Open Access Article
Theocharis Kentriab,
Paraskevas Dimitropoulosa,
Konstantina Niavia,
Eleana Kordoulic and
Soghomon Boghosian
*abd
aDepartment of Chemical Engineering, University of Patras, Patras, Greece. E-mail: bogosian@chemeng.upatras.gr
bInstitute of Chemical Engineering Sciences, FORTH/ICE-HT, Patras, Greece
cDepartment of Chemistry, University of Patras, Patras, Greece
dSchool of Science and Technology, Hellenic Open University, GR-26335 Patras, Greece
First published on 1st May 2026
In situ Raman and FTIR spectroscopy, the former complemented by 18O/16O exchange, are used to unravel the structural and configurational properties of the (MoOx)n phase dispersed on two TiO2 polymorphs (anatase and Degussa P25) at the temperature range of 430–120 °C and Mo surface density in the range of 0.5–5 Mo per nm2 under oxidative dehydrated conditions. The dispersed (MoOx)n phase supported on titania is heterogeneous; at coverages below ca. 1 Mo per nm2, isolated species prevail. Under dehydrated conditions, three MoOx species occur on titania in either mononuclear or polynuclear form depending on the temperature and coverage: (i) Species-I with a tetrahedral-like mono-oxo configuration, O
Mo(–O–Ti)3 with νMo
O = 996–999 cm−1; (ii) Species-II with a pyramidal-like mono-oxo configuration, O
Mo(–O–Ti)4 with νMo
O = 989–993 cm−1; and (iii) Species-III with a di-oxo termination configuration with νs/νas = 980–983/965–971 cm−1. Species-I is formed with the first order of priority and prevails at low coverages (<1 Mo per nm2), while its formation ceases at higher coverages. Species-II prevails at coverages of and above 1 Mo per nm2, while it constitutes the building unit of the associated polynuclear (MoO5)n domains at coverages higher than 2 Mo per nm2. Temperature cycling in the 430 °C → 250 °C → 175 °C → 120 °C → 430 °C sequence results in a reversible temperature-dependent Species-II ↔ Species-III transformation, mediated by the surface-retained water molecules. Species-II exhibits higher reactivity than Species-I, both with respect to surface-retained water molecules and hydrogen; the latter is judged from its subjection to facile 18O/16O exchange. These results are important for tuning the configuration of dispersed MoOx sites on titania and designing MoOx/TiO2 catalysts at the molecular level.
Significantly, the typical conditions chosen in experimental in situ spectroscopic studies of supported transition metal oxides reflect the so-called oxidative dehydration state, i.e. the presence of O2(g) to ensure the occurrence of the transition metal in its higher oxidation state and without the presence of H2O(g) in the feed gas.7,8,18–32,49–52 Additionally, it has often been postulated without sound pertinent experimental evidence that the prevailing MOx configurations obtained after the calcination of supported transition metal oxide catalysts are solely driven by thermodynamic constraints irrespective of the synthesis protocol and that they do not revert when temperature is lowered under dehydrated conditions.20,21,23,25–31,53–57 However, unprecedented reports demonstrating a reversible temperature dependence of the prevailing species for the dispersed WOx and VOx phases on TiO2 (ref. 7, 8, 58 and 59) as well as dispersed ReOx on TiO2 and ZrO2 (ref. 7, 8, 60 and 61) have controverted the above view, while it has been shown that the synthesis route can affect the speciation of the dispersed MOx phase, enabling catalyst design when synthesis methods based on molecular approaches have been followed.22,62–68 Despite the underestimation of the heterogeneity issue for the dispersed transition metal oxide phase, i.e. the co-existence of distinct species with different structures (e.g. pyramidal and tetrahedral) or termination configurations (e.g. mono-oxo and di-oxo), several paradigms of dispersed MOx phase heterogeneity on oxidic supports have been reported.2,7,8,69–75
The comprehensive exploration of the molecular structure and termination configuration of dispersed oxo-metallic phases requires the deployment of the full arsenal of molecular vibrational spectroscopy, including in situ Raman and FTIR spectroscopies complemented by 18O/16O isotope exchange studies.18,19,29 The absence of long-range order within the dispersed MOx phases makes molecular vibrational spectroscopy particularly suitable for studying the structural properties of the dispersed MOx phases. Hence, we take the view that the controversy of pre-2010 studies is to be identified in a number of deficiencies, including one or more of the following shortcomings: (i) applying only one type of vibrational spectroscopic method (i.e. either Raman or FTIR) without isotope exchange studies; (ii) overlooking the effect of coverage, e.g. by studying one single sample; (iii) omitting to investigate the temperature dependence of the dispersed phase speciation; and (iv) recording spectra after cooling at room temperature.
The heterogeneity of the MoOx phase dispersed in titania has recently been ascertained for low-loaded MoOx/TiO2(P25) catalysts.7 The aim of the present work is to explore the temperature and coverage effects on the speciation of the dispersed MoOx phase by determining the number of species present as well as their relative presence depending on temperature and coverage under dehydrated conditions. To this end, in situ molecular vibrational spectroscopies (Raman, FTIR), the latter in the overtone Mo
O stretching region, complemented by in situ Raman-18O/16O isotope exchange studies and Raman spectroscopy under forced dehydrated static equilibrium conditions8,58,59 have systematically been deployed. This study is performed using two titania polymorphs as support materials (anatase and Degussa P25) in the temperature range of 430–120 °C and surface coverage of 0.5–5 Mo per nm2. Finally, based on the vibrational selection rules and isotope effects, a differentiation between the termination configurations of the prevailing species is undertaken.
| Catalysts | ns (Mo per nm2) | Loading (wt% Mo) | SBET (m2 g−1) | CMo(VI) (M) | Support |
|---|---|---|---|---|---|
| 0.52MoTiO2(P25) | 0.52 | 0.4 | 47 | 8.4 × 10−4 | P25 |
| 1.3MoTiO2(P25) | 1.3 | 0.96 | 48 | 2.1 × 10−3 | P25 |
| 1.9MoTiO2(P25) | 1.9 | 1.4 | 48 | 3 × 10−3 | P25 |
| 2.9MoTiO2(P25) | 2.9 | 2.2 | 49 | 4.7 × 10−3 | P25 |
| 3.7MoTiO2(P25) | 3.7 | 2.9 | 49 | 6 × 10−3 | P25 |
| 4.3MoTiO2(P25) | 4.3 | 3.4 | 49 | 7.2 × 10−3 | P25 |
| 0.55MoTiO2(a) | 0.55 | 1.1 | 123 | 2.25 × 10−3 | Anatase |
| 1.1MoTiO2(a) | 1.1 | 2.2 | 120 | 4.5 × 10−3 | Anatase |
| 2.1MoTiO2(a) | 2.1 | 3.9 | 117 | 8.1 × 10−3 | Anatase |
| 2.7MoTiO2(a) | 2.7 | 6.0 | 115 | 1.0 × 10−3 | Anatase |
| 3.7MoTiO2(a) | 3.7 | 7.7 | 101 | 1.3 × 10−2 | Anatase |
| 4.9MoTiO2(a) | 4.9 | 9.2 | 100 | 1.6 × 10−2 | Anatase |
The specific surface area, SBET, of the calcined catalysts was measured by N2 adsorption/desorption as described before.67 The coverage for each catalyst sample, ns, in terms of Mo atoms per nm2 (Mo surface density) was calculated from the respective SBET and Mo wt%, and the obtained results are shown in Table 1, which compiles the catalyst characteristics. The catalyst samples are denoted as xMoTiO2(P25) and xMoTiO2(a), as shown in Table 1, where the prefix x stands for the respective Mo surface density in Mo per nm2, which is calculated using the formula as follows:
For each sample, the recording of Raman spectra started at 430 °C after 1 h of treatment under oxidative dehydrated feed conditions, namely 20% O2/He at a flow of 30 cm3 min−1. Helium and oxygen gases (99.999%) were obtained from Linde, and the feed gas mixture was sent through molecular sieve traps to remove eventual traces of humidity. The temperature was subsequently lowered to 250 °C, 175 °C and 120 °C, and in situ Raman spectra under flowing 20% O2/He were obtained after allowing the sample to attain steady state for 1 h and 30 min at each temperature. The temperatures were chosen to span the well-established temperature window of anatase as a support material (T < 480 °C) and an adequate number of values (i.e. 430 °C, 250 °C, 175 °C and 120 °C) to study the temperature dependence of the molecular structure. The sample was then heated in the in situ cell at 430 °C under flowing 20% O2/He, and the reinstatement of its initial structure was verified by recording the in situ Raman spectra after 1 h of treatment. The specific sequence of temperatures was not relevant to the reproduction of the Raman spectrum at a certain temperature. Hence, using an alternative sequence of temperatures (e.g. 430 °C → 120 °C → 175 °C → 250 °C or 250 °C → 430 °C → 120 °C → 175 °C), the in situ Raman spectrum could be reproduced at each temperature. The resolution (spectral slit width) was set to 7 cm−1 to enhance the signal, and a slow scanning protocol of 1.2 s photon counting per point in increments of 0.25 cm−1 was followed to achieve an adequate signal-to-noise ratio. Hence, a 1.5 h duration was necessary for each recording. Furthermore, to control and maintain the measurement precision within ±0.5 cm−1, the emission lines of a Ne lamp were recorded in the spectral region of interest to correct for eventual monochromator drifts. To account for the so-called “path length” effect caused by the Mo surface density variation in the 0.5–5 Mo per nm2 range, the obtained Raman spectra were subjected to an earlier described procedure of normalisation.8,80
O fundamental modes. In situ FTIR spectra were also obtained under the same conditions, i.e. flowing (30 cm3 min−1) 20% O2/He mixture, for the TiO2(anatase) and TiO2(P25) support materials at each recording temperature. The spectra obtained for the net supports were subtracted from the counterpart in situ FTIR spectra obtained for the samples, thereby resulting in situ difference FTIR spectra pertaining, in each case, to the dispersed (MoOx)n phases of the catalyst samples. Notably, the penetration depth and scattering properties depend on the packing density, resulting in different overall intensities. Hence, the spectra obtained for each support material at each temperature had to be scaled to match the spectrum obtained for each MoOx/TiO2 sample at the same temperature to produce a difference corresponding to the dispersed phase alone.The concept of static equilibrium Raman measurements in sealed quartz cells has been described elsewhere.58,59,81 The quartz cell, shown in Fig. 1, comprises a 2–3 cm long main compartment with 20 mm o.d., a ∼2 cm long appendix (6 mm o.d.) for containing the catalyst powder and a 6 mm o.d. stem. Around 50 mg of each catalyst was added into the cell, which was then attached to a vacuum/gas-addition line. A cylindrical core furnace was then mounted around the cell and heated to 200 °C, and the cell was subjected to dynamic vacuum (∼10−4 bar) for 1 h while keeping the trap of the vacuum line immersed in liquid nitrogen to condense any water forcibly removed from the catalyst sample. The valve connecting to the vacuum pump was then closed, and the furnace surrounding the sample was removed. Oxygen gas (Linde, 99.999%) was then admitted to the vacuum line and allowed to condense in the liquid nitrogen trap, thereby establishing an oxygen pressure of pO2 = 0.19 bar, i.e. the vapor pressure of oxygen at 77 K. Subsequently, oxygen gas contained in a known volume was condensed in the cell appendix by surrounding the cell bottom with liquid nitrogen, and the cell was afterwards sealed with a propane–oxygen torch, as shown in Fig. 1(B). Fig. 1(C) shows an actual photograph of a sealed cell, which has an oxygen pressure of pO2,298 K = ∼1.0 bar. The ratio of O2 molecules to the Mo moles contained in the cell was in the 40–65 range, thereby ensuring that Mo remains in the oxidation state VI. Results are reported from “static” cells made for the representative low coverage 1.3MoTiO2(P25) and 1.1MoTiO2(a) catalyst samples.
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| Fig. 1 (A) Schematic of the glass assembly used for sealing quartz cells containing catalyst powder under an oxygen atmosphere. (B) Photograph of the quartz cell immersed in liquid nitrogen, for condensing the oxygen gas added in the line, and propane–oxygen torch sealing the cell. (C) Picture of a quartz cell with a bottom appendix containing the catalyst powder and oxygen gas. Reproduced from ref. 59, with permission from the Royal Society of Chemistry. | ||
The optical furnace used for obtaining Raman spectra under static equilibrium has been described before.81,82 The 532.0 nm green line of a Spectra Physics Excelsior DPSS laser was used as the excitation source, and the scattered light was collected in a 90° horizontal geometry. The laser power was ∼20 mW on the sample. Rayleigh scattering was rejected by an edge filter. The monochromator (with a resolution set at 2 cm−1) used was an IHR-320 JY (ISA–Horriba Group) coupled to a CCD detector cooled to −56 °C and interfaced with the Labspec software. Raman spectra were recorded at a sequence of decreasing temperatures in the 430–120 °C range, and the reinstatement of the initial catalyst structure was confirmed by reproducing the Raman spectrum at 430 °C. The quartz cells containing the samples were allowed to reach equilibrium for 1 h and 30 min at each temperature.
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| Fig. 3 MoOx/TiO2(anatase) with a surface density of 1.1 Mo per nm2. (A–C) same as the caption to Fig. 2(D) Peak analysis of the sequential (430 °C → 250 °C → 175 °C) Raman spectra at a static equilibrium under pO2,300 K = 1.1 atm after subtracting the corresponding spectrum of bare TiO2(anatase). Laser wavelength, λ0 = 532.0 nm, laser power, w = 20 mW; and resolution = 2 cm−1. | ||
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| Fig. 4 MoOx/TiO2(P25) with a surface density of 0.52 Mo per nm2. (A–C) same as the caption to Fig. 2. | ||
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| Fig. 5 MoOx/TiO2(P25) with a surface density of 0.52 Mo per nm2. (A–C) same as the caption to Fig. 2. (D) peak analysis of the sequential (430 °C → 250 °C → 175 °C) Raman spectra at a static equilibrium under pO2,300 K = 1.3 atm after subtracting the corresponding spectrum of bare TiO2(anatase). Recording parameters of the spectra: same as caption to Fig. 3(D). | ||
The Raman spectra, having been subjected to a sound normalization procedure (see Experimental section), provide a consistent set of data for quantitative exploitation. Additionally, the subtraction of the bare TiO2(anatase or P25) in each case results in a baseline-corrected net difference spectrum assigned to the dispersed (MoOx)n phase, which is suitable for peak analysis. The fitting was performed using the nonlinear regression method based on the previously described85 Levenberg–Marquardt algorithm. The in situ FTIR spectra shown in Panels (C) of Fig. 2–5 are used to exploit the relative band intensities that complement the counterpart temperature dependence of the in situ Raman spectra.
The Mo
O stretching regions of the in situ Raman spectra shown in Fig. 2(A)–5(A) seemingly exhibit at 430 °C a single band feature that appears to possess more than one component, of which the one at the highest wavenumber is denoted as band (I). A second component, denoted as band (II), is discerned in the immediate lower wavenumber position that loses intensity relative to its high wavenumber counterpart band (I) with lowering of the temperature, while at the same time, a third feature (band (III), already existing at an even lower wavenumber but still within the Mo
O stretching region, emerges and grows at the expense of the intermediate wavenumber component, band (II). Lowering of component (II) is discerned in the 430 °C → 250 °C step together with the strengthening of component (III), while at 175 °C and 120 °C, band (II) is obscured by the high wavenumber wing of component (III). Significantly, feature (III) appears to consist of two components, as evidenced by the fact that their mutual relative intensities are maintained constant with varying temperatures. The positions of band (I)–(III) vary slightly depending on coverage and TiO2 polymorph and are found based on the peak analysis procedure as follows: 996–999 cm−1 for band (I); 989–993 cm−1 for band (II); and 980–983/965–971 cm−1 for the two components of band (III).
The evidence for the above effects is fully justified and further strengthened by the in situ FTIR spectra shown in panels (C) of Fig. 2–5. The in situ FTIR spectra are obtained in the first overtone region of the Mo
O stretching modes; hence, not only are the band wavenumbers approximately doubled but most importantly their mutual distances are also doubled, thereby enabling better discernment of the occurrence of the above-mentioned modes and their assignment to discrete species. Notably, the improvement of the separation between the observed bands in the overtone region does not reveal the occurrence of any further bands; hence, it appears that three species are present, of which the relative presence is temperature dependent. When lowering the temperature from 430 °C to 250 °C, band (II) is diminished, thereby allowing for a clear resolution of band (I), while further temperature lowering results in the simultaneous strengthening of the two components of band (III) at the expense of band (II). Hence, bands (I) and (II) are due to distinct sites, each possessing a single terminal Mo
O bond, hereinafter named Species-I and Species-II. Additionally, the double band (III) is due to a site possessing two Mo
O terminal bonds, i.e. a di-oxo site, named Species-III. Fig. 6 depicts the proposed structural models for Species-I, Species-II and Species-III in isolated/monomeric form. Species-I and Species-II presumably possess mono–oxo termination configurations, judged from the occurrence of one single Mo
O stretching mode in the vicinity of 1000 cm−1,19 while Species-III takes on a di-oxo configuration in full conformity with the expected possession of symmetric and antisymmetric stretching modes (νs, νas) in the lower region of the Mo
O stretching range, i.e. below 1000 cm−1 at a mutual distance of 10–40 cm−1 (νs > νas) with the νs mode exhibiting a higher Raman intensity compared to its νas counterpart.19,86,87 According to the spectral data displayed in Fig. 2(C)–5(C), the positions of the first overtones of bands (I)–(III) are 1976–1982 cm−1 for band (I), 1963–1966 cm−1 for band (II), and 1942–1949/1925–1935 cm−1 for the two components of band (III).
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| Fig. 6 Molecular structural models and Mo coordination/termination characteristics for Species-I, Species-II and Species-III in mononuclear representations. Reproduced from ref. 58, with permission from the Royal Society of Chemistry. | ||
Previously, both pyramidal-like, with five-fold coordination for Mo(CNMo = 5), and tetrahedral-like (CNMo = 4) configurations have been proposed for the mono-oxo O
Mo(–O–Ti)x sites dispersed on titania.7,8,17–21,23,25,30,31,83,88 The data in Fig. 2–5 strongly suggest the simultaneous occurrence of both types with relative presence controlled by temperature and coverage. In particular, Species-I with its νMo
O mode at 996–999 cm−1 takes on an O
Mo(–O–Ti)3 tetrahedral-like mono-oxo configuration, while Species-II with its νMo
O mode at 989–993 cm−1 takes on a O
Mo(–O–Ti)4 mono-oxo pyramidal-like arrangement. The wavenumber of a terminal Mo
O stretching mode is not governed solely by the termination configuration (e.g. mono-oxo Mo
O and di-oxo Mo(
O)2) but also by the Mo coordination number and ligand environment. In the case of the O
MoVI(–O–)3 and O
MoVI(–O–)4, where the sole difference pertains to the number of oxide ligands, it turns out that, according to the valence sum rule, for a total of 6 v.u., the distribution of bond orders among a large number of bonds results in a lower wavenumber for the Mo
O terminal stretching for O
MoVI(–O–)4, where Mo exhibits a five-fold coordination, compared to the respective wavenumber for the O
MoVI(–O–)3 species.79,89 Hence, the higher wavenumber position for νMo
O,Species-I compared to νMo
O,Species-II is fully justified by the lower Mo coordination number for Species-I. As discussed below, at higher Mo coverages, the structural units shown in Fig. 6 occur at adjacent sites and may undergo association (polymerisation) to form larger domains through the formation of Mo–O–Mo and O–Mo–O bridges (vide infra). Moreover, with reference to the above documented temperature-dependent Species-II ↔ Species-III interconversion, the following, previously justified,8,58,59,61 mechanistic scheme is proposed, accounting for the observed temperature-dependent behaviour of the in situ vibrational spectra (Fig. 2–5).
Fig. 7 portrays the above mechanistic scheme using the proposed molecular models for Species-II and Species-III. Very briefly, the mechanism involves water molecules, which are formed during the impregnation step of the surface hydroxyl titration and retained at the first layer of the support by H-bonds63,90,91 that are activated by lowering the temperature, thereby resulting in hydrolysis of anchoring Mo–O–Ti sites and subsequent surface hydroxylation and, in turn, dehydration and dehydroxylation/deprotonation upon heating. This effect is, by nature, expected to occur to a lower extent at high Mo coverage, where fewer surface hydroxyls and vacant deprotonated (Ti–O–) sites are available (vide infra).
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| Fig. 7 Effect of temperature on the MoOx species: (A) Species-I remaining stable in the 430–120 °C range; and (B) mechanism of the Species-II ↔ Species-III temperature-dependent reversible transformation. Reproduced from ref. 58, with permission from the Royal Society of Chemistry. | ||
The wavenumbers of the νs/νas pair for a dioxo MoO2 core surrounded by O ligands also depend on the coordination number of Mo. Hence, compared to (O
)2Mo(–O–Ti)3 Species-III (Fig. 6) with CNMo = 5, the known reference model compounds MoO2(SO4)22− and MoO2(SO4)34− possessing MoO2 dioxo cores and Mo in six-fold MoO6 coordination exhibited their νs/νas pairs at 957/918 and 935/895 cm−1, respectively,87 i.e. with a wavenumber downshift, justified by the high Mo coordination number.
At this point, it is worth mentioning that the principles and criteria for the peak analysis results shown in Fig. 2–5 panels (B) are as follows:
(i) A minimum number of bands to fit the Mo
O stretching region;
(ii) The occurrence of four bands originating from three species, as evidenced from the in situ Raman and FTIR spectra: (a) one band due to Species-I at the highest wavenumber position; (b) one band due to Species-II located at 5–6 cm−1 lower compared to its Species-I counterpart; and (c) two bands due to Species-III located at a mutual distance of 10–40 cm−1, corresponding to the νs/νas pair (with Iνs > Iνas and fixed Iνs/Iνas ratios, where I denotes the band intensity) for a di-oxo species;
(iii) fixed band widths and wavenumber positions (allowing ±1 cm−1 for measurement precision) for each sample;
(iv) Larger widths for the di-oxo terminal stretching modes compared to their mono-oxo counterparts.
The validity of the assignments made for bands (I) and (II) can be verified by exploiting the vibrational selection rules of anharmonicity at the diatomic approximation.86,92 Table 2 compiles the observed band wavenumbers for the νMo
O,1←0,R Raman fundamentals and νMo
O,2←0,IR IR first overtones for the mono-oxo Species-I and Species-II as well as the νs/νas Raman fundamentals and IR first overtones for the di-oxo Species-III. In the diatomic approximation, the observed vibrational fundamentals and first overtones for the mono-oxo species should comply with the following expressions:
νMo O,1←0 = ωMo O(1 − 2χMo O),
| (1) |
νMo O,2←0 = 2ωMo O(1 − 3χMo O),
| (2) |
O and χMo
O denote the primary (zero-order) wavenumber (corrected for anharmonicity) and the anharmonicity constant, respectively. Hence, the vibrational energy states are not equidistant, and the first overtone is expected at a wavenumber slightly below the doubled observed Raman fundamental,92 as is the case with the pertinent data compiled in Table 2. Moreover, the assignments of bands (I) and (II) to mono-oxo terminal stretches in the fundamental and first overtone regions, respectively, of the in situ Raman and FTIR spectra are confirmed by the reasonable calculated values for χMo
O (0.007–0.009, see Table 2) based on eqn (1) and (2).
| Sample | Species-I, mono-oxo O Mo(–O–Ti)3 |
Species-II, mono-oxo O Mo(–O–Ti)4 |
Species-III, di-oxo (O )2Mo(–O–Ti)3 |
O–Re–O | |||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| ν1←0, R | ν2←0, IR | χMo Oa |
ν1←0, R | ν2←0, IR | χMo Oa |
νs,1←0, R | νas,1←0, R | νs,2←0, IR | νas,2←0, IR | ||
| a anharmonicity constants, calculated based on eqn (1) and (2). | |||||||||||
| 0.55MoTiO2(a) | 997 | 1977 | 0.008 | 992 | 1966 | 0.009 | 982 | 969 | 1942 | 1928 | ∼925 |
| 1.1MoTiO2(a) | 999 | 1982 | 0.008 | 993 | 1967 | 0.009 | 983 | 971 | 1949 | 1935 | ∼930 |
| 0.52MoTiO2(P25) | 996 | 1976 | 0.008 | 989 | 1963 | 0.007 | 980 | 963 | 1942 | ∼1925 | — |
| 1.3MoTiO2(P25) | 997 | 1980 | 0.007 | 991 | 1966 | 0.008 | 981 | 965 | 1942 | ∼1925 | ∼925 |
The in situ Raman and FTIR results for the low coverage MoOx/TiO2(anatase, P25) catalysts in the 0.5–1.3 Mo per nm2 range are adequate for a preliminary discussion of the coverage effect. Significantly, vibrational spectra of low coverage catalysts do not “suffer” from the effects of vibrational coupling because extant MoOx sites occur primarily in isolated forms, thereby resulting in quite clear spectroscopic signatures pertaining to distinct configurations. Hence, the data in Fig. 2–5 are adequate to suggest that with increasing coverage from ∼0.5 to ∼1.2 Mo per nm2, Species-I presence remains stable, while Species-II presence significantly increases. Notably, at very low coverage of ∼0.5 Mo per nm2, O
Mo(–O–Ti)3 (Species-I) and O
Mo(–O–Ti)4 (Species-II) occur to comparable extents on anatase (Fig. 2), while Species-I prevails over Species-II on P25 (Fig. 4). When the coverage is increased to 1.1–1.3 Mo per nm2, Species-II clearly prevails over Species-I on both titania polymorphs. It is thus evident that the formation of Species-I occurs in the initial stage of the impregnation step through the titration of most basic hydroxyl sites. Once the most basic hydroxyl receptors are titrated, the formation of Species-II follows. This is in agreement with the higher abundance of high basicity surface hydroxyls on P25 compared to anatase.58,91 Moreover, as already mentioned, it is evident that Species-II is favoured at high temperatures, while with temperature lowering, Species-II transforms to Species-III, as shown in Fig. 7.
While at low Mo coverage (i.e. ≤1.3 Mo per nm2) the majority of the dispersed MoOx sites occur in isolated/monomeric form, formation of associated/polymeric (MoOx)n sites is also observed and in fact to different extents on the two TiO2 polymorphs. Hence, the broad features observed in the 850–950 cm−1 regions in the in situ Raman spectra shown in panels (A) of Fig. 2–5 are due to Mo–O–Mo and/or O–Mo–O functionalities.19,25,30,83,93 Evidently, a variation of related configurations involving Mo–O–Mo bridges within the dispersed amorphous (MoOx)n phase gives rise to multiple overlapping O–Mo–O and Mo–O–Mo functionalities and vibrational couplings thereof, resulting in a broad continuum in the pertinent region of the Raman spectra. Interestingly, a lower extent of association is evidenced for the TiO2(P25)–supported catalysts, as evidenced by comparing the in situ Raman spectra shown in Fig. 1(A) and (B) pertaining to the 0.55 Mo per nm2 MoOx/TiO2(a) with the corresponding in situ Raman spectra shown in Fig. 3(A) and (B) pertaining to the 0.52 Mo per nm2 MoOx/TiO2(P25) sample. Fig. S1 (SI) shows two examples of superpositions of spectra obtained for bare TiO2(anatase) at 175 °C and 250 °C on the corresponding spectra obtained for 1.1 Mo per nm2 MoOx/TiO2(anatase), substantiating the occurrence of a broad continuum in the 850–950 cm−1 region, which is ascribed to bridging Mo–O–Mo and/or O–Mo–O modes. The effect of coverage is further discussed below, in a separate section (vide infra).
18O)n modes.Based on an assumption for a strictly quadratic potential for the Mo
O site in a diatomic harmonic oscillator approximation, the 18O/16O substitution on the terminal Mo
16O site results in a so-called isotopic ratio given by the following formula:86,92
![]() | (3) |
For the Mo
O diatomic harmonic oscillator, the isotopic ratio equals 1.0513.
Assuming the most general quadratic potential functions, the theory of vibrational isotope effects shows that for the symmetric stretching ν1 and ν2 modes of a non-linear symmetric XY2 molecule (i.e. such as the triatomic di-oxo Mo
O2 moiety) the
ratio, where
and
pertain to the isotopically substituted XY(i)2 molecule (e.g. Mo
18O2), is independent of the potential constants and of the molecular angle. Moreover, for the case of the di-oxo MoO2 unit this ratio can theoretically be calculated equal to 1.052.95 Notably, DFT calculations on the (16O
)2Mo(–16O–Si)2 → (18O
)2Mo(–18O–Si)2 isotopic substitution resulted in a
isotopic ratio of 1.0517,33 which is identical to the isotopic ratio of 1.0513, as previewed for the diatomic Mo
O mono-oxo termination, based on eqn (3). Hence, one cannot differentiate between mono-oxo and di-oxo arrangements based solely on the isotopic shift value. In spectroscopically well-documented di-oxo Re(
O)2 termination configurations for ReOx dispersed on TiO2,60 CeO2 (ref. 74) and ZrO2,61 it has been shown that the observed isotopic shifts were not adequate to differentiate between mono-oxo and di-oxo termination configurations.
Fig. 8 shows the sequential in situ Raman spectra obtained for the low-coverage 0.52 and 1.3 Mo per nm2 TiO2(P25)-supported catalyst at 430 °C after 18O/16O exchange cycles, as indicated by each spectrum. Each 18O/16O exchange cycle consists of a reduction step under flowing 5% H2/He and a re-oxidation step under flowing 2% 18O2/He (see Experimental section). In situ Raman-18O/16O isotope exchange studies on MoOx/TiO2(anatase) have earlier been reported83 and will not be repeated here.
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| Fig. 8 MoOx/TiO2(P25) with surface densities of (A) 0.52 Mo per nm2 and (B) 1.3 Mo per nm2. In situ sequential Raman spectra obtained under flowing 2% 18O2/He after subsequent H2/18O2 reduction/oxidation isotope substitution cycles, as indicated by each spectrum. Recording parameters: same as the caption to Fig. 2(A). | ||
The isotopic splitting pattern for each sample, i.e. for 0.52 Mo per nm2 in Panel Fig. 8(A) and for 1.3 Mo per nm2 in Panel Fig. 8(B), primarily characterizes the termination configuration of the prevailing MoOx species in each case, i.e. Species-I (O
Mo(–O–Ti)3) for 0.52MoTiO2(P25) and Species-II (O
Mo(–O–Ti)4) for 1.3MoTiO2(P25). Notably, in both cases, single splitting is observed, i.e. a gradual evolution of one single band due to Mo
18O stretching, thereby corroborating the validity of the proposed mono-oxo termination configuration for both Species-I and Species-II. Notably, Species-II undergoes a more facile 18O/16O exchange of its terminal Mo
16O site, as evidenced by comparing the spectral sequences at Panels 8(A) and 8(B) after, e.g., 3, 5 and 10 18O/16O exchange cycles.
As previously observed for dispersed O
M(–O–Ti)n mono-oxo species (M = Mo, W, and V),58,59,83 with an increasing number of 18O/16O exchange cycles, a gradual red shift is observed for the M
16O mode of the non-substituted terminal sites. The observed red shift has been attributed to a gradual 18O/16O substitution of the anchoring 16O atoms that are next-nearest-neighbours to the terminal O atoms,19,83 i.e. 16O
Mo(–16O–Ti)n → 16O
Mo(–16O–Ti)n−1(–18O–Ti) → 16O
Mo(–16O–Ti)n−2(–18O–Ti)2. Importantly, the red shift of Mo
16O is clearly discerned from the 3rd 18O/16O exchange cycle for the 1.3 Mo per nm2 sample depicted in Fig. 8(B), thereby pointing to a more facile Mo–16O–Ti → Mo–18O–Ti exchange for Species-II compared to Fig. 8(A), which pertains to the 0.52 Mo per nm2 sample in which Species-I is the prevailing species.
DFT theoretical calculations44 showed that dissociative adsorption of hydrogen occurs favourably on unsaturated Ti–O–Ti and deprotonated Ti–O hydroxyl sites, thereby guiding the initial steps of 18O/16O exchange on lattice O atoms and thereafter by subsequent surface diffusion to anchoring O atoms (Mo–16O–Ti → Mo–18O–Ti). The lower nuclear charge of 18O causes a cascade effect, which weakens the non-substituted Mo
16O bond, thereby justifying the observed red shifts in Fig. 8 (992 cm−1 → 990 cm−1 for 0.52MoTiO2(P25) and 993 cm−1 → 989 cm−1 for 1.3 MoTiO2(P25)).
Hence, it turns out that both the terminal and the anchoring O atoms of the pyramidal-like O
Mo(–O–Ti)4 Species-II undergo a more facile 18O/16O exchange compared to the tetrahedral-like O
Mo(–O–Ti)3 Species-I.
It should finally be pointed out that the results of the in situ Raman-18O/16O isotope exchange studies on MoOx/TiO2(P25) are in full agreement with the previously reported83 pertinent results for the MoOx/TiO2(anatase) counterpart system.
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| Fig. 9 Effect of coverage for the MoOx/TiO2(anatase) catalysts in the 0.55–4.9 Mo per nm2 range under flowing 20% O2/He at 430 °C. (A) In situ Raman spectra. Recording parameters: same as the caption to Fig. 2(A). (B) In situ FTIR spectra. | ||
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| Fig. 10 Effect of coverage for the MoOx/TiO2(anatase) catalysts in the 0.55–4.9 Mo per nm2 range under flowing 20% O2/He at 175 °C. (A) In situ Raman spectra. Recording parameters: same as the caption to Fig. 2(A). (B) In situ FTIR spectra. | ||
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| Fig. 11 Effect of coverage for the MoOx/TiO2(P25) catalysts in the 0.52–4.3 Mo per nm2 range under flowing 20% O2/He at 430 °C. (A) In situ Raman spectra. Recording parameters: same as the caption to Fig. 2(A). (B) In situ FTIR spectra. | ||
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| Fig. 12 Effect of coverage for the MoOx/TiO2(P25) catalysts in the 0.52–4.3 Mo per nm2 range under flowing 20% O2/He at 175 °C. (A) In situ Raman spectra. Recording parameters: same as the caption to Fig. 2(A). (B) In situ FTIR spectra. | ||
With increasing coverage, band (II) attributed to Species-II grows in intensity and gradually obscures band (I) attributed to Species-I, of which the normalised intensity remains constant, thereby corroborating the observations pertaining to the low coverage samples (vide ante, Section 3.1, Fig. 2–5). Hence, the formation of the tetra-coordinated mono-oxo O
Mo(–O–Ti)3 Species-I precedes the formation of the penta-coordinated mono-oxo O
Mo(–O–Ti)4, which continues to form at higher concentrations of the precursor slurries. The gradual prevalence of Species-II over Species-I is best discerned in the in situ FTIR spectra (panels Fig. 9(B)–12(B)), where the band separation is nearly doubled in the overtone region. Importantly, the prevalence of Species-II over Species-I with increasing ns is also demonstrated for low coverage samples based on the peak analysis results shown in Fig. 2–5 (vide ante).
Additionally, with increasing coverage, band (II) attributed to Species-II gradually receives a high-wavenumber component that progressively prevails over its low-wavenumber counterpart, thereby resulting in a blue shift for the convoluted envelope of band (II). Notably, the pertinent blue shifts observed with increasing coverage in the in situ FTIR spectra in each case shown in Figure 9(B)–12(B) are approximately double compared to the respective shifts in the corresponding in situ Raman spectra in Figure 9(A)–12(A), obtained in the fundamental stretching region. Concomitantly, alongside the blue-shifting tendency of the band (II) envelope, a broad peak mass gradually emerges with increasing coverage in the in situ Raman spectra shown in Fig. 9(A)–12(A) and Fig. S2(A) and S3(A). The broad peak mass emerges at surface densities ns > 1 Mo per nm2 for the samples supported on TiO2-anatase (Fig. 9(A) and 10(A)) and at ns > 2 Mo per nm2 for the TiO2(P25)-supported samples (Fig. 11(A) and 12(A)) and gradually expands, seemingly consisting of several contributions, to fill the ca. 880–940 cm−1 range. The wavenumber location and gradual increase in the broad 880–940 cm−1 feature's intensity relative to the terminal Mo
O band intensity with increasing coverage are evident for Mo–O–Mo or O–Mo–O provenance. These bridging modes occur within associated (polymeric) (MoOx)n domains, of which the formation and growth are favoured with increasing coverage and can be subject to vibrational coupling86 to each other as well as to anchoring Mo–O–Ti modes, thereby accounting for the observed band overall broadness.
Hence, at low surface densities, i.e. ns < 1 Mo per nm2, Species-II with penta-coordinated Mo occurs mainly in isolated (monomeric) form, while at high coverages, it constitutes the building unit for the larger associated polymolybdate (MoOx)n domains. The gradual blue shift of the terminal νMo
O,Species-II mode, observed with increasing coverage (Fig. 9–12), is justified as follows. When the concentration CMo(VI) in the precursor slurries is increased, more support hydroxyls with progressively lower basicity are gradually titrated during the impregnation step, thereby resulting in lower electron donating abilities of O along Ti–O–Mo anchors and – by cascade effect – to slightly stronger terminal Mo
O bonds.
Previously, in agreement with the present proposed structural properties, density functional theory (DFT) calculations concluded that a distorted tetrahedral C3ν-like mono-oxo arrangement, i.e. Species-I, is the prevailing configuration for dispersed molybdena at very low coverage on TiO2-anatase.96 In particular, Species-I was found to occur on the most stable (101) anatase facet, while di-oxo Species-III was found to occur to a low extent on the minority (001) facet.96 Moreover, DFT calculations suggest that with increasing coverage the mono-oxo termination configuration is preserved in species with increased nuclearity (i.e. polymeric domains) and that the coordination number of Mo is increased from 4 to 5,44,97 in full agreement with the results of the present work. Moreover, experimental LIII–XANES work on anatase-supported molybdena provided evidence supporting the occurrence of penta-coordinated mono-oxo Mo in polymeric form for samples with high coverage.77
Fig. S4–S11 (SI) compile the temperature-dependent features of the sequential in situ vibrational (Raman, FTIR) spectra obtained for MoOx/TiO2(anatase) with coverage of 2.1–4.9 Mo per nm2 and for MoOx/TiO2(P25) with coverage of 1.9–4.3 Mo per nm2 under flowing 20% O2/He in the temperature range of 430–120 °C. Notably, the temperature–dependent features therein are mutatis mutandis similar to those discussed in the context of Fig. 2–5. Significantly, with increasing coverage, the number of closely related configurations increases, and the bands tend to broaden, overlap and become partially obscured by the growth of the Mo–O–Mo and O–Mo–O modes, whose high wavenumber wing overlaps with the bands attributed to Species-III. Additionally, the occurrence of associated polymolybdate domains gives rise to vibrational coupling, thereby preventing the clear discernment of the spectroscopic signatures due to the distinct extant species.
Mo(–O–Ti)4 Species-II exhibits the highest reactivity towards both surface-retained water molecules, transforming to (O
)2Mo(–O–Ti)3 with temperature lowering, as well as towards hydrogen, thereby undergoing facile 18O/16O isotope exchange of terminal and anchoring O atoms.
Mo(–O–Ti)3 configuration with a νMo
O terminal stretching mode at 996–999 cm−1; (ii) Species-II has a mono-oxo pyramidal-like O
Mo(–O–Ti)4 configuration with a νMo
O at 989–993 cm−1; and (iii) Species-III has a di-oxo (O
)2Mo(–O–Ti)x configuration with a νs/νas pair at 980–983/985–971 cm−1. The Mo
O terminal stretching wavenumbers depend on coverage, exhibiting a slight blue shift with increasing coverage.
(b) At low coverage, i.e. below 1 Mo per nm2 for MoOx/TiO2(anatase) and below 2 Mo per nm2 for MoOx/TiO2(P25), isolated mononuclear species prevail within the dispersed molybdena phase.
(c) Species-I (O
MoO3) prevails over Species-II at a low coverage of below 1 Mo per nm2, which is formed with the first order of priority during the impregnation step by the titration of the most basic support hydroxyls. Species-II gradually prevails over Species-I with increasing coverage. Moreover, at coverages exceeding ca. 2 Mo per nm2, polymolybdate (O
MoO4)n domains consisting of Species-II building units are predominant.
(d) By lowering the temperature in the 430 °C → 250 °C → 175 °C → 120 °C sequence, the mono-oxo Species-II undergoes a transformation to di-oxo Species-III, which is mediated by water molecules retained at the first layer of the support surface. The temperature-dependent Species-II ↔ Species-III transformation is fully reversible.
(e) Species-I is not affected by temperature cycling in the 430–120 °C range, as evidenced by its fixed νMo
O mode wavenumber position and stable normalised band intensity.
(f) The pyramidal-like O
Mo(–O–Ti)4 Species-II exhibits the highest reactivity towards surface-retained water molecules as well as towards hydrogen, thereby being subjected to the reversible temperature-dependent Species-II ↔ Species-III transformation and to a more facile 18O/16O exchange compared to Species-I.
(g) These results point to the feasibility of tuning the configurations of the prevailing (MoOx)n sites dispersed on titania polymorphs by the appropriate control of loading and temperature.
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