142
C. Portet et al. / Thermochimica Acta 497 (2010) 137–142
In general, while there was no effect of post-treatment on
versity of Pennsylvania) for helpful discussions. SEM and Raman
spectrometer were provided by Centralized Research Facilities of
Drexel University. The authors are grateful to the US Department of
Energy (DOE), EERE Program, grant number DE-FC36-04GO14282,
as well as to DOE’s Office of Basic Energy Sciences, for financial
support for this research.
both CO and CO2 evolving from CDC samples. The CO2 des-
orption profiles for the samples chlorinated at 800 and 1100 ◦C
are broadened and the maxima are not centered around 300 ◦C
(Fig. 6b and c) as for samples chlorinated at 600 ◦C (Fig. 6a and
b). The peak of CO desorbing at ∼1000 ◦C becomes narrower
and shifts to higher temperatures for samples chlorinated at 800
and 1100 ◦C (Fig. 6b and c). The change in CO desorption pro-
[22,23].
According to our experimental data, the formation of oxygen
surface moieties occurs after exposure of CDC samples to ambient
air. The TiC precursor has <2% of oxygen. Moreover, most of the
oxygen-containing surface functionalities [19,20] cannot survive
the temperatures used during CDC synthesis (≥600 ◦C).
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Acknowledgements
We are thankful to Professor Christopher Li (Drexel University)
for providing access to the TGA and Professor J.E. Fischer (Uni-