Facile one-step synthesis of hierarchical porous carbon monoliths as superior supports of Fe-based catalysts for CO2 hydrogenation

Chengyi Daia, Anfeng Zhanga, Min Liua, Junjie Lia, Fangyu Songa, Chunshan Song*ab and Xinwen Guo*a
aState Key Laboratory of Fine Chemicals, PSU-DUT Joint Center for Energy Research, School of Chemical Engineering, Dalian University of Technology, Dalian 116024, P. R. China. E-mail: guoxw@dlut.edu.cn; Fax: +86-0411-84986134; Tel: +86-0411-84986133 Tel: +86-0411-84986134
bEMS Energy Institute, PSU-DUT Joint Center for Energy Research, Department of Energy & Mineral Engineering, Department of Chemical Engineering Pennsylvania State University, University Park, Pennsylvania 16802, US. E-mail: csong@psu.edu; Fax: +1-814-865-3573; Tel: +1-814-863-4466

Received 6th December 2015 , Accepted 14th January 2016

First published on 18th January 2016


Abstract

A versatile strategy involving one-step desilication of coke-deposited spent zeolite catalyst was successfully developed to prepare hierarchical porous carbon monoliths (HPCMs). Such a strategy avoids the use of hard or soft templates and carbon sources, eliminates high temperature carbonization, simultaneously minimizing the emissions from processing spent catalysts. The resulting carbon exhibits a controlled morphology such as three-dimensional networks, hollow spheres or nanosheets, a high degree of graphitization and a multi-level porous structure. Its mesopore (2–50 nm) surface area can reach 522 m2 g−1 and both mesopore and macropore (50–350 nm) volumes are more than 1.0 cm3 g−1. Such hierarchical porous carbon was found to be a superior support for minimizing the nanoparticle size and enhancing the synergism of the Fe–K catalyst for promoting CO2 hydrogenation. Using such a catalyst results in increased conversion of carbon dioxide and enhanced selectivity of high value olefins (C[double bond, length as m-dash]2–4) and long-chain hydrocarbons (C5+).


1 Introduction

Porous carbon materials can offer superior physical and chemical properties, such as thermal conductivity, chemical stability, electric conductivity and low density, leading to their extensive use in batteries, supercapacitors, gas storage and as supports for many important catalytic processes.1–4 Conventional carbon materials, such as activated carbon (AC), are synthesized by carbonization and chemical (e.g. KOH5) activation of organic precursors, such as coal, wood, fruit shells, and polymers.6,7 These carbon materials normally have micropores with a high surface area. However, the narrow channels limit the diffusion access of molecules to the active site in the micropores. Recently, hierarchical porous carbon materials have been synthesized using (a) hard templates8–10 through impregnation, carbonization, and template removal, or (b) soft templates11–13 through condensation and carbonization. These methods overcome the limitation of micropores but suffer from complicated procedures and high costs. Therefore, finding an efficient and low cost strategy to synthesize hierarchical porous carbon is of great importance.14

ZSM-5 type zeolites offer a strong and tunable acidity, excellent shape selectivity and good hydrothermal stability, leading to their widely use in petrochemical fields.15,16 In the catalytic process, such as methanol to propylene (MTP) reaction, the acid sites on the outer surface can lead to the formation of coke with high degree of graphitization, which could cause the catalyst deactivation.17–19 With the rapid development of the chemical industry, large amounts of spent zeolite catalysts are produced every year. However, most of them are disposed of in landfills, which could lead to a serious environmental problem and a large waste of valuable materials.20

Herein, an efficient and low cost strategy involving one-step desilication of coke-deposited spent zeolite catalyst was successfully developed to prepare hierarchical porous carbon monoliths (HPCMs). Such strategy avoids the use of hard or soft template and carbon source, eliminates high temperature carbonization under inert atmosphere, and simultaneously, decreases the emission of spent zeolite catalyst. The resulting hierarchical carbon has been found to be a superior support of FeK for minimizing the nanoparticle size and enhancing the Fe–K synergism for promoting catalytic CO2 hydrogenation reaction, especially for increased conversion of carbon dioxide and enhanced selectivity of high value olefins (C[double bond, length as m-dash]2–4) and long-chain hydrocarbons (C5+).

2 Experimental

2.1 Synthesis of hierarchical porous carbon monoliths (HPCMs)

In this work, we selected three kinds of conventional high-silica ZSM-5 shaped catalyst, which were denoted as CAT-1, CAT-2 and CAT-3, respectively. The MTP reaction was performed at 500 °C in a fixed-bed reactor under atmospheric pressure. The WHSV for methanol was 3.0 h−1 with a MeOH/H2O molar ratio of 1[thin space (1/6-em)]:[thin space (1/6-em)]1. After fully deactivated in the MTP reaction, the three kind of spent catalysts were selected as carbon source. The zeolite was removed using a mixture of hydrofluoric acid (10% in water). After 24 h, the obtained monolithic carbon was washed with water several times and dried overnight at 100 °C. The monolithic carbons obtained from CAT-1, CAT-2 and CAT-3 was denoted as HPCMs-1, HPCMs-2 and HPCMs-3, respectively.

2.2 Synthesis of HPCMs supported catalysts

The samples of commercial activated carbon (AC) and HPCMs-1 were used as the support materials. The Fe-based catalyst was prepared by the incipient wetness impregnation method using ethanol aqueous solutions (95 wt%) of iron(III) acetylacetonate (Fe(acac)3) and potassium nitrate (KNO3). The catalyst was obtained after drying at 100 °C overnight followed by calcination in N2 at 500 °C for 3 h to decompose iron and potassium precursors, for which the heating rate was 2 °C min−1. The real Fe and K loading on the HPCMs-1 are 11.4 and 5.7 wt%, respectively, as measured by energy dispersive X-ray (Fig. S1).

2.3 Characterization

Powder X-ray diffraction (XRD) patterns were recorded on a Rigaku Smartlab diffractometer using nickel-filtered CuKα X-ray source at a scanning rate of 0.02° over the range between 5° and 80°. The crystallite phases were identified by comparing the diffraction patterns with the data of the Joint Committee on Powder Standards (JCPDS).

Transmission electron microscopy (TEM) and high resolution transmission electron microscopy (HRTEM) images were taken on a JEM-2100F instrument (JEOL Company) with an acceleration voltage of 200 kV. The samples for TEM analysis were prepared by dipping the copper grids into the ethanol solutions of the samples and drying at ambient conditions.

Scanning electron microscopy (SEM) images were obtained on a Hitachi S-5500 instrument with an acceleration voltage of 3 kV.

Thermo gravimetric analysis (TGA) was performed on an SDT Q600 (TA Instruments, USA) in the temperature range of 25–800 °C under air or N2 at a heating rate of 10 °C min−1.

Ar isotherms at −186 °C were measured in a Quantachrome autosorb-iQ2 gas adsorption analyzer. Prior to the measurement, the samples were degassed in vacuum (p/p0 < 10−7) at 300 °C for 10 h. The Brunauer–Emmett–Teller (BET) method was applied to calculate the total surface area, while the micro–meso porous size distribution was determined from Ar adsorption isotherm by quenched solid density functional theory (QSDFT).

The meso- and macro-porosity of the samples were measured by a mercury porosimeter (AUTOPORE IV 9500, Micromeritics, USA) with two low-pressure stations plus one high-pressure station and a maximum pressure of 33[thin space (1/6-em)]000 psia.

X-ray photoelectron spectroscopy (XPS) was conducted on an ESCALAB 250 (Thermo VG Corporation) using Mg Kα radiation (1253.6 eV, 15 kV, 10 mA, 150 W). The recorded spectra were fitted by a least square procedure to a product of Gaussian–Lorentzian functions. The concentration of each element was calculated from the area of the corresponding peak.

Raman spectra were collected using a Nicolet Almega XR Raman system with a 532 nm excitation laser from Thermo Fisher Scientific Inc.

H2-TPR measurements were carried out with ChemBET Pulsar TPR/TPD equipment (Quantachrome, USA) to analyse the reducibility of the calcined catalysts. Prior to the reduction, the calcined sample (0.10 g) was placed in a quartz tube in the interior of a controlled oven. The sample was flushed with high purity argon at 300 °C for 8 h to remove water and other contaminants then cooled down to room temperature. A gas mixture containing 5 vol% H2 in Ar was passed through the sample at a total flow rate of 30 ml min−1 with a heating rate at 10 °C min−1 up to 900 °C. A cooling trap was placed between the sample and the detector for removal of released water formed during the reduction process.

2.4 Catalytic testing

The catalytic hydrogenation of carbon dioxide was carried out in a pressurized fixed-bed flow reactor where a weighted 1 g catalyst was pretreated by reduction with pure H2 at 500 °C overnight. After the reduction, the feed gas was changed to the mixture of carbon dioxide and hydrogen under the reaction conditions of n(H2)/n(CO2) = 3 (molar ratio); P = 3 MPa; T = 400 °C and the space velocity was 3600 ml g−1 h−1.

The products were analyzed on-line by a gas chromatograph (FULI GC 97). Carbon monoxide, carbon dioxide and methane were analyzed on a carbon molecular sieve column with a thermal conductivity detector (TCD) while methane and C2–C8 hydrocarbons were analyzed with a flame ionization detector (FID) with a HayeSep Q column. Chromatograms were correlated through methane and product selectivity was determined based on carbon.

3 Results and discussion

3.1 Material synthesis and characterization

The schematic of HPCMs synthesis is shown in Fig. 1a. For ZSM-5 zeolite, during the MTP reaction process, the carbon species are mostly polycyclic aromatics. Due to the limitation of micropores, carbon deposits often exist on the surface of the zeolite, leading to severe diffusion restrictions and fast deactivation of catalyst. Although the activity can be enhanced by the calcination treatment, the catalyst activity and stability are difficult to achieve the level of fresh catalyst. Thus, after several regeneration treatments, the catalyst is no longer able to meet industrial requirements, and this kind of catalyst is called spent catalyst. We used spent catalyst as carbon source, after one-step zeolite removal using hydrofluoric acid, the HPCMs were obtained. Fig. 1b shows the image of fresh catalyst, which is cylinder with height of 1–10 mm and diameter of 2 mm. The spent catalyst and HPCMs maintained the macro-morphology of the fresh catalyst, while the yield of HPCMs depends on the coke content of spent catalyst. For spent CAT-1, the content of coke with weight loss temperature greater than 400 °C is 21 wt% (Fig. 2a). After zeolite movement, the yield of HPCMs-1 is about 20 wt%, similar with the coke content of spent CAT-1. The TG and DTG curves (Fig. 2b) show that the weight loss of HPCMs-1 under N2 at 800 °C was only 6 wt%, indicate the low content of oxygen or volatile substances in HPCM-1. The TG curves of it under air confirm that the zeolite could removal completely via hydrofluoric acid treatment.
image file: c5ra26009d-f1.tif
Fig. 1 (a) Schematic of the HPCMs synthesis; image of fresh catalyst (b), spent catalyst (c) and HPCMs (d).

image file: c5ra26009d-f2.tif
Fig. 2 TG and DTG curves of (a) spent CAT-1 under air, (b) HPCMs-1 under air and N2.

Fig. 3 shows the SEM and TEM images of the fresh catalyst and HPCMs. Due to the coke often deposit on the surface of ZSM-5, after zeolite remove treatment, the morphology of HPCMs will reverse copy the morphology of zeolite. For example, if the morphology of zeolite is aggregate (Fig. 3a), sphere (Fig. 3d) or rectangle (Fig. 3g), the HPCMs with reticular (Fig. 3b and c), hollow (Fig. 3e and f) or sheet (Fig. 3h and i) morphology will be obtained.


image file: c5ra26009d-f3.tif
Fig. 3 SEM (a, b, d, e, g, and h) and TEM (c, f and i) images of CAT-1 (a), CAT-2 (d), CAT-3 (g) and HPCMs-1 (b and c), HPCMs-2 (e and f), HPCMs-3 (h and i).

To determine the pore structure of HPCMs, Ar adsorption and desorption isotherms and Hg intrusion curve were measured. For HPCMs-1, the Ar adsorption and desorption isotherms show type III/IV (macropore/mesopore) characteristics (Fig. 4a). The increase in adsorption amount at p/p0 (0.6–0.9) indicates the existence of mesopores, from which calculated mesoporous (2–50 nm) volume is 0.53 cm3 g−1 (Table 1). The further Ar uptake at high p/p0 (0.9–1.0) demonstrates the existence of macropores. To exactly determine the macroporous structure of HPCMs-1, Hg intrusion curve was measured (Fig. 4c), from which calculated macroporous (50–350 nm) volume was 1.39 cm3 g−1. Fig. 4b and d show the micro–meso pore size distribution determined from Ar adsorption isotherm and the macropore distribution was determined from Hg intrusion curve, respectively. In addition, the pore structure of HPCMs-2 and HPCMs-3 were also determined by Ar adsorption–desorption technique, (Fig. 5) indicate all of the three HPCMs were meso–macro porous materials without micropores.


image file: c5ra26009d-f4.tif
Fig. 4 Ar adsorption and desorption isotherms at −186 °C (a), micro–meso pore size distribution (b), Hg intrusion curve (c) and macro pore size distribution (d) of HPCMs-1. The micro–meso porous size distribution was determined from Ar adsorption isotherm by quenched solid density functional theory (QSDFT), and the macroporous distribution was determined from Hg intrusion curve.
Table 1 Textural properties of the samples
Sample code Smicroa [m2 g−1] SBETb [m2 g−1] Vmicroa [cm3 g−1] Vmesoa [cm3 g−1] Vmacroa [cm3 g−1] Vporec [cm3 g−1]
a QSDFT method, micropore (d < 2 nm), mesopore (2 nm < d < 50 nm) and macropore (d > 50 nm).b BET method.c p/p0 = 0.99.d Measured from Hg intrusion, mesopore (24 nm < d < 50 nm) and macropore (50 nm < d < 350 nm).
HPCMs-1 0 218 0 0.53 (0.51d) 0.94 (1.39d) 1.47
HPCMs-2 0 557 0 1.01 1.07 2.08
HPCMs-3 0 253 0 0.59 0.60 1.19
HPCMs-1-650 47 301 0.02 0.45 0.90 1.37
HPCMs-1-750 479 724 0.16 0.60 0.94 1.70
HPCMs-1-850 481 941 0.18 0.72 0.87 1.77



image file: c5ra26009d-f5.tif
Fig. 5 Ar adsorption and desorption isotherms at −186 °C (a and c) and micro–meso pore size distribution (b and d) of HPCMs-2 (a and b) and HPCMs-3 (c and d).

The effect of KOH activation was also estimated. Ar adsorption and desorption isotherms at −186 °C and pore size distributions of HPCMs-1 after KOH activation are shown in Fig. 6a and b. With the rising temperature from 650 to 850 °C, the adsorption isotherms change from type III/IV to combined type I/III/IV (micropore/macropore/mesopore). Compared with HPCM-1, the BET surface area of HPCMs-1-850 increased from 218 m2 g−1 to 941 m2 g−1, mainly of micropores area growth. The micropore volume was also increased from 0 to 0.18 cm3 g−1. That because during the KOH activation, gases such as CO2 and CO were generated, resulting in the formation of micropores,21 meanwhile the mesopore and macropore were still retained after KOH activation, and finally obtained micro–meso–macro porous carbon monoliths as shown in Fig. 6b.


image file: c5ra26009d-f6.tif
Fig. 6 Ar adsorption and desorption isotherms at −186 °C (a) and micro–meso pore size distributions (b) of HPCMs-1 after KOH activation at 650, 750 and 850 °C for 3 h, respectively, KOH/HPMS-1 = 2[thin space (1/6-em)]:[thin space (1/6-em)]1 (weight ratio). The micro–meso pore size distribution was determined from Ar adsorption isotherm by quenched solid density functional theory (QSDFT).

To determine the chemical structure of HPCMs-1, XRD pattern, Raman spectrum and XPS spectra were measured. Before the removal of zeolite, the five characteristic diffraction peaks of MFI topology at 7.8°, 8.8°, 23.0°, 23.9°, and 24.4° clearly indicate the phase of ZSM-5 (Fig. S2, JCPDS: 44-0003). After remove zeolite, Fig. 7a shows the typical XRD patterns of HPCMs-1, the diffraction peaks of MFI topology disappear. The broad XRD peak at 2-theta value of 24.5° was attributed to the (002) reflection of the graphitic-type lattice and the corresponding interlayer spacing (0.36 nm) is slightly larger than that of natural graphite (0.34 nm), which represents well-developed graphitization.22,23 The interlayer spacing could also be measured from HRTEM image (Fig. 7a inset, Fig. S3), which in agreement with the XRD result. The weak XRD peak at 2-theta of 43.5° was attributed to the (101) reflection of carbon structure.


image file: c5ra26009d-f7.tif
Fig. 7 XRD pattern (a), Raman spectrum (b), XPS survey (c) and high-resolution C 1s XPS spectra (d) of HPCMs-1 (inset (a) HRTEM image of HPCMs-1. Inset (c) chart showing the percentages of carbon and oxygen according to XPS data).

The Raman spectrum of HPCMs-1 is shown in Fig. 7b. The peak positions of the D and G bands are 1340 and 1587 cm−1, respectively. The D band is a common feature of disordered carbons, while the G band is related to a graphitic carbon phase with an sp2 electronic configuration.24 The radio of these two bands (ID/IG) is 0.93[thin space (1/6-em)]:[thin space (1/6-em)]1, reflecting the partial graphitization of the carbons in the HPCMs. The XPS spectrum of HPCMs-1 is shown in Fig. 7c. According to the XPS data, atomic percentages of C (96.0 at%) and O (4.0 at%) can be determined. The high-resolution C 1s XPS spectrum showed a dominant peak at 284.5 eV and two small peaks at 285.9 and 288.4 eV (Fig. 7d). The peak at 284.5 eV corresponds to the sp2-hybridized graphitic carbon, while the peaks at 285.9 and 288.4 eV are attributed to C–OH and C[double bond, length as m-dash]O configurations, respectively.25

3.2 HPMCs as the support of Fe-based catalyst for the hydrogenation of carbon dioxide

Fig. 8a and b–d show TEM images of Fe–K/AC and Fe–K/HPCMs-1, respectively, for the commercial activated carbon (AC) as support, the metal oxide particles are of 17 nm mean size, whereas using HPMCs-1 as support, the mean size of metal oxide particles decrease to about 9 nm. The lattice spaces are measured to be 2.5 and 3.0 Å (Fig. 8d), which matches the values of the d-spacing of Fe3O4 (311) and Fe3O4 (220), respectively (JCPDS: 65-3107). Fig. S4 shows carbon (yellow), iron (red) and potassium (green) element mapping images of Fe–K/AC (a–d) and 15Fe10K/HPCMs-1 (e–h), respectively. Compared with Fe–K/AC, the iron and potassium in the sample of HPMCs-1 exhibit more uniform distribution, which is conducive to enhancing the promotion and improves the activity of the catalyst.
image file: c5ra26009d-f8.tif
Fig. 8 TEM (a–c) and HRTEM (d) images of Fe–K/AC (a) and Fe–K/HPCMs-1 (b–d), respectively; (e) XRD patterns of Fe/AC (e-1), Fe–K/AC (e-2) and Fe–K/HPCMs-1 (e-3); (f) H2 TPR profiles of Fe/AC (f-1), K/AC (f-2), Fe–K/AC (f-3) and Fe–K/HPCMs-1 (f-4). The insets in (a) and (b) show the particle size distributions of metal oxide based on measurements of approximately 100 nanoparticles by TEM.

The decrease of particle size of metal oxide supported on the HPMCs-1 was also demonstrated by XRD patterns in Fig. 8e. For the fresh catalysts, the XRD patterns exhibited the characteristic diffraction peaks of Fe3O4 (JCPDS: 65-3107) at 30.1°, 35.5°, 43.2°, 53.5°, 56.9° and 62.6°. The Fe/AC shows a sharp (311) peak, indicating the large particle size of Fe3O4. When the potassium was introduced in the catalyst, the peaks of Fe3O4 became broader, indicate the introduction of potassium is interaction to the enhancement of iron disperse, which is attributed to the interaction of iron and potassium. The wide diffraction peaks of Fe–K/HPCMs-1 suggest that Fe3O4 particle size is much smaller than on sample Fe–K/AC, which is consistent with the TEM and element mapping results.

The reduction behavior of catalysts was studied by H2-TPR. As shown in Fig. 8f, for the Fe–K supported on the AC, the reduction temperature of metal oxide is lower than the mono-metal loading samples. That is because the Fe–K catalyst has a higher metal dispersion, which has been proved by TEM images and XRD patterns. Thus, the catalyst Fe–K/HPCMs has the lowest reduction temperature, this result suggests that the catalyst Fe–K/HPCMs had the highest degree of reduction after reduction with pure H2 at 500 °C overnight.

Table 2 shows the catalytic performances of the carbon supported Fe-based catalysts for CO2 hydrogenation. For mono-metal Fe catalyst (Fe/AC), the conversion of CO2 was very low (5.6%) because of the weak adsorption of iron species to carbon oxide. For mono-metal K catalyst (K/AC), the conversion of CO2 was increase to 15.6, however, due to its weak activation ability to hydrogen, the selectivity of CO is very high (93.6%), mainly occurred reversed-water-gas-shift reaction. When the potassium was introduced in the iron-based catalyst (Fe–K/AC), the synergistic effect of iron and potassium simultaneously enhances the activation of hydrogen and adsorption of carbon dioxide,26,27 increasing the conversion of carbon dioxide to 27.0%. However, because of the uneven distribution of iron and potassium, the selectivity of hydrocarbon has not been improved. As expected, the use of HPCMs-1 as the support significantly increased the conversion of CO2 to 33.4%, decreased the selectivity of CO to 38.9% as well as increased the selectivity of high value C[double bond, length as m-dash]2–4 and C5+ hydrocarbons to 18.0% and 18.1%, respectively. Characterization and catalytic performance results show that the HPCMs is a superior support of FeK for minimizing the nanoparticle size and enhancing the Fe–K interaction for promoting catalytic performance of CO2 hydrogenation.

Table 2 CO2 conversion and selectivity of Fe/AC, K/AC, Fe–K/AC and Fe–K/HPCMs-1, respectively. Reaction conditions: n(H2)/n(CO2) = 3 (molar ratio); P = 3 MPa; T = 400 °C and the space velocity was 3600 ml g−1 h−1, time on stream 5 h
Catalyst CO2 conv. (%) Selectivity (%)
CO CH4 C[double bond, length as m-dash]2–4 C02–4 C5+
Fe/AC 5.6 66.3 24.6 0.4 8.7 0
K/AC 15.6 93.6 4.6 0.1 1.7 0
Fe–K/AC 27.0 92.5 4.2 0.6 2.4 0.3
Fe–K/HPCMs-1 33.4 38.9 13.5 18.0 11.5 18.1


4 Conclusions

In this work, hierarchical porous carbon monoliths have been successfully synthesized by an efficient and low cost strategy from coke-deposited spent zeolite catalyst. The resulting carbon exhibits a controlled morphology, a high degree of graphitization and a meso–macro porous structure. Such hierarchical porous carbon was found to be a superior support of FeK for minimizing the nanoparticle size and enhancing the Fe–K interaction for promoting catalytic performance of CO2 hydrogenation.

The present strategy in this work can be used for preparing a wide range of synthetic hierarchical porous carbon materials, because the spent catalyst with specific channels and morphologies can be selected to obtain the carbon material we need. For example, some spent zeolite catalysts with a large micro-pore size (e.g. Y or beta) may be used to synthesize microporous carbon material with high surface area.

Acknowledgements

The authors thank the financial support from the National Natural Science Foundation of China (21306018, 21503029, 21503027) and the Fundamental Research Funds for the Central Universities (DUT15ZD236, DUT15RC(3)027).

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Footnote

Electronic supplementary information (ESI) available: HRTEM image of HPCMs-1; XRD pattern of spent CAT-1; SEM images, carbon, iron and potassium element mapping images of Fe–K/AC and Fe–K/HPCMs-1, respectively. See DOI: 10.1039/c5ra26009d

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