3.1. Species Formed During Adsorption of O2 on Oxidized and Reduced Ceria
On oxidized ceria, even after evacuation of the samples at 773 K, we have observed only molecularly adsorbed O
2 by a weak band at 1555-1553 cm
-1. Although some authors report that no reactive O
2 adsorption occurs on oxidized ceria [
43,
62], others have observed superoxides with non-reduced samples evacuated at 673 K [
59]. In our experiments with oxidized samples we have treated them in O
2 immediately before evacuation at the target temperature (573-773 K). Note that ceria is very easy reduced and even minor amount of organic contaminants originally present in the sample or introduced during the experiments could lead to production of small amount of Ce
3+ during thermal treatment.
As a homonuclear diatomic molecule O
2 has no IR active mode. However, after adsorption, the symmetry is reduced and the O–O stretching modes, although with low intensity, become IR observable. The same phenomenon has been observed for similar molecules, as N
2 and H
2 [
85].
The possible active site for this adsorption form of oxygen on ceria are coordinatively unsaturated (cus) Ce
4+ cations and hydroxyl groups. The results presented in
Figure S4, (spectra a-c) clearly show that the ν(O–O) band increases in intensity with sample dehydroxylation which indicates the principal active sites are Ce
4+ cations. Indeed, Ce
4+ hydroxyls are of weak acidity and their complexes with O
2 are expected to be very weak. The conclusion that OH groups are not active sites for adsorption of molecular O
2 are consistent with the lack of molecularly adsorbed O
2 on the hydrated sample (reduced, evacuated at 573 K and then reoxidized at 100 K).
The ν(O–O) band appeared at 1553 cm
-1 with the sample which was reduced and evacuated at 773 K and then fast oxidized at 100 K (
Figure S4, spectrum d). The intensity was halved compared to the oxidized sample evacuated at the same temperature. This suggests that the fast oxidation creates some cus Ce
4+ sites acting as adsorption centers. However, it is also possible that some Ce
4+ sites are blocked by other adsorbed species (see below).
On reduced ceria we have detected two more types of adsorbed oxygen: superoxide and peroxide species and the
18O
2 isotopic experiments confirmed this assignment. This is in general agreement with literature data [
39,
41,
43,
59,
60,
61,
62].
Superoxide ion is a monovalent radical produced as a result of one-electron reduction of dioxygen and thus has an O−O bond order of ca. 1.5. Consequently the ν(O–O) stretching frequency is lower as compared to O2. This is consistent with the observation of the superoxide band around 1130 cm-1. Simple stoichiometric considerations show that two O2− radicals are necessary to formally substitute one O2− anion.
There are two possible configurations of the adsorbed superoxo species: end-on (η
1) or side-on (η
2) [
86], as shown in
Scheme 1:
If the end-on configuration is realized, the Ce4+(16O18O)- species should manifest two bands, depending on the position of the labelled atom. In our experiments we have not detected Ce4+(16O18O)- isotopologues. However, Li et al., in experiments with coadsorption of a 16O2-18O2 mixture succeeded to detect such species and reported they were characterized by one band only, at 1095 cm-1. This strongly indicates a side-on configuration of the superoxo species on ceria.
Consider now the peroxo species. In peroxides the oxygen atoms are linked by a single covalent bond and consequently the ν(O–O) modes are observed at lower frequencies as compared to superoxo species. In contrast to superoxide and similarly to O2−, it is a divalent anion. This makes peroxide anion suitable to fill oxygen vacancies on ceria.
Pushkarev et al. [
62] have reported that peroxides are not formed when ceria is reduced at 573 K, but appeared on 673 K reduced samples. Similar conclusions were made by Li et al. [
60,
61], who have not observed peroxides on ceria reduced by treatment in vacuo at 1000 K, but detected them on a hydrogen-reduced sample. This is in agreement with DFT studies [
87] indicating that O
2 interaction with oxygen vacancies on ceria produces peroxides. Thus, it appears that peroxides should acquire bridging configuration.
Raman studies report two kinds of peroxo species on ceria, characterized by bands at ca. 860 and 830 cm
-1 [
41,
43,
62]. A band at 883 cm
-1 have been reported in IR studies [
60,
61].
Interesting results have been reported by Bashir and Idriss [
88]. They adsorbed H
2O
2 on ceria and detected IR bands at 890, 850 and 835 cm
-1. The former band was attributed to side-on peroxide and the other two bands, to bridging species. The band at 890 cm
-1 almost disappeared after 363 K evacuation while the other two bands were still observable after 433 K evacuation. The similarity of these bands to the bands appearing after O
2 adsorption on reduced ceria confirms their assignment to peroxides.
Surprisingly, formation of Ce
4+-OOH
− species has not been reported. In fact, this possibility has been considered, but rejected on the basis of the expectation that OOH
- species should absorb at considerably higher wavenumbers [
88]. However, analysis of summarized literature data [
86] indicates that OOH
− species absorb at relatively low frequencies. Thus, it has been reported that Ti-OOH species produced by H
2O
2 adsorption on Ti silicalite sieve are characterized by a ν(O−O) band at 837 cm
-1 and a broad ν(O−O) band around 3400 cm
-1 [
89]. Indeed, H
2O
2 is weak acid and the protons from the OOH
- groups should tend to form H-bonds. This makes the OH mode difficulty discernible from H-bonded hydroxyls. We note that the OOH
− moiety is univalent and, as will be shown below, formation of Ce−OOH species will answer some open and unresolved question in ceria surface chemistry.
To form OOH species, a source of hydrogen is necessary. One possible source are the residual OH groups. However, it seems that dissolved hydrogen is a more important source. A look at
Figure 11B shows that peroxide species absorbing in the 850-820 cm
-1 spectral region are readily formed with samples having a high amount of dissolved hydrogen. Therefore, we propose that these species are hydroperoxides. By analogy, we may propose that the same accounts for the band at 810 cm
-1. In contrast, the band at 890 cm
-1 is typical of the hydrogen-free sample, which suggests that it is due to H-free O
22− species.
3.2. Ce3+ Sites Involved in Fast Oxidation
Based on our results, we can divide the Ce3+ sites on reduced ceria according to their reactivity into three groups:
Ce3+ cations that are fast oxidized at 100 K;
Ce3+ cations fast oxidized between 100 and 293 K, and
Ce3+ cations resisting oxidation at 293 K but oxidized at slightly higher temperature, up to 393 K.
The fraction of the sites in the third group is relatively small, about 10-15 % depending on the pretreatment conditions. Probably this is a problem of accessibility, because their Ce3+ electronic transition band is broad, suggesting heterogeneity. This does not exclude the possibility they to be located at subsurface layers.
The fractions of the other two kinds of Ce3+ sites are abruptly equal. This suggest that they are surface situated but differ in reactivity.
Consider first the sites fast oxidized at 100 K. It appears that they are of several different kinds, at least sites connected with OH groups and sites connected with residual carbonates.
Looking on the spectra presented in
Figure 7 one could conclude that the Ce
3+ sites attached to OH groups are fast oxidized with simultaneous production of O
2− species according to the following hypothetic reaction:
However, a careful analysis of the spectra indicates that the situation is much more complicated. Thus, if reaction (1) occurred, the OH band should undergo an additional shift at full oxidation (including the two Ce3+ sites) which was not observed in the experiments.
Note that during the fast oxidation of Ce3+ sites the formation of superoxides and peroxides as well as the concomitant changes (e.g. in the hydroxyl or carbonate regions) proceed in parallel. We attribute this to the so-called “wall effect”. Reactive adsorption of oxygen is irreversible and O2 molecules interact with the first appropriate site they meet in their way. Thus the ratio between the different Ce3+ sites oxidized at 100 K will not be determined by the differences in their affinity to oxygen. From this we may conclude that all Ce3+ sites participating in the fast oxidation are accessible and situated on the surface.
Consequently, an important conclusion on the location of surface carbonates can be made. There are sound arguments that they are not situated on the surface [
53,
55]. However, it appears that they on reduced samples at least part of them are connected to surface Ce
3+ sites. Thus could happen if the carbonates are located at the subsurface layer.
Bridging hydroxyls on ceria are of II or III type, i.e. connected with two or three cerium cations. However, it is important to note that for samples evacuated at 773 K the regular crystal planes are dehydroxylated and the residual hydroxyls are located at edges, corners or other defect sites. Therefore, the Ce3+ ions connected to OH groups should be highly accessible. It is also expected that a large part of Ce3+ sites are not connected to OH groups or carbonate ions.
A widely accepted reaction of ceria reduction is that leading to formation of oxygen vacancies:
where □ denotes an oxygen vacancy.
Reoxidation needs formation of divalent anion and this can be easily achieved according to the reaction:
At temperatures above ca. 473 K peroxides completely decompose and the original state typical of oxidized ceria surface is restored:
Most probably analogous reaction occurs when Ce3+ sites from bridging hydroxyls are oxidized, because it was already noted that no step oxidation of the two Ce3+ sites was detected.
It was, however, noted that the formation of superoxide species cannot be explained by the model of surface oxygen vacancy and is rather indicative of presence of low-coordinated Ce
3+ sites [
87]. We propose that such Ce
3+ sites can be produced by reduction of Ce
4+ sites connected to terminal OH groups:
Indeed, the results presented on
Figure 6,
Figure 7 and
Figure 13 show that after the fast oxidation the terminal OH groups on the CeO
2-NC sample are not regenerated. It is logic to expect that the charge balance is achieved by formation of a Ce
4+-O
2− complex, e.g. according to the following reaction:
Thus, one of the possible locations of the Ce4+–O2− species is on the place of the original terminal Ce4+–OH groups.
It was established that oxidation at 100 K leads to obtaining of a highly stable semioxidized state of ceria. However, a large part of Ce3+ sites are additionally oxidized at temperatures intermediate between 100 and 293 K. First, some extra superoxide species were produced in this way. This indicates proceeding of reaction (6) and evidences the existence of a fraction of less reactive isolated Ce3+ sites. However, the superoxide band started to decline with the temperature rise and particular peroxide species were produced at its expense.
Based on similar observation, Li et al. [
60] proposed the following evolution of the oxygen adspecies on ceria:
According to our results this equation should be divided in two independent parts: evolution of peroxo and evolution of superoxo species.
It was also noted that peroxides could be directly decomposed thus producing lattice oxygen on the place of the oxygen vacancy.
Consider now the superoxide species. The fact that they form on isolated ex-Ce
3+ sites indicates that they must evolve by forming monovalent anions. A hypothetic candidate for this is the O
− anion. However, we have no indication of its formation. In contrast, we already proposed that the bands below 850 cm
-1 characterize hydroperoxo species. Thus, a possible reduction of the Ce
4+-O
2− species is according to the following reaction:
In this case the interaction proceeds with hydrogen dissolved in ceria. Indeed, it was established that it promotes formation of hydroperoxides. We cannot exclude some hydroperoxides to be formed with participation of hydrogen from surface OH groups.
After decomposition of the Ce
4+-OOH groups the original terminal hydroxyls typical of oxidized surface are restored:
The initial stage of this reaction was documented in our IR results (see
Figure 6B, spectrum k).
The O
− radicals are IR invisible but has been observed on some oxides by ESR [
90]. Although suggested [
60], these species have not been reported for pure ceria. In any case, we cannot totally rule out the possibility that, under hydrogen-deficient conditions, direct decomposition of O
2− to O
− occurs, the latter ensuring the charge balance instead of OH
− or OOH
−.
In conclusions, the evolution of the adsorbed oxygen species on isolated Ce3+ sites and on oxygen vacancies follow two different and independent routes.
3.3. Fine Structure of Ce3+ Band
It was found that Ce3+ band has a fine structure. This explains the different values of the band position reported in the literature. To the best of our knowledge, the fine structure of this band has not been discussed. Therefore, this work is the first attempt to assign the different components of the band. We realize that additional work has to be done for the precise attribution, but our results allow making some definite conclusions.
At first, is was unambiguously established that the position of the sub-bands strongly depends on the presence of OH group(s) in the first coordination sphere of Ce
3+ cations. Comparison between the spectra of reduced sample evacuated at 773 K and 573 K (
Figure 11A, spectra c and d, respectively) clearly shows that the components around 2133 and 2096-95 cm
-1 consumed during the fast oxidation at 100 K are much more intense with the highly dehydroxylated sample and therefore should be associated with Ce
3+ sites having no OH groups in vicinity. The same seems to be also valid for the band at 2105 cm
-1. In contrast, the band at 2109 cm
-1 appears with enhanced intensity with the hydroxylated sample and thus can be associated with Ce
3+ cations connected with the extra OH groups on this sample (3664 cm
-1).
On the basis of the above considerations one could expect that Ce3+ cations bound on residual carbonates should also possess a specific spectral behavior. Unfortunately, on the basis of our experiments, we are not able to draw any definite conclusions at this stage.
Comparison between the samples reduced at different temperatures (
Figure 11A, spectra a-c) clearly shows that the component at 2126 cm
-1 corresponds to Ce
3+ sites that are produced more difficult during reduction.
The sites that resist fast oxidation at 100 K but are oxidized at higher temperature up to 293 K give rise to a broad Ce3+ band with two resolved components at 2118 and 2112 cm-1.
Finally, the small fraction of sites residual to oxidation at 293 K produce a broad band at 2109 cm-1. Since the band does not differ significantly from the above discussed band, we could suggest that the inertness of these sites could be due to low accessibility. It is not excluded they to be in the subsurface layer.
At the beginning of this study we aimed to establish a clear relationship between the band components and the exposed crystal facets. However, it appears that the positions of the components depend on too many factors and at this stage we desist to make definite conclusions. Further specially designed experiments are necessary to answer this question and to establish eventual dependence between the component position and location of the Ce3+ on different crystal planes and edges.