Chemistry Letters Vol.32, No.5 (2003)
437
handling for XRD analysis, was observed for VOx/MgO as well
as those from MgF2 and MgO. These observations agree with
the gas-phase product analysis shown in Figure 1.
The reason why only deposition of vanadium oxides pro-
moted chlorine absorption should be related to capability for de-
composition of CCl4. Klabunde et al. reported that vanadium
oxides supported on MgO showed the highest ability for CCl4
decomposition among several metal oxides and the order in
the activity was as follows: V > Mn > Co > Fe > Cu >
Ni.6 Facile formation of unstable vanadium halides (or oxyhal-
ides) would be related to the activity for chlorine absorption, i.e.
CCl4 decomposition. After the CFC12 decomposition by VOx/
MgO, a small amount of yellowish deposition of VF3O was ob-
served in the reactor and at downstream of reaction gas flow, a
dark green hygroscopic material, which was assigned to VClO
by XRD analysis, was formed. VClO was probably originated
from VCl3O. These two oxyvanadium compounds are easily
melted or evaporated under the reaction condition employed
in this system (boiling point for VF3O and VCl3O are 753 K
and 400 K, respectively). Such unstable intermediate com-
pounds can migrate to MgO-rich sites to react with MgO to alter
back to vanadium oxides with formation of magnesium halides
until almost all of MgO are consumed. However, as available
amount of MgO decreased, they evaporated to loss from the
MgO. In this way, addition of vanadium oxides can enhance
CFC12 decomposition and the absorption of both chlorine and
fluorine as magnesium halides.
Figure 1. CFC12 decomposition by VOx/MgO (l, ꢄ) and
FeOx/MgO (n, Ã). CFC12 conv. (solid), CO2 select. (open).
Reaction temperature: 723 K.
From these results, supporting transition metal oxides on
MgO was effective for destructive adsorption of CFC12 with
halogen fixation as magnesium halides, but fixation of chloride
was found to be difficult except for VOx/MgO. Even for VOx/
MgO, which exhibited the highest activity, the complete decom-
position of CFC12 to CO2 and halides takes place until MgO
consumption becomes below 30%, and then efficiency of de-
composition decreased as more MgO is consumed. But even
when stoichiometric amount of CFC12 was loaded to the sys-
tem, MgO conversion reached over 80% and formations of by-
products were still quite small at CFC12 loading of stoichio-
metric amount to MgO. Destructive halogen fixation by
transition metal supported MgO is a promising method to de-
compose CFCs without releasing corrosive acid gases. Further
studies to reveal detail mechanism of this destructive halogen
fixation and to improve the system are under way.
Figure 2. XRD patterns of FeOx/MgO (a) and VOx/MgO (b)
after reaction with CFC12 for 3 h. MgO (ꢄ), MgF2 (n), and
MgCl2ꢃnH2O (s).
In short, selective fluorine absorption happened to proceed
throughout the CFC12 decomposition. However, VOx/MgO
showed high CO2 selectivity of 96% and negligible formation
of CCl4, hence remarkable activity to CFC12 decomposition
and simultaneous halogen fixation.
Since FeOx/MgO exhibited high activity to CFC12 decom-
position with selective fluorine absorption, VOx/MgO and
FeOx/MgO were studied further to understand details of the de-
composition of CFC12 with halogen absorption. As time course
of CFC12 decomposition shown in Figure 1, VOx/MgO exhib-
ited high activity by the reaction time of 1 h to decomposition of
CFC12 to form CO2 as the only gas-phase product. However, as
MgO was consumed to be halides, the efficiency of the decom-
position gradually decreased. FeOx/MgO showed high CFC12
conversion, but CO2 selectivity was just around 50% throughout
the reaction and CCl4 was always formed as a dominant by-pro-
duct.
XRD patterns of VOx/MgO and FeOx/MgO after the reac-
tion indicated formation of magnesium halides (Figure 2). Prob-
ably because of high dispersion and low content of vanadium
oxides and iron oxides, all observed diffraction patterns were
originated from magnesium compounds. For FeOx/MgO after
the reaction, only MgF2 and remained MgO were found and
MgCl2 was not clearly observed while diffraction pattern origi-
nated from MgCl2ꢃnH2O, which was formed by the hydration of
hygroscopic MgCl2 by exposure to ambient air during sample-
References
1
Y. Takita, G.-R. Li, R. Matsuzaki, H. Wakamatsu, H.
Nishiguchi, Y. Moro-oka, and T. Ishihara, Chem. Lett., 1997, 13.
Y. Takita, H. Wakamatsu, M. Tokumaru, H. Nishiguchi, M. Ito,
and T. Ishihara, Appl. Catal., A, 194, 55 (2000).
S. Karmakar and H. L. Greene, J. Catal., 151, 394 (1995).
B. M. Weckhuysen, G. Mestl, M. P. Rosynek, T. R. Klawietz, J.
F. Haw, and J. H. Lunsford, J. Phys. B: At. Mol. Opt. Phys., 102,
3773 (1998).
2
3
4
5
K. J. Klabunde, J. Stark, O. Koper, C. Mohs, D. G. Park, S.
Decker, Y. Jiang, I. Lagadic, and D. Zhang, J. Phys. Chem.,
100, 12142 (1996).
6
7
8
Y. Jiang, S. Decker, C. Mohs, and K. J. Klabunde, J. Catal., 180,
24 (1998).
K. J. Klabunde, A. Khaleel, and D. Park, High Temp. Mater.
Sci., 33, 99 (1995).
S. P. Decker, J. S. Klabunde, A. Khaleel, K. J. Klabunde, Envir-
on. Sci. Technol., 36, 762 (2002).
Published on the web (Advance View) April 16, 2003;DOI 10.1246/cl.2003.4 36