5736 J. Phys. Chem. B, Vol. 102, No. 30, 1998
Letters
1000 cm-1 range (not shown for sake of brevity). The same
interaction in the used sample (Figure 4b) produces quite
different effects: immediately an erosion of the main band from
the low-frequency side, at ∼2100 cm-1, and a decrease of the
band assigned to CO adsorbed on Zr4+ sites are observed. At
increasing contact times the 2132 cm-1 band reduces slightly
in intensity. Molecular CO2 is not detected, and some bands
gradually increase with the contact time in the carbonate-like
region (Figure 4c) assigned to bidentate carbonate and to
bicarbonate species;20 however, the intensities of these bands
are significantly lower than those on the fresh samples.
Probably, on the used samples, where positive gold sites are
already present before oxygen contact, the oxygen does not
activate CO for carbonate-like species formation at the border-
line of the bidimensional metallic particles with the support.
From the data discussed it appears evident that on the used
sample only a small fraction of the exposed gold sites, those
associated with the weak component at ∼2100 cm-1, exhibits
the usual reactivity toward oxygen while the electron-deficient
two-dimensional metallic islands, which are the vast majority
of the exposed gold sites on the used samples, appear signifi-
cantly less reactive than the neutral gold sites exposed on three-
dimensional particles of the new sample. Electronic and/or
structural reasons can be at the origin of the observed differ-
ences. The positive gold sites give rise to stronger Au-CO
bonds, and this fact can cause a reduction of the oxidation
activity. The role of the oxidation state and that of the CO on
Cu, Cu2O, and CuO bond strength in the CO oxidation reaction
has been discussed by Jernigan and Somorjai.21 Moreover, the
coordinative unsaturation of the surface atoms can play a role.
The three-dimensional and almost spherical particles seen by
HRTEM on the fresh sample expose a large amount of step
and corner sites, where CO and oxygen can be adsorbed in close
contact, while flat, bidimensional particles expose mainly highly
coordinated sites.
References and Notes
(1) Haruta, M. Catal. Today 1997, 36, 153 and references therein.
(2) Haruta, M.; Tsubota, S.; Kobayashi, T.; Kageyama, H.; Genet M.
J.; Delmon, B. J. Catal. 1993, 144, 175.
(3) Andreeva, D.; Idakiev, V.; Tabakova, T.; Andreev, A. J. Catal.
1996, 158, 354.
(4) Sakurai, H.; Haruta, M. Appl. Catal. A 1995, 127, 93.
(5) Boccuzzi, F.; Chiorino, A.; Tsubota, S.;. Haruta, M. J. Phys. Chem.
1996, 100, 3625.
Figure 4. FTIR absorbance spectra of CO-O2 interactions on Au/
(6) Haruta, M. Catal. SurVeys Jpn. 1997, 1, 61.
ZrO2 samples. (a) Fresh sample, spectral range 2400-2000 cm-1
:
(7) Baiker, A.; Kilo, M.; Maciejewski, M.; Menzi S.; Wakaun, A. In
New Frontiers in Catalysis; Guczi, L., et al., Eds.; Elsevier Science
Publishers: Amsterdam, 1993; pp 1257.
dashed curve, 10 mbar of CO; full line, spectrum taken 10 min after
the admission of O2. (b) Used sample, spectral range 2400-2000 cm-1
:
dashed curve, 10 mbar of CO; full lines,1-4 spectra taken at increasing
times after the admission of O2 (2, 6, 8, 10 min). (c) Used sample,
spectral range 4000-1000 cm-1: dashed curve, 10 mbar of CO; full
lines,1-3 spectra taken at increasing contact times (2, 6, 10 min).
(8) Boccuzzi, F.; Guglielminotti, E.; Pinna, F.; Strukul, G. Surf. Sci.
1997, 377-379, 728.
(9) Ruggiero, C.; Hollins, P. Surf. Sci. 1997, 377-79, 583.
(10) Dumas, P.; Tobin, R. G.; Richards, P. L. Surf. Sci. 1986, 171, 579.
(11) France, J.; Hollins, P. J. Electron Spectrosc. Relat. Phenom. 1993,
64/65, 251 and ref 5.
(12) Hollins P. Surf. Sci. Rep. 1992, 16, 53 and references therein.
(13) Hoffman, F. M.; Paul, J. J Chem. Phys. 1997, 86, 2990; 87, 1957.
(14) Campbell, C. T. Surf. Sci. Rep. 1997, 27, 1. Xu, X.; Vesecky, S.
M.; Goodman, D. W. Science 1992, 258, 788.
(15) Guillemot, D.; Boresvkov, V. Yu.; Kazansky, V. B.; Polisset-Thfoin,
M.; Fraissard, J. J. Chem. Soc., Faraday Trans. 1997, 93, 3587.
(16) JCPDS 4-784; 10-299; 16-46; 18-580; 28-442.
(17) (a) Alvarez, M. M.; Khoury, T. J.; Schaaff, T. G.; Shafigullin, N.
M.; Vezmar, I.; Whetten, R. L. J. Phys. Chem. B 1997, 101, 3706. (b)
Logunov, S. L.; Ahmadi, T. S.; El-Sayed, M. A.; Khoury, J. T.; Whetten,
R. L. J. Phys. Chem. B 1997, 101, 3713.
(18) van der Zande, B. M. I.; Bohmer, M. R.; Fokkink, L. G. J.;
Schonenberger, C. J. Phys. Chem. B 1997, 101, 852.
(19) Somorjai, G. A. Catal. Lett. 1992, 12, 17 and references therein.
(20) Guglielminotti, E. Langmuir 1990, 6, 5.
initially observed at 2108-2116 cm-1. Many of the observed
features are similar to those previously reported for other gold-
containing samples;5 in particular, the shift of the main band
and the shoulder at higher frequency were ascribed to the
presence of uncoordinated gold sites able to chemisorb oxygen
and carbon monoxide at the same time. The intensification of
the CO absorption band, not observed on the previously
examined samples in similar conditions,5 can be related to a
transient increase in the local CO pressure produced by the
oxygen inlet. This effect was not detected on the previously
examined samples because of their higher reaction rate due to
the smaller size of the gold particles. The band related to CO
adsorbed on Zr4+ sites decreases in intensity, and molecular
CO2 is detected (band at 2351 cm-1). Moreover, on the fresh
sample, very strong bands grow up in the carbonate-like 1700-
(21) Jernigan, G. G.; Somorjai, G. A. J. Catal. 1994, 147, 567.