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Thermochimica Acta
journal homepage: www.elsevier.com/locate/tca
Reaction mechanism of strontium cobaltite synthesis from equimolar
mixture of Sr(NO
3
)
2
and Co(NO
3
)
2
∙6H
2
O under air atmosphere
Cemal Aslan, Sedat Ilhan, Ahmet Orkun Kalpakli, Cem Kahruman, Ibrahim Yusufoglu
⁎
Istanbul University-Cerrahpasa, Engineering Faculty, Metallurgical and Materials Engineering Department, 34320, Avcilar, Istanbul, Turkey
ARTICLEINFO
Keywords:
Strontium cobaltite
Brownmillerite
Perovskite
Characterization
Thermal analysis
ABSTRACT
Strontium cobaltite was produced by heating the mixture containing equimolar amounts of Sr(NO
3
)
2
and Co
(NO
3
)
2
∙6H
2
O under dynamic air atmosphere. The reactions occurred during heating were determined and the
intermediate and fnal products obtained at each reaction step were characterized using TG/DTA-MS, ICP-OES,
XRD and FT-IR techniques. The oxygen stoichiometry of strontium cobaltite was determined using iodometric
titration method and carbonation process.
It was determined by thermal analysis results that Co(NO
3
)
2
∙6H
2
O was decomposed to CoO by forming the
intermediate products Co(NO
3
)
2
∙4H
2
O, Co(NO
3
)
2
∙2H
2
O, Co(NO
3
)
2
∙H
2
O, Co(NO
3
)
2
, CoOOH, Co
2
O
3
and Co
3
O
4
.Sr
(NO
3
)
2
was decomposed to SrO. Sr
6
Co
5
O
15
was formed by solid state reaction of SrO, Co
3
O
4
and O
2
. Sr
2
Co
2
O
5
was produced at elevated temperatures from Sr
6
Co
5
O
15
and Co
3
O
4
.
Analyses carried out for the characterization of compounds obtained at diferent isothermal conditions
showed that fnal product Sr
2
Co
2
O
5
was obtained via Sr
14
Co
11
O
33
and Sr
6
Co
5
O
15
.Sr
2
Co
2
O
5
was decomposed to
a mixture of Sr
6
Co
5
O
15
and Co
3
O
4
with a mole ratio of 1 : 0.333 during slow cooling to the room temperature.
1. Introduction
Strontium cobaltite (SrCoO
3-δ
), which is one of the oxides in the
ABO
3-δδ
perovskite crystal structure, has a wide range of oxygen stoi-
chiometry depending on the temperature, oxygen partial pressure, and
heat treatment method, and therefore has diferent crystalline struc-
tures. Strontium cobaltite has oxygen permeability, ionic and electronic
conductivity and electrochemical activity. Strontium cobaltite is used as
gas sensor, gas detection probe, oxygen separator membrane, cathode
material in solid oxide fuel cells, solid electrolyte and electrode mate-
rial in super capacitors. Strontium cobaltite, which has mixed ionic and
electronic conductivity (MIEC), has recently become increasingly im-
portant [1–11].
Rodriguez et al. [12,13] indicated that Sr
2
Co
2
O
5
has rhombohedral
structure at low temperatures while it has brownmillerite structure
which is a modifed perovskite structure at temperatures higher than
1173 K and there is no diference between chemical composition of
these two structures. While the high temperature structure of Sr
2
Co
2
O
5
remains stable when quenched, it undergoes changing during slow
cooling. According to Takeda et al. [14], strontium cobaltite has
brownmillerite or perovskite structure depending on oxygen defciency
at temperatures above 1073 K. While the sample, quenched to room
temperature from the temperatures between 1073 and 1273 K, has
brownmillerite structure, sample decomposes into cubic perovskite
(SrCoO
2.29
) and brownmillerite structure (SrCoO
2.42
) during slow
cooling. The sample annealed at the temperatures below 1073 K con-
sists of cobalt-defcient strontium cobaltite (SrCo
1-u
O
x
, u ≈ 0.1) and
Co
3
O
4
. Harrison et al. [15] reported that Sr
2
Co
2
O
5
is decomposed to
Sr
6
Co
5
O
15
and Co
3
O
4
during cooling in air for the frst time. Vashook
et al. [4,5] found that SrCoO
x
gains and gives of oxygen during cooling
and heating, respectively. They emphasized that oxygen exchange is
related to phase transformations explained by Rodriquez et al. [13]
between 773 K and 1223 K and is related to the ordered-disordered
mechanism of oxygen vacancies in the cubic phase between 1238 and
1273 K. When δ values for SrCoO
2.5-δ
are less than 0.16, between 0.16
and 0.21 and greater than 0.21, rombohedral, cubic perovskite-like and
disordered-cubic perovskite phases formed, respectively. While XRD
and DTA results do not show any phase change up to 1173 K, above this
temperature, transformation from rhombohedral phase to cubic phase
is seen. According to the results of TG/DTA, the transformation from
rhombohedral to cubic phase occurs at 1173 K in air and 1151 K in Ar
during heating. DTA results show the transformation to low tempera-
ture phase with exothermic peaks at 1051 K in air and 995 K at Ar
during cooling. Ito et al. [16] determined the valence numbers of cobalt
atoms in the lattice of the brownmillerite structure as 4+ for the oc-
tahedral location and 2+ for the tetrahedral location. This charge
https://doi.org/10.1016/j.tca.2019.03.030
Received 28 November 2018; Received in revised form 20 March 2019; Accepted 24 March 2019
⁎
Corresponding author.
E-mail address: yusufogl@istanbul.edu.tr (I. Yusufoglu).
Thermochimica Acta 676 (2019) 52–63
Available online 01 April 2019
0040-6031/ © 2019 Elsevier B.V. All rights reserved.
T