D. Gamarra, A. Martínez-Arias / Journal of Catalysis 263 (2009) 189–195
193
+
Fig. 5. Intensity of the Cu carbonyl as a function of reaction temperature under
the indicated CO-PROX mixtures. Overlapping CO(g) contributions were subtracted
as required for this determination by using a reference run performed over inert
KBr under the same experimental conditions.
Fig. 6. DRIFTS spectra of the CeO2 support recorded under the simple CO + H2
+
O2 CO-PROX mixture at the indicated temperatures.
droxyls at that active region could somewhat limit the interfacial
redox processes and consequently the CO oxidation activity, the
deactivation effect appears lower than that observed in the pres-
ence of CO2 in the mixture (Fig. 3), thus indicating the greater
hindering of interfacial redox activity induced by carbonate-type
species.
The region of the spectra related to carbonate-type species re-
flects also the significant hydroxylation degree present over the
sample, leading to frequency modifications for this type of species
or formation of new type of complexes [38,39], as well as a general
which limits the ceria-promoted reduction leading to generation of
partially reduced CuOx active sites at such interfaces, taking into
account our previous hypothesis on the nature of active sites for
this reaction [32]. Evidence for the interfacial location of the car-
bonate species formed can be based on differences with spectra
recorded under CO-PROX conditions for the copper-free ceria sup-
port, Fig. 6, for which practically no oxidation activity was detected
below ca. 453 K. Thus, while the carbonate-related species formed
for copper-free ceria appear fairly similar to those detected for
CuO/CeO2 (basically bidentate species giving most intense bands
−1
intensity decrease for this type of species (ca. half integral inten-
at 1574 and 1306 cm
and poly- or mono-dentate ones at 1493
−1
and 1387 cm−1; note there is a certain shift in these values with
respect to those observed for CuO/CeO2, Fig. 1), they begin to ap-
pear at comparatively higher temperature in the absence of copper,
thus revealing a promoting effect of copper oxide on its forma-
tion and its possible location at ceria positions at or close to the
oxide–oxide interface (which could also explain the shift in bands
positions).
sity in the 1700–1000 cm
range, comparing spectra at 303 K
in the absence and presence of water in the feed). Thus, bands
−1
at 1554 and 1325 cm
may correspond to bidentate carbon-
ates while above ca. 383 K bands are formed at ca. 1547 and
−1
1372 cm−1, which along with those at 2935 and 2845 cm
can
correspond to formate species [39]; we do not believe this indi-
cates onset of WGS at that temperature since, as mentioned above,
WGS activity is residual below ca. 473 K in this type of catalysts
and furthermore requires copper reduction to a metallic state [47],
likely far from being achieved under the employed conditions ac-
cording to XANES analysis of another catalyst of this type [46]. It
On the other hand, the presence of CO2 in the reactant mix-
ture apparently has also an important detrimental influence on
H2 oxidation, according to Fig. 3. This can be related to a CO2-
induced impediment for propagation of the reduction (also pro-
moted to some extent, smaller than the effect produced over in-
terfacial sites, by ceria) over the dispersed CuO particles, which
could provide most active sites for such reaction [32], as suggested
by recent operando-XANES investigation on another catalyst of this
type [46].
−1
cannot be fully discarded that the band detected at ca. 1345 cm
may correspond to the mentioned formate species too, although
it shows a parallel evolution with a band at 1438 cm−1, suggest-
ing that it may correspond to mono- or poly-dentate carbonates
(most intense terminal CO stretching modes) [37,38], somewhat
shifted with respect to analogous bands detected in the absence of
water in the feed as a consequence of the relatively higher hydrox-
The low CO oxidation activity detected at low temperature in
the presence of water in the feed (Fig. 3) is reflected by the
+
ylation degree of the sample surface. Other smaller contributions
strong hindering of formation of Cu carbonyls (Figs. 5 and 7).
−1
are detected at ca. 1510 and 1305 cm
which could be related
The DRIFTS spectra evidence a strong hydroxylation degree for the
to the formation of carboxylate species [38], while small amounts
of hydrogen-carbonate species (bands or shoulders at ca. 1600 and
1399 cm−1) can also be formed at relatively high temperature. It is
noteworthy that, as it was observed in the presence of CO2 (Fig. 4),
onset of CO oxidation (above ca. 373 K) is accompanied by gen-
surface of the sample under this condition (Fig. 7). This is evi-
−1
denced by the strong intensity of a broad band at ca. 3317 cm
,
−1
which along with weaker ones at ca. 3692 and 1625 cm
can
be attributed to the presence of undissociated water molecules on
the sample surface (the two former correspond to OH stretching
modes and the latter to HOH bending [37]). The significant de-
crease of these species at temperatures above ca. 373 K allows
onset of CO oxidation (Fig. 3). Therefore, it appears that the re-
action onset shift is mainly related to a water-induced blocking
phenomenon which prevents access of the reactant molecules to
the interfacial active sites for consequent reductive activation and
reaction. Although above that temperature, the formation of hy-
−1
eration of the band at 1438 cm
(1478 cm−1without water in
the feed) suggesting, as outlined above, that formation of the cor-
responding carbonate (or carbonite, see above discussion) species
can be associated to the interfacial reduction processes associated
to generation of active sites for the reaction. Further experiments
are in course in order to corroborate and get details on this type
of correlation.