3.1. Characterization
The activity study of the defined CoTiO
3 and Co
2TiO
4 phases is imposed after their formation in the stationary state during a study of the x%/TiO
2 catalysts in ODH of ethane, hence the importance of associating the latter to this study. The X-ray diffraction patterns of the prepared x% Co/TiO
2 samples are displayed in
Figure 1. An examination of the obtained results reveals that the sample diffractogram with a low concentration of cobalt 3.8 wt % (
Figure 1, curve b), is characterized by peaks of the anatase titania (JCPDS file #84-1286). For the 7.5 and 15.0 wt% cobalt samples, in addition to anatase, a few peaks were observed (
Figure 1, c, d), denoting Co
3O
4 formation (JCPDS file no. 78-1970). The intensity of the system exhibits a direct correlation with the concentration of cobalt, whereby higher cobalt concentrations lead to increased intensity levels. Additionally, when the Co content increases from 7.5% to 15%, the average particle size ranges from 17 to 19 nm, which is in agreement with the findings reported by Ho et al. [
32]. The study revealed the presence of Co
3O
4 crystallites in samples that contain as little as 1.5% of Co within the anatase and rutile mixture, which also has a surface area of 50 m
2 g
-1. The findings of this work are different from those reported previously and by other researchers, which could be a result of the greater surface area of anatase present in our samples. This leads to improved dispersion of Co
3O
4 and potentially the formation of some amorphous species that are not identifiable by X-ray diffraction.
The XRD patterns of CoTiO
3 and Co
2TiO
4 samples calcined at different temperatures are shown in
Figure 2A and
Figure 2B, respectively. For both samples, it can be observed that the calcination at 550°C leads mainly to a mixture of phases: CoTiO
3, Co
2TiO
4 and Co
3O
4. The Co
2TiO
4 is minority compared to the other phases. Increasing temperature to 750°C for the CoTiO
3 sample decreases the intensity of the Co
2TiO
4 lines. Similarly, a significant decrease in the Co
3O
4 lines can be observed. Calcination at higher temperature (1150°C) leads to single-phase systems: the ilmenite CoTiO
3 and spinel Co
2TiO
4 phases.
On the other hand, the study of ilmenite CoTiO3 phase by XRD showed that the Ti4+ and Co2+ ions occupy slightly distorted octahedral sites. The ilmenite structure is found in oxides with the formula ABO3 when the A and B ions have similar sizes and a total charge of +6. The name ilmenite comes from the mineral FeIITiIVO3, which has a structure similar to corundum. It consists of a compact hexagonal arrangement of oxygen ions and cations occupying two thirds of the octahedral sites. Divalent and tetravalent ions form alternating layers. On the other hand, Co2TiO4 has an inverse spinel structure which can be represented by the formula Co2+(Co2+Ti4+)O4, where half of the Co2+ ions occupy the tetrahedral sites, the other half of the Co2+ ions and Ti4+ ions occupy the octahedral sites.
Table 1 shows the Specific Surface Areas (m
2/g) (SSA) of Co(x%)/TiO
2 and CoTiO
3 and Co
2TiO
4 defined phases. It has been noticed that the SSA of the CoTiO
3 and Co
2TiO
4 phases are lower than the Co(x)/TiO
2 samples and these values decrease when calcination temperature of CoTiO
3 and Co
2TiO
4 increase, which could be due to sintering and reduction in the number of active sites available for catalysis.
Diffuse reflection UV-visible-NIR spectroscopy offers valuable insights into the oxidation state of transition metals, their coordination, and the symmetry of their surrounding environment. Co/TiO
2 absorption spectra in the UV-visible-NIR are displayed in
Figure 3. It should be noted that distinguishing between different species is challenging for two distinct considerations: (i) in the 1100 - 1500 nm wavelength range, the v1 transition of octahedral ions partially overlaps with the v
2 transition of tetrahedral species. In addition, the high coefficient of absorption of the tetrahedral species makes it difficult to detect the first transition; (ii) in TiO
2, a Co
2+ → Ti
4+ charge transfer can take place. Indeed, an absorption of Co
2+ modified MgTi
2O
5 in the 400-500 nm wavelength region was assigned to this transition mode [
12,
33]. It is important to consider Co
2+ to Ti
4+ charge transfers since cations of active phase and the support have variable valence. The UV spectrum of TiO
2 shows strong absorption related to the interband transition and maxima around 320 and 220 nm are attributed to Co
2+ to Ti
4+ charge transfers. The 3.8 wt% Co sample has slight absorption in the visible range (
Figure 3), however for 7.5 and 15 wt% Co samples, new bands appear and intensify with increasing Co load. The near-infrared (NIR) region has a broad band in the 1200 and 1600 nm interval, as well as the band of 2"(OH) harmonics of residual hydroxyl groups, which is located close to 1380 nm. The visible range has another band around 700 nm, and a shoulder with a maximum at 420 nm in the range of 400 and 600 nm observed only in the loaded 15 wt% Co sample (
Figure 3, curve d). These results indicate the presence of different cobalt species [
12].
The UV-visible-NIR spectra of the CoTiO
3 and Co
2TiO
4 samples calcined at different temperatures (550, 750 and 1150°C) are shown in
Figure 4A and
Figure 4B. In general, the calcination temperature changes drastically the position, shape and relative intensities of the bands.
In the case of the CoTiO
3 sample calcined at 550° C, two broad bands A and B appear at 596 and 760 nm respectively. The calcination temperature has no effect on the position of these bands, however, a variation in their relative intensities is observed after calcination. In the NIR part, a notable modification of the maxima of the bands was observed. Indeed, the sample calcined at 550°C is characterized by the appearance of the bands at 1250, 1350 and 1530 nm and a shoulder at 1750 nm (
Figure 4A; spectrum a) which are already attributed to the transition
4A
2(W)→
4 T
1 (F) divalent cobalt in tetrahedral site. The treatment at 1150°C leads to the appearance of an intense and broad band centered at 1530 nm (
Figure 4A, spectrum c). Also note that in the ilmenite CoTiO
3 structure
, the Co
2+ ions are in octahedral symmetry. In the olivine Co
2SiO
4 structure taken as reference, the Co
2+ occupy the octahedral interstices. The UV-visible spectrum of this compound (data not shown) has a similar appearance with that of the ilmenite CoTiO
3 phase (
Figure 4, spectrum c). The bands at 600, 760 and 1530 nm are assigned to the three
4 T 1g →
4 T
1g (P);
4T
1g →
_ 4 A
2g (F) and
4 T
1g→
4 T
2g (F) divalent Cobalt in octahedral sites.
The fundamental 4F level of the Co2+ ion in the tetrahedral field breaks down into the lowest ,4A2 4 T1 and 4 T2. The transition 4A2 (F) →4T2 (F) is forbidden to the electric dipole approximation and allowed to the magnetic dipole approximation. It is indeed very weak and often appears in the infrared region. The two transitions 4A2 (F) →4T1 (F) and 4A2 (F) →4T1 (P) give very high intense absorption bands, often in three components because of the spin-orbit coupling.
The spectrum of the Co
2TiO
4 sample calcined at 550°C is similar to that of CoTiO
3 calcined at the same temperature of 550°C
(Figure 4B, curve a). After treatment at 750°C (
Figure 4B, curve b), its appearance changes radically in the visible part. Indeed, it is noticed the appearance of several absorptions: 588,638 and 688 nm and a shoulder around 750 nm.
At higher calcination temperature, a broad absorption spreads between 1300 nm up to 1820 nm which has already been observed in the case of soda-lime glasses where divalent cobalt and in tetrahedral symmetry [
12]. The two shoulders around 535 and 720 nm are respectively attributed to the
4T
1g →
4T
1g (F) and
4T
1g→
4T
1g (F) of Co
2+ in octahedral sites. The band at 720 nm has already been observed in the case of CoNaY zeolites [
34].
Laser Raman spectroscopy is a widely used tool in the field of supported and unsupported catalysis. The obtained data for the three Co/TiO
2 catalysts are depicted in
Figure 5A. The band observed at 397, 514 and 640 cm
-1 are characteristic of TiO
2 anatase structure, (curve a). When 3.8% wt of cobalt was added, the spectrum was not impacted (spectrum b). In contrast, higher cobalt levels spectra show bands close to 692 cm
-1 and two shoulders at 487 and 528 cm
-1, suggesting the formation of Co
3O
4 [
12,
35].
The Raman spectra of the two CoTiO
3 and Co
2TiO
4 phases calcined at 1150°C are shown in
Figure 5B. As far as the spinel is concerned, no Raman vibration mode has been observed in the frequency range between 200 and 1000 cm
-1 (
Figure 5B-a). On the other hand, the Raman spectrum of the ilmenite CoTiO
3 phase (
Figure 5B, spectrum b) shows several bands respectively at 688, 450, 379, 332, 263 and 233 cm
-1 and two shoulders at 602 and 204 cm
-1. The mode of vibration at 688 cm
-1 is the most intense. Several isostructural compounds such as (Ni; Fe; Mg)TiO
3 exhibit the same Raman line around 700 cm
-1 . It corresponds to the mode of vibration A
1g of symmetrical elongation of octahedron MO
6 [
36].
The XPS spectra of the CoTiO
3 and Co
2TiO
4 phases are illustrated in
Figure 6A and
Figure 6B, respectively. The spectral lines of the Co2p of these compounds such as the Co2p
3/2 binding energies, the spin-orbit coupling ΔE (Co2p
1/2 -Co2p
3/2) as well as the S/M ratios (satellite intensity/main peak intensity ratio) are reported in
Table 2.
The Co2p
3/2 binding energies (CoTiO
3 : 781.2 eV; Co
2TiO
4 : 781 eV) as well as the ratio (S/M) are in good agreement with the presence of paramagnetic ions (Co
2+). The energy difference ΔE (Co2p
1/2 -Co2p
3/2) is 16 eV in the case of CoO [
12]. It is close to the CoTiO
3 phase ΔE value, which contains only Co
2+ in octahedral sites. For the spinel phase, a ΔE value of 15.8 eV is observed. It should be noted that this difference in energy of the 2p
1/2 and 2p
3/2 electrons usually allows the distinction of the tetrahedral sites, the octahedral sites, however, in the case of the mixed spinel, this discrimination is practically impossible.
3.2. Catalytic Results and Discussion
In order to find a Co/TiO
2 compound adequate to compare the studied CoTiO
3 and Co
2TiO
4 phases, the experiments were conducted at temperature of 550°C. Firstly, the conversion on pure TiO
2 as support has been less than 5%. At steady state, for some Co/TiO
2 catalysts, the ethane conversion increase with reaction temperature in the range 450-550°C (
Figure 7). The conversion rate increases as the cobalt amount increases, reaching a plateau from 7.5 wt% Co. The catalyst loaded 7.5wt% of Co shows a conversion, at 550°C, around 22.2% with an ethylene yield close to 13.3% (60% selectivity).
This result allows us to select the sample containing 7.5 wt % Co as a reference to compare the catalytic performances of the CoTiO
3 and Co
2TiO
4 phases.
Figure 8 shows the variation of ethane conversion as a function of time on Co(7.5)/TiO
2 at 550°C, compared to CoTiO
3 and Co
2TiO
4 catalytic activities. For the Co (7.5)/TiO
2, the conversion decreases from 33% to around 22.2% when it reaches steady state after 3 h of reaction. During this time, the specific surface has been significantly reduced and the color of the catalyst changes from light gray to green, probably due to the change in the coordination and/or the oxidation state of the cobalt cations.
Figure 8 displays also the conversion of ethane with time over the defined phases CoTiO
3 and Co
2TiO
4 calcined at 550 and 1150 °C, respectively. The evolution of the ethane conversion shows that these solids are stable over time regardless of the temperature of their calcination. At 550°C the ethane conversion is of the same order of magnitude as that measured with the Co (7.5)/TiO
2 sample. Therefore, it can be surmised that the octahedral Co
2+ ions, present in these phases, are responsible of the activity [
12,
31]. This result is in agreement with the behavior observed in catalysts modified by phosphorus [
12] and confirms the role played by the Co
3+ ions in the orientation of the reaction.
On the other hand, the catalytic results obtained for the CoTiO
3 and Co
2TiO
4 samples calcined at different temperatures (550°C and 1150°C) are reported in
Table 3. By comparing these performances, the following observations can be made:
• The evolution of overall conversion (
Figure 8) shows that these materials are stable over time regardless of their calcination temperature. At 550°C, the overall conversion of ethane is of the same order of magnitude as that measured with the Co(7.5)/TiO
2 sample (α
g= 22.2%).
• For a calcination temperature of 550°C, the selectivity towards ethylene (
Table 3) is slightly higher in the case of CoTiO
3.
• No significant modification of catalytic activity was observed after calcination at 1150°C, but the production of COx becomes higher.
Apparent activation energy of C
2H
6 oxydehydrogenation on the defined phases catalysts was calculated using the Arrhenius equation (Eq. 1). The relationship between the reaction rate r and the reaction rate constant k was obtained using the theory of reaction series. The expression for the catalytic reaction rate r is identical to that used by Wang et al. [
37].
k is the reaction rate constant, A is the pre-exponential factor, E is the apparent activation energy, and R is the molar gas constant. In Eq. 2, 𝛼, 𝛽, and 𝛾 are reaction orders; C
1, C
2, and C
n are reactant concentrations. In Eq. 4, α is the conversion of reactants, F is the gas flow rate, and M is the mass of the catalyst.
By combining (1), (2) and (3) equations, if the linear relationship between ln(r) and 1/T can be fitted, then the slope of the line is determined. After further calculation, the apparent activation energy E can be obtained (
Table 3).
The obtained values of E for each of the defined phases calcined at 550-1150°C are represented in
Table 3. The values are quite low and the phases calcined at higher temperatures are higher. The order of magnitude of the values suggests a certain influence of the homogeneous phase reaction.
The performance of the catalysts has been compared, determining their selectivity for the same conversion at the identical experimental conditions. At temperature reaction of 550°C, all the catalytic results obtained for the CoTiO
3 and Co
2TiO
4 samples calcined at different temperatures (550°C and 1150°C) are reported in
Figure 9. The evolution of the total conversion shows a notable modification of the catalytic activity after calcination at 1150°C, however the production of CO
x becomes higher. It has been observed that both catalysts have comparable performances when calcined at 550°C. After calcination at 1150°C, the CoTiO
3 phase became more efficient.
Impact of Water Vapor in ODH reaction
In general, water increases the surface acidity and, in this sense, facilitates desorption.
Table 4 summarizes the results obtained when steam was added to the reaction mixture at different percentages. It was observed that both phases CoTiO
3 and Co
2TiO
4 show the same catalytic behavior in the presence of water, whatever their calcination temperature.
It can be pointed out that there is a decrease in the overall ethane conversion and an increase in the ethylene selectivity when the percentage of water increases (
Table 4). On the other hand, it is also noticeable that the yield of ethylene increases slightly with a reaction mixture containing 1.7% of H
2O.
The comparison of the selectivity, obtained for different catalysts, can be appreciated from the plots shown in
Figure 9 and
Figure 10. It is possible to classify the samples in two categories, the first one, the less selective in ethylene, includes the samples tested with the dry mixture. The second category, more selective, is obtained in the presence of steam.
From these obtained results, it can be considered that the limiting step is the desorption of the ethylene molecule from the catalyst surface. The presence of water vapor in the reaction mixture promotes this desorption through competition for site occupation. However, at high percentages of water vapor, a significant portion of the active sites are occupied, leading to a significant decrease in overall conversion. The increase in C
2H
4 selectivity is therefore due to an increase in the OH* species at the catalyst surface [
38] relative to the O* species, which favors total oxidation.