The increase in greenhouse gas concentrations in the atmosphere, especially as a result of anthropogenically produced CO2, is causing climate change [1]. The capture and conversion of CO2 to produce chemicals or carbonaceous fuels via photochemical [2-4], electrochemical [5-8], and catalytic methods [9-12] is a challenge. CO2 reduction by photo-and/or electro-catalytic approaches is currently the subject of much research, but efficient electrocatalysts for CO2 reduction to desirable fuels are still not available. An alternative of particular interest is the reduction of CO2 to CO with H2, which can be generated by water electrolysis, using renewable electricity, via the reverse water-gas shift (RWGS) reaction.
The RGWS, which is a key reaction in the heterogeneous catalytic hydrogenation of CO2, is mildly endothermic with an enthalpy change of [13, 14]:
CO produced by the RWGS reaction can be further hydrogenated to fuels, e.g., methanol, providing a sustainable source of liquid fuel [15, 16].
Catalysts that are active in the WGS reaction are generally also active in the RWGS reaction. Various catalysts for the WGS reaction have been investigated [17-20], e.g., Cu-based Cu/ZnO/Al2O3, Fe-based Fe-Cr, and Ce-based Pt/CeO2. Supported Au nanocatalysts have been developed for CO oxidation at low temperatures [21, 22] and the WGS reaction [21, 23-26]. Because of its high oxygen-storage capacity, the CeO2 support in Ce-based catalysts promotes strong interactions with Au, particularly in the WGS reaction [27-30]. However, only a few studies [10, 11] have focused on Au/CeO2 catalysts for the RWGS reaction. Localized surface plasmon resonance can enhance the catalytic activities of TiO2-supported Au catalysts under visible-light illumination in the RWGS reaction [10]. Quantitative temporal analysis of products has been used to investigate the mechanism of the RWGS on a supported Au/CeO2 catalyst to determine the ability of CO2 to reoxidize a prereduced Au/CeO2 catalyst surface and its activity [11].
Here, we show that a Au/CeO2 catalyst is highly active in the low-temperature RWGS reaction and highly selective for CO production at atmospheric pressure. The effects of the operating conditions, namely temperature, gas hourly space velocity (GHSV), and the molar ratio of the reactants (i.e., H2/CO2) on CO2 conversion were investigated. In situ diffuse-reflectance infrared Fourier-transform spectroscopy (DRIFTS) and mass spectrometry were used to identify the reaction intermediates to clarify how the reaction proceeds over a Au/CeO2 catalyst. High-resolution transmission electron microscopy (HRTEM) and N2 adsorption desorption measurements were conducted on the Au/CeO2 catalyst before and after a 6 h catalytic reaction to investigate the catalyst durability.
A Au/CeO2 catalyst was prepared using a modified incipient wetness impregnation method [22, 31]. A commercial CeO2 powder support (Rare-Chem Hi-Tech Co., China) was impregnated with HAuCl4 solution under stirring, followed by aging overnight at room temperature, rinsing twice with aqueous ammonia solution and deionized water, and drying at 80 ℃ for 8 h to give the Au/CeO2 catalyst.
The Au loading on the Au/CeO2 catalyst was determined using inductively coupled plasma atomic emission spectroscopy (ICP-AES; Optima 2000DV, USA). The specific surface area of the catalyst was determined using the Brunauer Emmett Teller (BET) method, based on N2 adsorption desorption at-196 ℃ (NOVA2200e, Quantachrome Corporation, USA). The catalyst surface morphology and microstructure were examined using HRTEM (Tecnai F30 microscope, operated at 200 kV).
The reaction was performed in a quartz-tube reactor of inner diameter 7.5 mm at atmospheric pressure and temperatures ranging from 300 to 500 ℃. The reactor was loaded with 1 g of the Au/CeO2 catalyst or CeO2. Prior to the reaction, the catalyst or support was activated in N2 (60 mL/min) by heating from room temperature to 500 ℃ at a rate of 10 ℃/min and then maintaining the temperature for 2 h. After activation, mixtures of CO2 and H2 with H2/CO2 molar ratios of 1, 2, or 3 were fed into the reactor to start the reaction. The gas flow rates were controlled using mass flow controllers. The inlet and outlet gases were analyzed online using two gas chromatography (GC) systems, by the internal standard method [32]. N2 was used as the internal standard gas for determining CO2 and CO, and He was used for determining H2.
The conversions of CO2 (XCO2) and H2 (XH2), and the CO selectivity (SCO) were calculated as follows:
where CCO2out, CH2out, CCOout, CN2out, and CHeout denote the concentrations of CO2, H2, CO, N2, and He in the outlet gas, FCO2in and FH2in denote the inlet flow rates of CO2 and H2, and FN2 and FHe denote the flow rates of the internal standard gases N2 and He. The time-on-stream for each performance data point analyzed online using GC in Figs. 2-5 was 1 h. GC data were recorded every 20 min. The mean CO2 conversion was obtained as the average of three measurements.
Thermodynamic equilibrium (TE) conversion values were calculated by the Gibbs free-energy minimization method using HSC Chemistry software (v7.0).
The durability of the Au/CeO2 catalyst was tested by performing the reaction for 6 h under the conditions 400 ℃, H2/CO2 molar ratio=1, and GHSV=12000 mL/(h·g).
In situ DRIFT spectra were recorded from 4000 to 1000 cm-1 at a resolution of 4 cm-1using an FT-IR spectrometer (Nicolet 6700, USA) with a mercury cadmium telluride detector. The intensities were evaluated in Kubelka Munk units. A sample of around 0.2 g was loaded in a DRIFTS cell. DRIFTS was performed as follows. (1) The sample was pretreated in Ar (50 mL/min) at 500 ℃ for 2 h. (2) The temperature was decreased to 400 ℃. (3) The Ar was switched to CO2 and H2 (25 mL/min), and the reaction was performed at 400 ℃ for 1 h. (4) The system was purged with Ar (50 mL/min) at 400 ℃ for 0.5 h. (5) The temperature was increased to 500 ℃ at a rate of 10 ℃/min. (6) The temperature was kept at 500 ℃. The DRIFTS data were recorded for in situ observation of formate formation during step 4 (Fig. 6), and for investigating the decomposition of formate to CO and H2O as a function of time after step 5 (Fig. 7). The outlet gas from the DRIFTS cell was monitored simultaneously using a mass spectrometer (HPR-20QIC, Hiden, UK).
The Au loading on the Au/CeO2 catalyst, determined using ICP-AES, was 3.0 wt%. The BET surface areas of the Au/CeO2 catalyst before and after reaction for 6 h were 68 and 64 m2/g, respectively.
Fig. 1 shows high resolution TEM images of the Au/CeO2 catalyst before and after catalytic reaction for 6 h. The lattice fringe spacing values of 0.20, 0.31, and 0.27 nm represent Au (200), CeO2 (111), and CeO2 (200), respectively, enabling them to be distinguished although the contrasts in the TEM images are very similar. The size of the Au particles on the Au/CeO2 catalyst was 4-5 nm, and did not change much after reaction for 6 h. X-ray diffraction (XRD) did not detect Au in a Au/CeO2 catalyst for the WGS reaction [33] because of the low Au loading (1.85 wt%). Similarly, for our Au/CeO2 catalyst for the RWGS reaction, the Au loading was low (3 wt%), therefore the intensity of the Au peak was low and could not be observed in the XRD patterns; no clear difference was observed between the CeO2 patterns before and after reaction for 6 h (data not shown).
Our previous X-ray photoelectron spectroscopy [22] study suggested that Au is present in a mixture of oxidation states, i.e., Au0, Au1+, and Au3+, in the fresh Au/CeO2 catalyst. In situ reduction of cationic Au occurs during CO oxidation at room temperature [22], which implies that Au0 primarily catalyzes the reaction. The significant decrease in the reduction temperature observed in H2 temperature-programmed reduction implies that the presence of Au facilitates the reduction of surface oxygen species [22].
Fig. 2 shows the effect of temperature on CO2 conversion over the Au/CeO2 catalyst. GC analysis showed that CO is the only carbonaceous product. The GC results suggest that CO selectivity was nearly 100% under all the conditions used in this study. The CO2 conversion over the Au/CeO2 catalyst increased rapidly from 2.9% at 300 ℃ to 30.3% at 500 ℃. It is worth noting that the CO2 conversion approached the TE value above 450 ℃. In the absence of Au, the CeO2 support was almost inactive in the reaction below 500 ℃. Fig. 2 therefore shows that Au contributed significantly to the catalytic activity of Au/CeO2 in CO2 conversion.
Fig. 3 shows that the CO2 conversion increased from 15.4% to 25% to 27.6%, and the H2 conversion decreased from 16.1% to 13.2% to 9.2%, with increasing H2/CO2 ratio from 1 to 2 to 3. The enhanced CO2 conversion was attributed to the reaction equilibrium shifting forward as the concentration of the other reactant, i.e., H2, increased. The molar ratio of consumed H2 to consumed CO2 remained at approximately 1 for all three H2/CO2 ratios; this is consistent with the stoichiometric ratio in CO2 reduction via equation 1. The results show that selectivity for CO was nearly 100% in CO2 reduction with H2 over the Au/CeO2 catalyst.
Fig. 4 shows the effect of the GHSV on CO2 and H2 conversions over the Au/CeO2 catalyst at a H2/CO2 molar ratio of 1. The CO2 or H2 conversion decreased linearly with increasing GHSV, with identical slopes; this is consistent with the H2/CO2 stoichiometric ratio of 1 in Equation (1). At a low GHSV, the long residence time would enable TE to be achieved. At a GHSV of 6000 mL/(h·g), which is much lower than the typical GHSV of 12000 mL/(h·g), CO2 conversion reached 20.7%, approaching the TE value of 22.4%.
The effects of temperature, H2/CO2 molar ratio, and GHSV on the conversions of CO2 and H2 over the Au/CeO2 catalyst were investigated. The CO2 conversion approached the TE value under various conditions, i.e., above 450 ℃ at a GHSV of 12000 mL/(h·g) (Fig. 2), or at 400 ℃ and a GHSV of 6000 mL/(h·g) (Fig. 4). The molar ratios of consumed H2 to consumed CO2 for various H2/CO2 molar ratios were approximately the same and consistent with the stoichiometric ratio of the reaction; this is evidence of nearly 100% CO selectivity. GC showed that the only carbonaceous product was CO, providing further evidence that the CO selectivity was nearly 100%. Figs. 3 and 4 show the approximate ratios of consumed H2 to consumed CO2; the changes in H2 and CO2 conversions with changes in GHSV had the same slope, confirming that the reaction follows Equation (1).
Fig. 5 shows the durability of the Au/CeO2 catalyst during reaction for 6 h. The CO2 and H2 conversions decreased slightly and the conversion values were consistent with those in Fig. 3; the CO selectivity remained at around 100%. HRTEM images of the Au/CeO2 catalyst before and after reaction for 6 h (Fig. 1) showed that the Au particle size was unchanged. The catalytic activity of a Au-based catalyst is generally highly sensitive to the Au particle size at the nanometer level. The HRTEM images in Fig. 1, which show no obvious changes in the Au particle during the durability test, therefore indicate only slight variations in the catalytic activities, i.e., CO2 and H2 conversions.
Supported metal catalysts for CO2 reduction with H2 to CO (the RWGS reaction), e.g., Pd-In/SiO2 [34] and Ni/CeO2 [27], that give nearly 100% CO selectivity [34] or low CO selectivity because of the formation of methane as a byproduct [27] have been developed. Figs. 2-5 show that our Au/CeO2 catalyst gave nearly 100% CO selectivity, and a high catalytic activity for CO2 conversion approaching the TE value. Because such high catalytic activities and nearly 100% CO selectivity were achieved, we examined the mechanism of the reaction over the Au/CeO2 catalyst.
Two main reaction mechanisms for the RWGS reaction, i.e., the redox mechanism and the associative formate mechanism, have been proposed and are still the subject of debate [11, 12]. We investigated the mechanism by examining in situ DRIFT spectra of the Au/CeO2 catalyst and CeO2 support to identify the surface species formed during the reaction; the spectra are shown in Fig. 6. The bands at 1540, 1374, and 2865 cm-1 in the spectrum of the Au/CeO2 catalyst, and at 1525, 1366, and 2842 cm-1 in the CeO2 support spectrum, are ascribed to νas(COO), νs(COO), and ν(CH), respectively, of surface formate species [35-37]. The amount of surface formate species on the Au/CeO2 catalyst was much larger than that on the CeO2 support, which suggests that the Au/CeO2 catalyst greatly accelerates the formation of formate species. The results confirm that surface formate species are formed during CO2 reduction with H2. We used in situ DRIFTS and mass spectrometry to study the decomposition of surface formate species to determine whether the formate species are intermediates in formation of the target products.
Fig. 7 shows the profiles of the normalized peak areas of ν(COO) and ν(CH), and the integrated mass spectral signals of CO and H2O formed by decomposition of surface formate species as a function of time on the Au/CeO2 catalyst. The DRIFT and mass spectra basically show the same change profiles. The normalized peak areas of ν(COO) and ν(CH) were acquired by integration from 1800 to 1100 cm-1 and 3100 to 2700 cm-1, respectively. The amounts of CO and H2O formed were determined by integration of the mass spectral signals at m/z=28 and 18, respectively. The profiles of the normalized peak areas of ν(COO) and ν(CH) obtained using DRIFTS and the amounts of CO and H2O formed, determined from the mass spectra, represent the decomposition of surface formate species with time on the Au/CeO2 catalyst. The DRIFTS peak area gradually decreased and then stabilized on approximately the same time scale as the corresponding decrease in the mass spectral signal before stabilization. The data for the CeO2 support are not presented here because of the low intensity of the signal. It can be concluded that CO2 selective reduction with H2 to CO and H2O over the Au/CeO2 catalyst involves a surface formate intermediate.
In summary, we synthesized a Au/CeO2 catalyst that was highly active in CO2 reduction with H2 to CO (the RWGS reaction) at low temperatures ( < 500 ℃) and atmospheric pressure. The Au in the Au/CeO2 considerably increased the catalytic activity for CO2 conversion compared with that of the CeO2 support. The catalyst showed high activity, approaching the TE value under the conditions H2/CO2 molar ratio=1, at temperatures above 450 ℃ and GHSV=12000 mL/(h·g), or 400 ℃ and GHSV=6000 mL/(h·g); nearly 100% CO selectivity was achieved. The CO2 conversion increased with increasing H2/CO2 ratio, and the ratio of consumed H2 to consumed CO2 was approximately consistent with the stoichiometric ratio of the reaction. In terms of the mechanism, DRIFTS and mass spectrometry showed that the reaction over the Au/CeO2 catalyst proceeds via a surface formate intermediate; this accounts for the high activity of the Au/CeO2 catalyst at low temperature in the RWGS reaction.