72
C.-W. Tang et al. / Thermochimica Acta 473 (2008) 68–73
Table 2
Experimental and theorization of a series of cobalt oxide for TG-MS
Sample
CoOOHc
Reaction process
Weight loss (%)a
Theoretical
Outlet gas (C)b
Experimental
H2O
300
O2
12CoO(OH) → 4Co3O4 + O2 + 6H2O
2Co3O4 → 6CoO + O2
13
19
7
12
20
8
920
c
Co3O4
2Co3O4 → 6CoO + O2
–
–
820
920
A
B
CoOd
6CoO + O2−→ 2Co3O4−→ 6CoO + O2
A:7
B:-7
A:7
B:-8
a
Measurement of TG.
Measurement of mass analyzer.
By TG-MS flow He.
By TG-MS flow air.
b
c
d
A convenient procedure for preparing a series of pure cobalt
oxides is presented; it involves the decomposition of CoOx in a
nitrogen environment at different temperatures.
TG-MS, XRD, Raman, FTIR and TPR analyses are demonstrated to
be useful in identifying the series of cobalt oxides. The D-280 sam-
ple [CoO(OH)] has a hexagonal structure that gives rise to Co3O4
and CoO in helium at 280 and 850 ◦C, respectively. The D-450 sam-
ple [Co3O4] has a spinel structure that gives rise to CoO in helium at
820 ◦C. The D-950 sample [CoO] has a faced-centered cubic struc-
ture that can be oxidized to Co3O4 at 200–600 ◦C and decomposed
to CoO at 850–1000 ◦C in air, respectively. The preparation of mate-
rials and the analysis of their thermal behavior is a convenient way
to control and determining the purity of cobalt oxide.
Fig. 7. Analysis of the outlet gases from the decomposition of D-450 by TG-MS (heat-
ing rate of 10 ◦C min−1 under He): O2 (red). (For interpretation of the references to
color in this figure legend, the reader is referred to the web version of the article.)
Acknowledgements
We are pleased to acknowledge financial supports for this study
from Academia Sinica and the National Science Council of the
Republic of China.
to O2 at 820 ◦C. The weight loss of 8% is caused mainly by the
decomposition of Co3O4 to CoO, according to Eq. (7).
Fig. 8 shows the TG profile of the D-950 sample in air. The weight
increase of 7% involves mainly the oxidation of CoO to Co3O4 as
the temperature is increased from 250 to 900 ◦C, followed by the
desorption of oxygen to CoO at above 900 ◦C. Comparing the theo-
retical weight variations of the proposed reaction (columns 2 and
3 in Table 2) with the experimental results demonstrated that CoO
can undergo oxidation–reduction in air, according to Eq. (8).
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