on the catalytic surface. It is accommodated in the O
2
-
vacancies formed by partial substitution of A-site cations with
∗
Corresponding author. Tel.: +66 2 562 5555x2167; fax: +66 2 579 3955.
E-mail address: fsciarw@ku.ac.th (A. Worayingyong).
lower valence ions or by vacancies of B-site cations, and involves
diffusion of O
2
-
ions through the lattice with the formation of
neighbouring high valence metal ions [7]. Catalytically active
elements (B-site cations) in the perovskite can also be substi-
tuted by other atoms to generate oxygen vacancies [8]. Oxygen
adsorption from the gas phase and further incorporation of oxy-
gen atoms into a lattice, usually leads to three charged oxygen
species, namely O
2
-
,O
-
and O
2-
, depending on vacant sites
[8]. The adsorbed oxygen () is believed to be more active and
reacts with hydrocarbons at lower temperature than the lattice
oxygen () [7,9]. During a catalytic reaction, a perovskite often
exists with non-stoichiometric composition, including typically
the surface oxygen vacancy which could form active oxygen
species by adsorbing oxygen (adsorbed oxygen) from gas phase
capable for oxidation reaction [5,7].
Metal oxide surfaces have been studied by characterizing
hydroxyl (–OH) groups with infrared spectroscopy [10]. X-ray
photoemission spectroscopy has also been used to assess the sur-
face properties of metal oxides [11] in both hydroxyl and oxide
forms. Adsorbed oxygen () and lattice oxygen () equilibrium
could be changed by altering metal A/B ratio in the perovskite
lattice [7].
0927-7757/$ – see front matter © 2008 Elsevier B.V. All rights reserved.
doi:10.1016/j.colsurfa.2008.01.042