Open Access Article
Wenbin Li,
Jiyun Ren,
Wenjie Guo,
Qing Guo,
Sai Zhang
* and
Yongquan Qu
*
School of Chemistry and Chemical Engineering, Northwestern Polytechnical University, 710072 Xi'an, China. E-mail: zhangsai1112@nwpu.edu.cn; yongquan@nwpu.edu.cn
First published on 1st June 2026
The practical application of dry reforming of methane (DRM) is hindered by catalyst deactivation, primarily due to the deviation of the ideal 1
:
1 H2
:
CO stoichiometry for competitive CH4 and CO2 adsorption/activation. Excessive CH4 decomposition results in H2
:
CO > 1 with carbon deposition, while predominant CO2 chemisorption leads to H2
:
CO < 1 with the favorable reverse water-gas shift (RWGS) side reaction. Herein, we demonstrate an *O-migration coupling strategy on Pt/CeO2 featuring Pt clusters and frustrated Lewis pairs (FLPs, consisting of two Ce3+ and one lattice oxygen) to achieve near-stoichiometric and durable DRM. The FLP sites on the CeO2 support, independent of Pt–CeO2 interfaces, reduce CO2 to CO while generating *O species. These *O species migrate to Pt clusters, driving the partial CH4 oxidation. Through this *O-migration-enabled spatial decoupling of CO2 reduction and CH4 oxidation, the catalyst delivers a near-stoichiometric H2
:
CO ratio of 0.99 and an unprecedented CH4 conversion rate of 93.9 mol gPt−1 h−1 at 700 °C. Moreover, stable performance is exhibited for over 400 h, with a turnover number exceeding 7
200
000. This work establishes oxygen migration coupling as a potential strategy for spatially decoupled redox catalysis beyond DRM.
:
CO ratio deviating from unity.7–11 As illustrated in Fig. 1a, excessive CH4 adsorption and decomposition lead to elevated H2
:
CO ratios (>1) and severe carbon deposition, causing catalyst deactivation.7,12,13 Conversely, predominant CO2 chemisorption triggers the reverse water-gas shift (RWGS) reaction, resulting in sub-stoichiometric H2
:
CO ratios (<1) and compromised hydrogen utilization.11,14–17 Therefore, the rational design of catalysts that can balance CH4 and CO2 activation is essential to realize near-stoichiometric DRM, enabling durability and industrial-scale application.
A temporal decoupling strategy, chemical looping DRM, has been developed to address competitive adsorption by separating CH4 oxidation and CO2 reduction into alternating steps over oxygen-storage materials (Fig. 1b).18–20 This approach effectively suppresses coking formation and avoids RWGS, enabling near-stoichiometric H2
:
CO ratios (∼1). Despite this promise, the practical implementation of chemical looping DRM suffers from inherent drawbacks, including energy-intensive temperature swings, reliance on inert gas purging for phase separation, and sluggish kinetics of oxygen mobility in oxygen storage materials, collectively hindering scalability and operational flexibility.
Herein, we report a rationally designed catalyst featuring dual-active sites of Pt clusters and frustrated Lewis pairs (FLPs) (Fig. 1c), where CH4 oxidation and CO2 reduction proceed concurrently yet remain spatially segregated on distinct catalytic sites, subsequently coupling through *O migration across the CeO2 support. The FLP sites on CeO2(110), composed of adjacent Ce3+ Lewis acids paired with a neighbouring lattice O2− Lewis base (Fig. 1c),21 exhibit exceptional CO2 adsorption and activation, outperforming conventional oxygen vacancies and metal–CeO2 interfaces. This enables spatial decoupling of CO2 reduction from CH4 dissociation on Pt clusters. Mechanistically, CO2 reduction at FLP sites directly generates CO and reactive *O species; the *O then migrates rapidly across the CeO2 surface to Pt clusters, where it drives the partial oxidation of CH4 to H2 and CO (Fig. 1c). This dynamic coupling affords a near-stoichiometric H2
:
CO ratio of 0.99, which in turn delivers exceptional catalytic stability (>400 h) with a turnover number exceeding 7
200
000. Moreover, the catalyst achieves a remarkable CH4 conversion rate of 93.9 mol gPt−1 h−1 at 700 °C, surpassing recently reported state-of-the-art systems.
Density functional theory (DFT) calculations were employed to guide this design. As shown in Fig. 2a and S1–S5, CO2 adsorption at the oxygen vacancy (OV) on CeO2(110) (CeO2(110)-OV) is significantly stronger than that on CeO2(111)-OV, with an adsorption energy of −2.51 eV. Although this value is more negative than that for CO2 adsorption on Pt6 clusters, it remains comparable to that at the Pt6–CeO2 interface, indicating that an isolated OV is insufficient to achieve the full spatial decoupling. Notably, constructing adjacent OV pairs on CeO2(110) creates the FLP sites (Ce3+…Ce3+, O2−; Fig. 2b), which dramatically enhance CO2 adsorption, with an energy of −3.30 eV (Fig. 2a). In contrast, creating more OVs on CeO2(111) merely increases the number of OVs without creating a distinct adsorption site (Fig. 2b). These results confirm that a FLP on CeO2(110), coupled with Pt clusters, provides an ideal platform for spatially decoupled catalysis toward efficient and stoichiometric DRM.
Guided by the above analysis, we synthesized porous CeO2 nanorods (denoted as CeO2-FLP) designed to host FLP sites through a sequential low- and high-pressure hydrothermal method.21,32 Dark-field transmission electron microscopy (TEM) images revealed a well-defined porous architecture with an average pore size of 2–3 nm (Fig. S6a). High-resolution TEM showed lattice fringes with a lattice fringe spacing of 0.19 nm, corresponding to the CeO2 [220] planes (Fig. S6b), indicating the preferential growth along the [110] direction. X-ray photoelectron spectroscopy (XPS) analysis of Ce 3d and O 1s peaks indicated the abundance of surface defects in CeO2-FLP, as evidenced by the Ce3+ (29.4%, Fig. S7a) and Ce3+-O (52.4%, Fig. S7b) fractions. The abundance of OV, along with the exposure of (110) facets, suggests the effective formation of FLP sites on the CeO2-FLP surface.21,33,34
Subsequently, Pt clusters were deposited on CeO2-FLP (Ptcluster/CeO2-FLP) using H2PtCl6·6H2O as the precursor via a photo-assisted reduction process. The actual Pt loading was quantified to be 0.9 wt% using inductively coupled plasma optical emission spectroscopy (ICP-OES). High-angle annular dark-field scanning transmission electron microscopy (HAADF-STEM) images of Ptcluster/CeO2-FLP revealed brightness variation on CeO2-FLP (Fig. 2c), indicating the presence of Pt clusters with an average size of 0.9 ± 0.1 nm (Fig. S8). CO chemical adsorption determined a Pt dispersion of 43.2% (Table S1). Importantly, Ptcluster/CeO2-FLP retained high Ce3+ (30.9%) and Ce3+-O (55.2%) fractions (Fig. S7), confirming the preservation of the FLP-rich surface.
The DRM performances of Ptcluster/CeO2-FLP were evaluated in a fixed-bed reactor at a feed ratio of CH4
:
CO2
:
N2 (2
:
2
:
1). At 700 °C, Ptcluster/CeO2-FLP achieved a CH4 conversion of 75.7% (Fig. S9), approaching the thermodynamic equilibrium (76.0%, at 700 °C), along with a CH4 conversion rate of 93.9 mol gPt−1 h−1. This activity substantially exceeds that of state-of-the-art catalysts (Fig. 2d and Table S2). Importantly, the H2 and CO production rates reached 187.7 mol gPt−1 h−1 and 189.5 mol gPt−1 h−1, respectively, giving a near-stoichiometric H2
:
CO ratio of 0.99. Therefore, Ptcluster/CeO2-FLP delivers an unprecedented combination of high activity and ideal product stoichiometry for DRM (Fig. 2e and Table S2).
:
CO ratio plummeted to 0.5, indicating severe deviation from stoichiometric product ratios (Fig. 3b). These comparative results unequivocally establish that the FLP sites are essential for achieving exceptional DRM activity and stoichiometry.
Kinetic analysis at low conversions (<20%) further elucidates the critical role of FLP. The CO2 reaction order over Ptcluster/CeO2-FLP was significantly lower than that over Ptcluster/CeO2-OV (Fig. 3c), indicating higher CO2 surface coverage on the FLP-containing catalyst. Arrhenius plots (ln
k vs. 1/T, Fig S13 and S14) revealed that the activation energy (Ea) for CO2 conversion on CeO2-FLP (59.6 kJ mol−1) was substantially lower than that on CeO2-OV (79.1 kJ mol−1). Thus, the higher CO2 coverage on Ptcluster/CeO2 results in the stronger conversion capacity, directly distinguishing FLP from OVs. This trend was further supported by CO2 temperature-programmed desorption (CO2-TPD, Fig. S15), in which CeO2-FLP displayed an additional strong desorption peak at ∼500 °C, confirming enhanced CO2 adsorption at the FLP sites.
More importantly, introducing Pt clusters onto CeO2-OV significantly reduced the Ea for CO2 conversion from 79.1 kJ mol−1 (CeO2-OV) to 71.5 kJ mol−1 (Ptcluster/CeO2-OV, Fig. S14). In the absence of FLP sites on CeO2 supports, CO2 adsorption and activation are influenced by Pt or the Pt–CeO2 interface, consistent with previous reports. Conversely, depositing Pt onto CeO2-FLP exhibited a negligible effect on the Ea for CO2 conversion, as evidenced by the nearly identical values for Ptcluster/CeO2-FLP (55.7 kJ mol−1) and CeO2-FLP (59.6 kJ mol−1; Fig. S14). Different form conventional OV sites, these kinetic results experimentally demonstrate that CO2 activation occurs predominantly on FLP sites rather than at Pt clusters or the Pt–O–Ce interfaces, with Pt clusters playing a negligible direct role in CO2 transformation.
Subsequently, in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS) was employed to monitor the roles of FLP under the given reaction conditions. Both Ptcluster/CeO2-FLP (Fig. 3d) and Ptcluster/CeO2-OV (Fig. 3e) exhibited characteristic vibrational signatures of bicarbonate (*HCO3, at 1602 cm−1) and formate (*HCOO, 1505 cm−1) intermediates, confirming the CO2 chemisorption on CeO2 supports.35,36 However, Ptcluster/CeO2-FLP exhibited strong capacity of transformation of b-CO32−, as evidenced from their much weaker adsorption peaks at ∼1300 cm−1. Furthermore, Ptcluster/CeO2-FLP displayed an obvious *CO adsorption band (∼2046 cm−1) associated with Pt clusters, which was not detected on Ptcluster/CeO2-OV. This critical distinction confirms that CeO2-FLP enables a direct CO2-to-CO reduction pathway.37,38 Moreover, during CO2 exposure on Ptcluster/CeO2-FLP, the Ce3+-OH stretching mode (∼3656 cm−1) attenuated while Ce4+-OH features (∼3733 cm−1 and ∼3698 cm−1) intensified (Fig. 3d and e),39–41 indicating the accumulation of *O species within the CeO2-FLP lattice during the CO2-to-CO reduction, accompanied by the Ce3+-to-Ce4+ oxidation.
When a CH4 flow was introduced into the in situ reactor, Ptcluster/CeO2-FLP exhibited a significantly enhanced intensity of *CO adsorption on Pt clusters, indicating that the CH4 oxidation occurred on the Pt sites (Fig. 3f). Meanwhile, the vibrational features corresponding to the *CH3 (∼1342 cm−1), *CH3O (∼1471 cm−1), *CH4O (∼1583 cm−1) and Pt-bound *HCOO (∼1517 cm−1) species emerged during CH4 flow, along with the disappearance of CeO2-bound *HCOO bonding (∼1509 cm−1) and *CO32− (∼1397 cm−1) intermediates. Simultaneously, the Ce4+ species (Ce4+-OH, 3733 cm−1) was reduced to Ce3+ (Ce3+-OH, 3658 cm−1) along with these transformations. Thus, these findings collectively demonstrate that CH4 oxidation is mediated by lattice *O species originating from CeO2-FLP supports.
In contrast, Ptcluster/CeO2-OV exhibited negligible activity for this reaction pathway (Fig. 3g). The CH4 exposure on Ptcluster/CeO2-OV induced the rapid emergence of *CH3 (at ∼1342 cm−1) and *CH4 (at ∼1557 cm−1) species, indicating that CH4 adsorption and activation occurred on Pt sites.42,43 However, CO production remained consistently low, demonstrating limited further oxidation of activated *CH3 and *CH4 species to *CO. Furthermore, the partial retention of Ce4+ species (Ce4+-OH, 3733 cm−1) indicated the restricted *O migration during CH4 flow, owing to the poor capacity for CO2 activation/reduction of CeO2-OV. Concomitantly, the disappearance of *HCO3, *HCOO, and b-CO32- species could be attributed to the *H spillover from Pt into the CeO2-OV supports.
Sequential CO2/CH4 pulse experiments further quantified the FLP functions. Ptcluster/CeO2-FLP showed distinct CO2 consumption over 14 pulse cycles, corresponding to an *O storage capacity of 0.136 mmol gcat−1. This observation contrasted sharply with Ptcluster/CeO2-OV, which exhibited a negligible *O storage capacity (0.008 mmol gcat−1), consistent with in situ DRIFTS spectra confirming only adsorption of CO2 on CeO2-OV (Fig. 3h). Subsequent CH4 pulses revealed drastically higher consumption on Ptcluster/CeO2-FLP (0.129 mmolCH4 gcat−1) than that on Ptcluster/CeO2-OV (0.023 mmolCH4 gcat−1). The close match between CH4 consumption and *O storage on Ptcluster/CeO2-FLP confirms efficient transfer of the FLP-generated *O species to Pt sites for CH4 oxidation.
To further decipher the mechanistic roles of Pt species in CH4 activation, the single-atom Pt and Pt nanoparticles (average size 2.2 ± 0.1 nm) were deposited on CeO2-FLP, yielding Pt1/CeO2-FLP (Fig. S16) and PtNP/CeO2-FLP (Fig. S17), respectively. ICP-OES determined Pt loadings of 0.5 wt% for Pt1/CeO2-FLP and 1.0 wt% for PtNP/CeO2-FLP. Notably, the surface properties of the supports in Pt1/CeO2-FLP and PtNP/CeO2-FLP were similar to those of Ptcluster/CeO2-FLP (Fig. S18 and Table S1), enabling the systematic investigations of Pt speciation effects on CH4 activation while excluding the influences of supports.
The Pt L3 edge X-ray absorption near-edge structure (XANES) was used to investigate the electronic states of Pt. The white line peak of Pt1/CeO2-FLP was located at 11
567.4 eV, close to that of PtO2 (Fig. 4a). The k3-weight Fourier transforms of extended X-ray absorption fine structure (EXAFS) spectra of Pt1/CeO2-FLP delivered one prominent peak at ∼1.64 Å, which was labeled as the Pt–O bond (Fig. 4b and S19). The lack of Pt–Pt coordination confirmed the atomically dispersed Pt supported on CeO2-FLP. The wavelet transform analysis directly revealed the absence of Pt–Pt bonds in Pt1/CeO2-FLP (Fig. 4c). In contrast, Ptcluster/CeO2-FLP and PtNP/CeO2-FLP exhibited the white line peaks between Pt foil and PtO2 (Fig. 4a), indicating the mixed valence states of Pt. Meanwhile, both Pt–Pt and Pt–O bonds were clearly observed from the k3-weight Fourier transforms of EXAFS spectra. Compared to PtNP/CeO2-FLP, the higher white line peak revealed more amount of the Pt–O bond in Ptcluster/CeO2-FLP, which could be clearly observed from the wavelet transform analysis. Quantitatively, Pt1/CeO2-FLP, Ptcluster/CeO2-FLP and PtNP/CeO2-FLP exhibited the Pt–O fractions of 100%, 45.4% and 24.2%, respectively, as well as the Pt–Pt fractions of 0%, 54.6% and 75.8%, respectively (Table 1).
| Sample | Paths | Nb | R (Å)c | σ2 (×10−3 Å2)d | S02 | E0 (eV) | R Factor |
|---|---|---|---|---|---|---|---|
a The data ranges used in the fit are 2.0 ≤ k ≤ 13.0 Å−1 and 1.2 ≤ R ≤ 3.5 Å, and depend on the quality of data. The number of fitted variable parameters was 10, which was smaller than the total number of independent data points, approximately 16.1. R-Factors for these fittings are all below 0.02.b Average coordination number. The half path length.c The paths for Pt–O, Pt–Pt are from the crystal structure of PtO2 (P63mc) and Pt (Fm m).d Debye–Waller factor. |
|||||||
| Pt foil | Pt–Pt | 12.0 | 2.77 | — | — | — | — |
| PtO2 | Pt–O | 6.0 | 2.07 | — | — | — | — |
| Pt1/CeO2-FLP | Pt–O | 3.4 ± 0.1 | 2.04 ± 0.07 | 5.2 ± 0.9 | 0.8 | 7.4 | 0.018 |
| Ptcluster/CeO2-FLP | Pt–O | 4.4 ± 0.4 | 2.07 ± 0.02 | 2.1 ± 0.2 | 0.8 | 8.5 | 0.012 |
| Pt–Pt | 5.3 ± 0.5 | 2.82 ± 0.16 | 5.2 ± 0.1 | ||||
| PtNP/CeO2-FLP | Pt–O | 3.0 ± 0.7 | 2.10 ± 0.03 | 7.0 ± 2.9 | 0.8 | 8.7 | 0.008 |
| Pt–Pt | 9.4 ± 0.2 | 2.78 ± 0.14 | 5.8 ± 0.6 | ||||
For the DRM reaction, Ptcluster/CeO2-FLP, featuring the co-existence of Pt–O and Pt–Pt bonds, delivered the highest CH4 conversion rate compared to Pt1/CeO2-FLP and PtNP/CeO2-FLP (Fig. 4d and S20), as well as the lowest Ea of 64.1 kJ mol−1 for CH4 conversion (Fig. 4e and S21). These observations confirm that the highest intrinsic activity of Pt clusters originates from a synergistic interplay between Pt–Pt and Pt–O bonds in CH4 activation. This synergy arises from the presence of coordinatively unsaturated metal and oxygen on the Pt surface, which promotes the formation of the adsorbed CH4 σ-complexes and then facilitates C–H bond cleavage in the complexes.25,44 Furthermore, due to the similar surface properties of supports, all Pt/CeO2-FLP catalysts exhibited comparable Ea values for CO2 conversion (Fig. 4e), further confirming the strong capacity of FLP for CO2 adsorption/activation and the negligible influence of Pt active sites on this process.
The CH4 activation on Pt/CeO2-FLP was further investigated by CH4 temperature-programmed reduction (CH4-TPR). After the pre-treatment with Ar purging, a CH4 flow was introduced to probe the catalyst surface. The CeO2-FLP supports alone exhibited no detectable activation peaks (Fig. S22), further confirming that the CH4 adsorption and activation occur exclusively at Pt sites. Importantly, Ptcluster/CeO2-FLP exhibited the strongest peak intensity and the lowest initiation temperature compared to both Pt1/CeO2-FLP and PtNP/CeO2-FLP (Fig. S22). These observations directly confirmed the highest capacity of Ptcluster/CeO2-FLP for the CH4 adsorption and activation in DRM.
Subsequently, in situ DRIFTS experiments were performed to compare the behaviors of Pt clusters and nanoparticles under the given reaction conditions. Under CO2 flow, PtNP/CeO2-FLP exhibited spectral changes nearly identical to those of Ptcluster/CeO2-FLP, consistent with their similar CeO2 surface properties for CO2 adsorption (Fig. 4f). Upon switching to CH4 flow, characteristic peaks corresponding to adsorbed *CH4 (1557 cm−1) appeared on PtNP/CeO2-FLP, confirming CH4 adsorption (Fig. 4g). Unlike Ptcluster/CeO2-FLP, no clear signals for *CHxO intermediates were detected on PtNP/CeO2-FLP. Moreover, the Ce4+-OH peak persisted even after 9 min CH4 flow, indicating restricted *O migration from the support to the Pt nanoparticles. Together with CH4-TPR results, these observations demonstrate that Pt clusters uniquely promote the migration of *O species, which in turn enhances CH4 activation and overall DRM activity.
Building on the foregoing analysis, the spatially separated Pt clusters and FLP sites serve distinct roles in CH4 oxidation and CO2 reduction, respectively, with *O migration acting as the key coupling step, as illustrated in Fig. 1c. To further probe the origin and transfer of *O species, we performed 18O-isotope labeling experiments. Because labeled CO2 can lead to ambiguity from residual adsorption or desorption of 18O-containing species, we designed the experiment using H218O pretreatment, which readily dissociates on CeO2 but not on Pt clusters.32,45,46 Specifically, after pretreating Ptcluster/CeO2-FLP with H218O at 150 °C for 30 min, purging with Ar for 30 min was performed to remove physically adsorbed species. The programmed temperature increase of CH4 oxidation from 200 °C to 750 °C (10 vol.% CH4/He, 50 mL min−1) revealed the appearance of the C18O/CO signal (Fig. 4h), which directly demonstrated that *O species stored in the CeO2-FLP support participate in CH4 oxidation through oxygen transfer to Pt clusters. Furthermore, the H2 signal appears simultaneously with the CO/C18O signals, indicating that CH4 dissociates on Pt sites, with CO and H2 formation. Notably, the observed C18O signal indicates that the oxygen involved in CH4 oxidation originated predominantly from H218O-derived *18O species stored in the CeO2-FLP support rather than from the lattice oxygen. Together, these results strongly support a spatially decoupled reaction pathway in which *O migration couples CO2 reduction on the support with CH4 oxidation on Pt clusters.
:
CO ratios (1
:
1) and long-term catalytic stability. As shown in Fig. 5a, this activity balance is inherently determined by the quantitative relationship between FLP sites (responsible for CO2 reduction) and Pt clusters (mediating CH4 oxidation). While the FLP sites remain fixed within the CeO2-FLP supports, we precisely adjusted the number of Pt centers by controlling the Pt loadings. HAADF-STEM images revealed that increasing Pt loadings from 0.5 wt% to 2.0 wt% enhanced the densities of Pt clusters while preserving their similar cluster dimensions (an average diameter of 0.9–1.0 nm, Fig. S23). This controlled variation in Pt cluster population enabled systematic modulation of the FLP-to-Pt site ratios, a crucial factor governing overall DRM performance.
For DRM, Pt loading significantly influenced reaction kinetics and product stoichiometry. At 0.5 wt% Pt loading, the CH4 conversion rate of 115.7 mmol gcat−1 h−1 was lower than the CO2 conversion rate of 169.7 mmol gcat−1 h−1, resulting in a significantly reduced H2
:
CO ratio of 0.81 at 700 °C (Fig. 5b and S24). Elevating the Pt loading to 1 wt%, accompanied with a higher density of Pt clusters, drastically improved the enhanced CH4 conversion rate (405.4 mmol gcat−1 h−1), matching the CO2 conversion rate of 405.6 mmol gcat−1 h−1. Simultaneously, the H2
:
CO ratio approached 0.99, nearly achieving a stoichiometric ratio of 1 (Fig. 5b). Therefore, increasing the Pt loading facilitated the optimal matching between Pt clusters and FLP sites.
Further increasing the Pt loading to 2 wt% resulted in CH4 and CO2 conversion rates similar to those observed for Ptcluster/CeO2-FLP with 1 wt% Pt loading (Fig. 5b and S24). This observation demonstrated that the CH4 activation and conversion depended on the migration of *O species generated from the CO2 reduction on FLP of CeO2-FLP, rather than the availability of Pt clusters. Consequently, CH4 conversion rates plateau at the 1 wt% Pt loading, as additional Pt clusters cannot compensate for the limited *O supply from the FLP. The extra CH4 conversion would lead to carbon deposition on the catalyst surface (Fig. 5a). Carbon balance analysis before and after the reaction revealed greater carbon imbalance for Ptcluster/CeO2-FLP with higher Pt loadings, indicating direct carbonization of CH4 on Pt (Fig. S25). Raman spectroscopy of the spent Ptcluster/CeO2-FLP catalysts proved the direct evidence of carbonaceous species (Fig. S26). After 45 h reaction at 700 °C, thermogravimetric analysis (TGA) quantified a carbon deposition rate of 2.69 mg gcat−1 h−1 for the 2 wt% Ptcluster/CeO2-FLP catalysts, which was ∼7 times higher than that for 1 wt% and 0.5 wt% catalysts (0.39 and 0.38 mg gcat−1 h−1, respectively; Fig. S27). Collectively, these results reveal the critical role of the balanced FLP-to-Pt site ratios in achieving efficient DRM performance with stoichiometric H2
:
CO output.
Kinetic analysis further clarified the activity matching requirements between Pt clusters and FLP sites (Fig. S28). The comparable Ea values of Ptcluster/CeO2-FLP for CO2 conversion indicated that CO2 adsorption and transformation predominantly occurred on FLP sites (Fig. 5c). Theoretically, similar Pt clusters in Ptcluster/CeO2-FLP should yield comparable Ea values for CH4 conversion. However, when the Pt loading was 0.5 wt%, the relatively large distance between Pt clusters and FLP sites resulted in a higher Ea value for CH4 conversion. In contrast, sufficient Pt loading (>1.0 wt%) reduces the average spatial distance between Pt clusters and FLP sites, leading to sufficient migration and supply of *O species and thus delivering comparable Ea values for CH4 conversion. When the number of Pt clusters matched that of FLP sites, the Ea values for CH4 conversion and CO2 conversion were also comparable, thereby facilitating the DRM reaction with a near-stoichiometric ratio of H2
:
CO ≈ 1. This kinetic deconvolution highlights the critical roles of the available Pt clusters and FLP sites in balancing *O supply (from FLPs) and CH4 activation (at Pt) for DRM.
The CO2 pulse experiments revealed that Ptcluster/CeO2-FLP with varying Pt loadings exhibited comparable *O storage capacities (0.129–0.136 mmol gcat−1, Fig. 5d). These findings further confirm that FLP sites act as active centers for CO2 reduction, generating reactive *O species that subsequently participate in CH4 oxidation pathways. Specially, the Pt loading of 0.5 wt% yielded a low rate of 0.043 mmol gcat−1 due to the insufficient amount and density of Pt clusters. When the Pt loadings were elevated to 1.0 wt% and 2.0 wt%, the CH4 consumption increased to 0.129 mmol gcat−1 and 0.138 mmol gcat−1, respectively. Excessive Pt loading did not enhance DRM activity, as the FLP sites imposed a kinetic bottleneck of the *O supply from the CO2 reduction.
Notably, the observed CH4 consumption over Ptcluster/CeO2-FLP did not scale with the population of Pt clusters as the Pt loading increased from 1.0 wt% to 2.0 wt%, contradicting the scenario where only interfacial oxygen is involved in the reaction. This deviation indicates that the *O species are not confined to the Pt–CeO2 interface. Instead, the facile migration of oxygen across the CeO2-FLP support enables the entire oxygen reservoir of the carrier to participate in CH4 oxidation. Consequently, these findings further demonstrate that CO2 activation occurs extensively on the FLP sites of CeO2-FLP, thereby achieving spatial decoupling from CH4 oxidation at the Pt clusters.
Additionally, the optimal synergy of Pt clusters and FLP sites directly enhances catalytic stability. Ptcluster/CeO2-OV, lacking FLP sites, exhibited inferior stability, as evidenced by the substantially declined conversions of CH4 and CO2 during a period of 45 h (Fig. 5e). Similarly, Ptcluster/CeO2-FLP with either insufficient (0.5 wt%) or excessive (2.0 wt%) Pt loading exhibited compromised durability, attributable respectively to limited CH4 activation capacity and inadequate *O-migration kinetics. In contrast, the optimally matched Ptcluster/CeO2-FLP (1 wt% Pt loading) catalyst delivered exceptional long-term stability, maintaining nearly constant CH4 conversion rates (Fig. 5e) and a near-stoichiometric H2
:
CO ratio (Fig. S29) for over 400 h. During the initial 100 h, when the H2/CO ratio remained near 1, no detectable water appeared in the product stream, indicating effective suppression of the RWGS reaction. However, XPS analysis of the spent Ptcluster/CeO2-FLP catalyst revealed both reduced surface defects and accumulated carbonaceous species (Fig. S30), which together mask Pt clusters and FLP sites. Notably, a slight 15% loss in activity during long-term testing was completely reversed by a simple CO2 treatment (Fig. 5e). This remarkable stability reflected in a turnover number (TON) exceeding 7
200
000 per exposed Pt site for CH4 conversion (Fig. 5f and S31). To the best of our knowledge, Ptcluster/CeO2-FLP represents the first to simultaneously achieve such a record-high TON and unprecedented activity, with its TON value nearly double the previously reported maximum (Fig. 5f).
Finally, we propose a catalytic process for DRM on Ptcluster/CeO2-FLP that spatially decouples CO2 reduction and CH4 oxidation, as illustrated in Fig. 1c. The CO2 reduction step follows a Mars–van Krevelen (MvK) mechanism: CO2 is adsorbed and activated at FLP sites, directly forming CO and leaving *O species on the CeO2-FLP support. Subsequently, the *O species migrate from FLP sites to Pt clusters. On Pt clusters, CH4 is converted to CO and H2 via *CHxO intermediates, facilitated by the migrated *O species. Thus, while the individual CO2 reduction step obeys the classical MvK redox cycle, the overall process represents a modified MvK-type pathway enabled by spatial decoupling and *O migration between distinct active sites. This design separates CO2 reduction (FLP sites) from CH4 oxidation (Pt clusters) and couples them through oxygen spillover. Through precise matching of Pt clusters and FLP sites, the two half-reactions are efficiently coupled, leading to a near-stoichiometric H2/CO ratio and sustained DRM activity.
:
CO ratio. This catalyst separates the antagonistic adsorption and activation steps: CO2 is selectively reduced at FLP sites on the CeO2(110) facet, while CH4 is partially oxidized on Pt clusters, with *O shuttling dynamically between the two sites. This *O-transport mechanism intrinsically couples the two half-reactions, maintains a balanced redox cycle, and effectively maintains a H2
:
CO ratio of 0.99 while suppressing coke formation and deactivation pathways. As a result, the catalyst delivers a record CH4 conversion rate of 93.9 mol gPt−1 h−1 at 700 °C with stable operation exceeding 400 h under continuous, isothermal conditions. Although the present study employs Pt/CeO2(110) as a model platform, the underlying principle is not limited to this specific combination. The key requirements are: (i) a reducible oxide support capable of forming FLP sites (adjacent oxygen vacancies) that strongly activate CO2 and (ii) metal sites (clusters or nanoparticles) that can activate CH4 and accept migrating *O species. Many earth-abundant metals (e.g., Ni, Co, and Ru) and other reducible oxides (e.g., TiO2, WO3, and In2O3) are known to exhibit similar oxygen spillover behavior and have been reported to form frustrated Lewis pair-like defects under reducing conditions. Therefore, we anticipate that the spatial decoupling strategy can be extended to more practical catalyst compositions, guided by the design principles established here.
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