Huiling
Wang
abc,
Qiang
Li
bce,
Jing
Chen
*de and
Hongpeng
Jia
*bce
aCollege of JunCao Science and Ecology (College of Carbon Neutrality), Fujian Agriculture and Forestry University, Fuzhou 350002, China
bXiamen Key Laboratory of Materials for Gaseous Pollutant Control, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China. E-mail: hpjia@iue.ac.cn; Fax: +86-592-6190767; Tel: +86-592-6190767
cKey Laboratory of Urban Pollutant Conversion, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China
dFujian Institute of Research on The Structure of Matter, Chinese Academy of Sciences, Fuzhou 350002, China. E-mail: jing.chen@fjirsm.ac.cn
eUniversity of Chinese Academy of Sciences, Beijing 100049, China
First published on 16th May 2024
Resource utilization of carbon dioxide (CO2) is an effective strategy to mitigate global warming and achieve carbon neutrality and peak carbon goals. It is well known that different preparation methods affect the catalytic performance of catalysts. Herein, we designed an efficient Ru–ZrO2/C catalyst for photothermal catalytic CO2 reduction by pretreating UiO-66 in a N2 atmosphere and then loading Ru species. Compared to the reference sample of Ru/ZrO2 obtained by calcining UiO-66 in an air atmosphere, Ru–ZrO2/C exhibits much superior catalytic activity under full-spectrum light irradiation with a methane yield of 504.1 mmol g−1 h−1 and selectivity of 98.9%, respectively. In addition, the catalytic performance of Ru–ZrO2/C for photothermal CO2 methanation remains stable without obvious reduction in a 24 hour continuous test. The physicochemical characterization studies of Ru–ZrO2/C determine that the remarkable heat resistance, effective light-heat conversion ability, abundant oxygen vacancies, low-valence Ru, and good CO2 adsorption properties are responsible for the enhanced performance of photothermal CO2 hydrogenation. This work expands the application of MOFs as precursors and provides an effective guide for designing highly efficient photothermal catalysts for solar fuel production.
In recent years, metal–organic frameworks (MOFs) have garnered significant attention due to their unique properties, including controllable chemical structures, uniform pores, and tunable electronic structures.12–15 In previous literature studies, MOFs were frequently employed in the photocatalytic reduction of CO2 by exploiting their exceptional light adsorption properties and excellent adsorption of CO2.16–18 Besides, carbon material is also an excellent photothermal material support due to its chemical inertness, structural tunability, and excellent full-spectrum absorption characteristics.19–21 Recent research has explored novel methods for synthesizing metal oxide/porous carbon nanocomposites using MOFs as precursors, opening new avenues for catalyst development.22,23 Therefore, studies to expand the application of MOFs as a precursor and template for the preparation of metal oxide carbon nanocomposites are carried out. In turn, it is essential to study the heat treatment process of MOFs under an inert atmosphere.24 Apart from this, pyrolysis of MOFs is an effective and simple strategy for dispersing reactive metals. For instance, Ru as an active site can be well atomically dispersed on the surface of zirconia/porous carbon due to the generation of oxygen vacancies in ZrOx.24 The catalytic performance of a catalyst is influenced not only by the carrier but also by the active metal loaded on the catalyst. Ye et al. report that group VIII metals (Ru, Rh, Ni, Co, Pd, Pt, Ir, and Fe) have excellent photothermal capabilities.25 Moreover, numerous studies have shown that the less expensive noble metal Ru has excellent CO2 methanation properties.26–28 Precious metal (e.g., Ru and Rh) nanoparticles significantly increase the local temperature and activate H2 in photothermal catalysis, which triggers CO2 (or CO32−) hydrogenation.6,25,29,30
Herein, a metallic zirconium metal–organic framework (UiO-66) was used as a precursor for the preparation of zirconia–carbon nanocomposites (ZrO2/C) by heat treatment under a N2 atmosphere, while a reference support was prepared under an air atmosphere.24 Then a series of Ru-based catalysts were prepared via the impregnation method. The optimal Ru–ZrO2/C catalysts exhibit good photothermal performance during the light-driven CO2 hydrogenation reaction. The rCH4 of Ru–ZrO2/C under full-spectrum simulated sunlight conditions reaches 504.1 mmol g−1 h−1 with high selectivity (98.9%). By contrast, under the same reaction condition, the Ru/ZrO2 catalyst as a reference sample is sluggish. In addition, the activity and selectivity of Ru–ZrO2/C for photothermal CO2 methanation remain stable in a long-term test. The physicochemical characterization tests of Ru–ZrO2/C determine that the remarkable heat resistance, effective light-heat conversion ability, low-valence Ru, and good CO2 adsorption properties are responsible for the enhanced performance of photothermal CO2 hydrogenation. This demonstrates that ZrO2/C as a photothermal support has an important contribution to the catalytic performance of the catalysts. This not only expands the application of MOFs as precursors but also provides new ideas for the construction of efficiently loaded photothermal catalysts.
The two supports of zirconia–carbon nanocomposites (ZrO2/C) and zirconia (ZrO2) were prepared as follows. UiO-66 powder was annealed in a tube furnace and heated to 400 °C at a rate of 5 °C min−1 for 30 min and then to 600 °C at a rate of 2 °C min−1 for 2 hours in an N2 atmosphere (100 mL min−1). After cooling to room temperature, the black ZrO2/C was obtained. The reference support ZrO2 was obtained via annealing UiO-66 in air.
The Ru-based catalysts were fabricated via the wet impregnation method. The Ru–ZrO2/C samples were prepared as follows: first, 200 mg of ZrO2/C and a quantitative RuCl3·3H2O solution were added to 200 mL of deionized water under ultrasonic treatment for 10 min to form a suspension. Then, the suspension was stirred at 350 rpm for 6 hours at room temperature. Finally, the resulting solution was stirred in a 90 °C water bath until dry. The solids were reduced at 300 °C for 3 hours in H2 (30 mL min−1). The reference sample Ru/ZrO2 was synthesized similarly except that ZrO2 was used directly to replace ZrO2/C as the support.
![]() | (1) |
![]() | (2) |
Here, F represents the gas flow rate (mL min−1); [CH4] and [CO] are the respective concentrations (vol%) of CH4 and CO detected by the online GC.
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Fig. 1 (a) XRD patterns, ZrO2 represents JCPDS PDF# 96-210-0389; (b) N2 adsorption–desorption isotherms; (c) pore distribution of the samples. |
Samples | Ru loading (wt%) | S BET (m2 g−1) | D BJH (nm) | Total pore volume (cm3 g−1) |
---|---|---|---|---|
ZrO2/C | — | 16.6 | 3.7 | 0.03 |
Ru–ZrO2/C | 3.3 | 35.5 | 3.7 | 0.05 |
Ru/ZrO2 | 3.2 | 41.3 | 3.9 | 0.06 |
The N2 static adsorption–desorption isotherms were obtained to examine the adsorption properties, specific surface area, and pore size of the samples (Fig. 1b and c). Specific surface area (SBET) and total porosity were calculated using BET and BJH methods. The relationship between the structural characteristics and support of the samples is shown in Table 1. The SBET of pure ZrO2/C is 16.6 m2 g−1 while adding Ru increases the SBET value of Ru–ZrO2/C to 35.5 m2 g−1. A similar trend is also reflected in the variation of pore volume for Ru–ZrO2/C. It can be reasonably assumed that a small amount of Ru species in the precursor matrix of ZrO2/C maintains its intrinsic structure and avoids excessive shrinkage during the pyrolysis process.37 It is noteworthy that the SBET and total pore volume of the reference sample (Ru/ZrO2) are larger than that of Ru–ZrO2/C. This suggests that surface area might not be the primary factor influencing catalytic activity.
The morphology and structure of the samples were investigated using TEM and HRTEM. The TEM images of ZrO2/C and ZrO2 (Fig. S3a and b†) show a typical quasi-cubic shape. The TEM images of Ru–ZrO2/C, Ru–ZrO2/C-3h (Ru–ZrO2/C reacted for 3 hours of the photothermal catalytic reaction), and Ru/ZrO2 are shown in Fig. 2a–c. There is no obvious change in the morphology between the fresh and used Ru–ZrO2/C. HRTEM images of ZrO2/C and ZrO2 show a distance of 0.297 nm corresponding to the (111) plane of ZrO2 (Fig. S3c and d†). HRTEM patterns of Ru–ZrO2/C, Ru–ZrO2/C-3h, and Ru/ZrO2 clearly show the microstructure of ZrO2 and tiny Ru metal nanoparticles in Fig. 2d–f, where the Ru nanoparticles have a well-defined lattice with the same distance of 0.205 nm, corresponding to the (011) plane of Ru. The size of Ru nanoparticles over Ru–ZrO2/C and Ru/ZrO2 is 3.2 nm and 5.5 nm, respectively. The Ru nanoparticles are dispersed in the microstructure of ZrO2/C, and the corresponding elemental mapping diagrams are shown in Fig. 2g. However, no carbon is observed in the HRTEM image of Ru–ZrO2/C and Ru/ZrO2. According to the above analysis, no carbon is observed in the XRD pattern and HRTEM image of Ru–ZrO2/C probably because the amorphous structure of carbon is formed during the calcination process. In addition, carbon is a typical photothermal material and may provide a facile electron transport pathway for CO2 methanation.21 Moreover, the energy dispersive spectroscopy (EDS) elemental mapping shows that the elements of Ru, Zr, and O are uniformly dispersed throughout the microstructure of the cubic particles, which roughly confirms that Ru–ZrO2/C is mainly composed of C, O, Zr, and Ru combined with the HRTEM image (Fig. 2d and g).
As displayed in Fig. 3a, the rate of CH4 production (rCH4) of Ru/ZrO2 at the ninth hour is 104.5 mmol g−1 h−1. Nevertheless, the rCH4 of Ru–ZrO2/C is 504.1 mmol g−1 h−1 with nearly 98.9% selectivity of CH4 under the same reaction conditions, which is much higher than that of Ru/ZrO2. Furthermore, the production rate of Ru–ZrO2/C remains stable, with high SCH4 (≈98.0%) during 24 hours of CO2 methanation at a light intensity of 2858 mW cm−2 (Fig. S7†). In addition, the catalytic durability for multiple cycle tests over Ru–ZrO2/C at a light intensity of 2858 m W cm−2, lasts for at least 24 h (each cycle for 4 h, 6 cycles). During the 6 cycles, the CH4 production rate did not change significantly, indicating that the catalyst had stable reactivity. The HRTEM image and XRD spectra of Ru–ZrO2/C-3h (Fig. 2e, h, and S9†) show no significant changes in the catalyst and as well as no agglomeration and sintering during the catalytic reaction, confirming the structural stability of Ru–ZrO2/C during the reaction process. In addition, Ru–ZrO2/C exhibits good catalytic performance compared with the recently reported photothermal CO2 hydrogenation catalysts (Table S1†). Therefore, Ru–ZrO2/C prepared by pyrolysis of UiO-66 in an N2 atmosphere is an excellent choice for photothermal CO2 methanation reactions with high performance.
To investigate the role of light in the CO2 methanation reaction process, the catalytic performance of the Ru–ZrO2/C catalysts was evaluated in different optical regions (Fig. 3b). When under the full solar spectrum with a light intensity of 2614 mW cm−2, the rCH4 of Ru–ZrO2/C reached 504.1 mmol g−1 h−1 and the surface equilibrium temperature of the catalyst (Teq) detected by the thermocouple was 370 °C. By introducing circulating cooling water around the reactor, the surface temperature of the catalyst reduces to 338 °C from 370 °C, and simultaneously the rCH4 drops to 461.5 mmol g−1 h−1. Moreover, by cutting off the infrared light at the above full-spectrum incident light intensity (2614 mW cm−2), the Teq of the catalyst reduced to 324 °C and the rCH4 only reaches 262.1 mmol g−1 h−1 under irradiation of UV-vis light. However, after increasing the incident light intensity to 3146 mW cm−2, the Teq and rCH4 significantly increased to 370 °C and 507.5 mmol g−1 h−1, respectively, which was comparable to the rCH4 at full-spectrum temperature (370 °C). Besides this, using the ice-water bath method under vis-IR incident light conditions to control the surface temperature at 337 °C, the rCH4 of the CO2 methanation reaction was similar to that under the full-spectrum ice-water bath conditions (338 °C, 461.5 mmol g−1 h−1). These indicate that Ru–ZrO2/C exhibits similar catalytic activity at different light intensities when the temperature reaches the same value. That is to say, the Ru–ZrO2/C photothermal catalytic material may convert concentrated solar energy into thermal energy and then drive the reaction, which is similar to conventional thermocatalysis. Subsequently, we further investigate the photothermal CO2 catalytic reactions at different light intensities over Ru–ZrO2/C catalysts. As shown in Fig. 3c, the surface temperature and rCH4 of Ru–ZrO2/C increased proportionally with increasing light intensity. This indicates that the reaction temperature plays an important role in the photothermal catalytic process, while conventional photocatalysis involving photoinduced electrons is not effective in the system.11 At similar surface temperatures, Ru–ZrO2/C exhibits similar rCH4 in both photo- and thermally driven catalytic processes at a light intensity of 2614 mW cm−2 (Fig. 3d), suggesting consistent thermocatalytic performance with CO2 methanation. In summary, the photothermal CO2 methanation over Ru–ZrO2/C is essentially a light-driven thermocatalysis, where light mainly acts as a heat source to supply thermal energy and then triggers the CO2 methanation reaction over the catalyst. Furthermore, it can be seen from the above that the temperature is an important factor in the CO2 methanation reaction. However, as shown in Fig. 3a and c, even at a similar Teq, the rCH4 of the catalyst Ru/ZrO2 (290 °C, 104.5 mmol g−1 h−1) is lower than that of Ru–ZrO2/C (286 °C, 162.8 mmol g−1 h−1). This suggests that the catalytic performance of Ru–ZrO2/C is also affected by other factors.
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Fig. 4 (a) DRS spectra of the samples; (b) the surface temperature of the samples at a light intensity of 2614 mW cm−2; (c and d) EPR spectra of Ru–ZrO2/C and Ru/ZrO2. |
EPR is further executed at −173 °C to discuss oxygen vacancies (OVs). As shown in Fig. 4c and d, ZrO2/C exhibits a characteristic oxygen vacancy signal at g = 2.003, much stronger than that of ZrO2. Notably, after loading Ru nanoparticles on ZrO2/C, the signal intensity of OVs on Ru–ZrO2/C is significantly lower than that on ZrO2/C (Fig. 4c), which could be attributed to the occupation of OVs by Ru.21 The oxygen defects in ZrO2/C are likely to affect metal adhesion and anchoring and limit the growth of Ru nanoparticles.41,42 This suggests that more OVs formed by calcination under N2 conditions promote the anchoring of Ru species, which may be one of the reasons for the elevated methanation reaction activity of Ru–ZrO2/C. In contrast, the signal intensity of OVs on Ru/ZrO2 is higher than that on ZrO2 (Fig. 4d) due to the Ru species promoting the formation of OVs during the reduction process in H2.43 However, due to the lower catalytic activity of Ru/ZrO2 with abundant oxygen vacancies compared with Ru–ZrO2/C, it is reasonable to think that oxygen vacancies are not the main factor for catalytic activity.
X-ray photoelectron spectroscopy (XPS) was performed to better understand the elemental composition and surface chemical states of catalysts. The Ru 3d photoelectron line is usually used to detect the chemical state of ruthenium, but since this line overlaps with the C 1s line, we replace the Ru 3d spectra with Ru 3p spectra to avoid interference from C 1s.44,45 The spectra for the Ru 3p line for Ru–ZrO2/C and Ru/ZrO2 catalysts are depicted in Fig. 5a and b. Meanwhile, Table 2 summarizes the ratios of different chemical states of all catalysts. The high-resolution Ru 3p spectra indicate that Ru consisted of mainly metallic states (Ru0) and a certain amount of Ru4+. The binding energies of 461.6 eV and 463.9 eV are assigned to the Ru 3p3/2 of Ru0 and Ru 3p1/2 of Ru4+ of Ru–ZrO2/C, respectively.46,47 The Ru 3p XPS spectrum of Ru/ZrO2 is shown in Fig. 5b. We can obtain the value of Ru0/Ru4+ following Ru–ZrO2/C > Ru/ZrO2 (Table 2). The result agrees with EPR results, where OVs promote anchoring of Ru. Remarkably, the Ru 3p binding energy of Ru–ZrO2/C-3h moves toward higher binding energy regions, suggesting the migration of electrons from Ru to the support during the photothermal CO2 hydrogenation process (Fig. S10a†). This observation indicates a strong interaction between Ru nanoparticles and the support, which is usually considered an indicator of high activity for metal-based heterogeneous catalysts.34,45 Also, the ratio of Ru0/Ru4+ increases from 1.62 to 2.46 after CO2 methanation for 3 hours. This proves that there is more production of Ru0 species during the CO2 hydrogenation reaction. It has been reported in the literature that under suitable temperature conditions, metallic Ru as an active form of the metallic phase can activate H2 molecular to initiate CO2 hydrogenation.6,13 The high value of Ru0/Ru4+ is one of the reasons for the highest activity on Ru–ZrO2/C exceeding that on Ru/ZrO2. Moreover, it further explains the increase in activity at the beginning of the stability experiment. In the O 1s spectra, the spectra of Ru–ZrO2/C and Ru/ZrO2 can be divided into three peaks (Fig. 5c and d). Namely, the peaks can be attributed to the surface adsorbed oxygen species (533.3 eV),48–50 oxygen vacancies (532.1 eV),41 and lattice oxygen (530.3 eV),51,52 respectively. The surface adsorbed oxygen species may come from the surface hydroxyl groups, transformation of the surface adsorbed O2 molecules, adsorption of water molecules, and CO32−.53 The O 1s spectra determine the presence and concentration of OVs in catalyst samples. We note that the values of OVs/Olatt of Ru–ZrO2/C, Ru/ZrO2, and Ru–ZrO2/C-3h are similar (Fig. 5c, d, S10b,† and Table 2). According to previous reports, oxygen vacancies contribute to the CO2 methanation reduction reaction.54–56 The photoreduction of CO2 is enhanced by the photoreduction of g-C3N4 with nitrogen-rich vacancies and the oxidation of BiOCl with oxygen-rich vacancies in BiOCl/g-C3N4 Z-type heterojunctions. The DFT calculations revealed that BiOCl/g-C3N4 Z-type heterojunctions engineered with double defects can reduce the energy barrier, and are thermodynamically more inclined to release CO.57 In the construction of a TiO2/g-C3N4 scheme heterojunction, abundant oxygen vacancies enhance photocatalytic CH4 production and selectivity. In addition, DFT calculations showed that oxygen vacancies could effectively modulate the energy barrier, leading to a decrease in the production of the two-electron product CO, while improving the selectivity of the eight-electron reaction. Meanwhile, the oxygen vacancies promoted the formation of ultrafast charge carrier transport channels and facilitated the transfer of photoexcited charges to the surface, thus enhancing the high redox capacity in the catalytic reaction.58 In this study, we analyzed EPR signals before and after loading Ru on the support and found that ZrO2/C obtained by calcination under inert gas conditions had more abundant oxygen vacancies than ZrO2 obtained by calcination in air. ZrO2/C has significantly more oxygen vacancies than ZrO2, and the introduction of Ru decreases the oxygen vacancies, probably because the Ru atoms are tilted and anchored to the oxygen defects of ZrO2−x.59 In XPS characterization, Ru0/Ru4+ of Ru–ZrO2/C is significantly higher than that of Ru/ZrO2, which just proves the anchoring of Ru by oxygen vacancies. Also, it's worth noting that the CH4 yield increased with the Ru loading on ZrO2/C increasing from 0.4% to 4.6% (Fig. S6†). Fig. S6† and Table 1 indicate the key role of Ru nanoparticles as catalytic active sites for CO2 methanation. The above analysis shows that Ru is the active site of CO2 methanation and is the main reason for the enhancement of catalytic activity. In contrast, the oxygen vacancy concentration increased after the introduction of Ru into ZrO2. However, the catalytic activity of Ru/ZrO2 did not increase due to the increase in oxygen vacancies, so it is reasonable to assume that oxygen vacancies are not the main reason for the difference in the activity of Ru–ZrO2/C and Ru/ZrO2. Based on the EPR and XPS analysis, we conclude that N2 calcination may make ZrO2/C have more OVs, enhance the anchoring of Ru, obtain a lower Ru state, and thus enhance the catalytic performance.34
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Fig. 5 (a–d) Ru 3p and O 1s of Ru–ZrO2/C and Ru/ZrO2, respectively; (e and f) CO2-TPD and CH4-TPD profiles of Ru–ZrO2/C and Ru/ZrO2. |
Samples | The binding energy of Ru | Binding energy of O | Molar ratios by XPS | ||||
---|---|---|---|---|---|---|---|
Ru0 | Ru4+ | Oads | OVs | Olatt | Ru0/Ru4+ | OVs/Olatt | |
Ru–ZrO2/C | 461.6 | 463.9 | 533.3 | 532.1 | 530.3 | 1.62 | 0.36 |
Ru/ZrO2 | 462.0 | 463.9 | 532.9 | 531.8 | 530.6 | 1.54 | 0.35 |
Ru–ZrO2/C-3h | 462.1 | 464.8 | 533.5 | 532.1 | 530.4 | 2.46 | 0.37 |
The better adsorption capacity of the reactants facilitates more reactant molecules to participate in the reaction, while the better desorption capacity of the products accelerates the departure of the product molecules, and leaves more adsorption sites for the subsequent CO2 hydrogenation reaction. In this study, the CO2-TPD profile is obtained as shown in Fig. 5e. Ru–ZrO2/C shows a strong signal at the center of 460 °C and 663 °C, which is attributed to the medium-strength and strong basic sites, respectively. The peaks at around 663 °C can be attributed to the CO2 adsorption on the strong basic sites and surface oxygen vacancies.60 Beyond this, the CO2 desorption signal extends up to 700 °C due to the presence of strongly basic sites. The intensity of Ru–ZrO2/C is significantly higher than that of Ru/ZrO2, suggesting the presence of more CO2 adsorption active sites on Ru–ZrO2/C. More CO2 adsorption active sites can adsorb and activate more CO2 molecules and promote electron–CO2 interactions, thus favoring the formation of CH4.47 In addition, the CH4-TPD spectra of Ru–ZrO2/C show that the desorption of CH4 is lower than that of Ru/ZrO2 (Fig. 5f), which indicate that CH4 is less likely to be adsorbed on the surface of Ru–ZrO2/C than Ru/ZrO2. Therefore, CH4 as a product can be rapidly desorbed from the Ru–ZrO2/C surface and leave more active sites for adsorption and activation of CO2 molecules.47 This ultimately improves the catalytic performance of light-driven CO2 methanation.
In situ DRIFTS is performed under a continuous flow of the mixture gas (10% CO2, 40% H2, and 50% He) to identify the intermediates involved and to determine the CO2 reaction pathways. The intermediates appear in the infrared fingerprint region at 1200–1700, 1900–2500, and 3000–3050 cm−1, and the band assignments of the surface-activated species are shown in Table S2.† The in situ DRIFTS spectra of Ru–ZrO2/C at different temperatures are recorded after reaching reaction equilibrium under the same continuous flow reaction conditions as photothermal catalysis (Fig. 6a). The signals of the characteristic peaks increase dramatically with the increase in reaction temperature. After the introduction of the mixture gas at 250 °C, bands of bidentate carbonates (b-CO32−, 1581, 1542, and 1513 cm−1) are observed.61 With the temperature increasing from 250 to 400 °C, the signals of the important intermediates are enhanced in the bands at 1230, 1641, and 1900–2100 cm−1 belonging to COOH*, CH3O−, and linear CO, respectively. The characteristic bands at 1305 and 3016 cm−1 correspond to CH4, which gradually increases as the temperature increases from 250 °C to 400 °C. Meanwhile, similar peaks are observed on Ru–ZrO2/C without light, as shown in Fig. 6b. This indicates that photothermal and thermal CO2 hydrogenation follow a similar reaction pathway, which again suggests that the photo-generated electrons play a minor role in CO2 methanation and the reaction system is a light-driven thermocatalytic reduction reaction.62
Based on the above discussion, a photothermal catalytic reaction mechanism for CO2 reduction on Ru–ZrO2/C is proposed. The light-absorbing properties of ZrO2/C and the “nano-heater” effect of ruthenium nanoparticles convert light energy into heat energy through the photothermal effect under irradiation, thus triggering the catalytic CO2 methanation reaction. CO2 and H2 are adsorbed on the catalyst surface, H2 is dissociated into H atoms, and H atoms reduce the adsorbed CO2 and intermediate products on the catalyst surface. The adsorbed CO2 molecules are dissociated to produce the intermediate HCOO* (CO2 + O* → OCO2* + OH* → HCOO*),63 which generates CO intermediates and a small amount of H2O by the reverse water–gas reaction, and a small amount of CO signal escapes to be detected by the detector (CO2(g) + H2(g) → CO(g) + H2O(g)). Most of the intermediates such as CO*, H*, HCOO*, and hydroxyl groups are adsorbed on the surface of the catalyst and further react to produce CH4 (CO* + H* → HCOO* + H* → H3CO* + OH* → *CH4).64 This is confirmed by the in situ DRIFTS spectroscopic results, and it is finally converted to CH4 by the methanation reaction, which can be expressed as follows: CO2–CO–CH3O−–CH4.65
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ta01821d |
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