Li-Jing Zhoua,
Yongcun Zoua,
Guo-Dong Lia,
Xiaoxin Zou*a,
Jun Zhaoa,
Meihong Fana,
Yipu Liua and
Dejun Wangab
aState Key Laboratory of Inorganic Synthesis and Preparative Chemistry, College of Chemistry, Jilin University, Changchun 130012, China. E-mail: chemistryzouxx@gmail.com
bDepartment of Chemistry, Tsinghua University, Beijing 100084, China
First published on 14th May 2014
A porous Co3O4 material with unique octahedron-in-octahedron core–shell-type morphology is prepared via a facile precursor-mediated synthetic route. This material possesses large surface area and good catalytic activity for water oxidation reaction.
Over the past decades, several oxides based on transition metals such as Fe, Ni, Mn and Co have been investigated for water oxidation reaction (WOR).5 Cobalt(II,III) oxide (Co3O4) among them has been shown to be a promising WOR catalytic material due to its high activity, good stability and earth-abundance.6–12 In view of the fact that the WOR with Co3O4 is a heterogeneous catalytic process, considerable amount of research effort was recently made to optimize Co3O4's catalytic performance by increasing its surface area. Large surface area is anticipated to give high surface reactive sites, large contact area with reactants, and thereby improved catalytic activity. To increase Co3O4's surface area, convenient and efficient strategies mainly include (1) making it in nanostructured form,6–9 and (2) creating porous structure in it.10–12 In 2009, Esswein et al. revealed the size-dependent water oxidation activities of Co3O4 nanoparticles.6 Since then, there are several studies on new methods for the preparation of nanostructured Co3O4 WOR catalysts with unsupported, ultrasmall-sized, and/or ligand- and surfactant-free features.7–9 For example, Müller and co-workers synthesized surfactant-free, unsupported Co3O4 nanoparticles (<5 nm) with high WOR activity using a pulsed laser ablation method.8 Besides nanostructured Co3O4 materials, porous Co3O4 materials with large surface areas were also synthesized and applied for water-oxidation applications. Jiao et al. prepared a series of mesoporous silica/carbon supported Co3O4 nanoclusters as efficient WOR catalysts.10 And hard template method was also used by some groups to fabricate mesoporous Co3O4 WOR catalysts.12 Despite many achievements made in this field, as outlined above, template-free synthesis of porous Co3O4 materials with clean surface, large surface area and catalytic activity were not reported.
Herein, we report a facile, precursor-mediated, template-free synthetic route to prepare a porous Co3O4 material (hereafter denoted as Co3O4-1) that possesses an octahedron-in-octahedron core–shell-type morphology, a large surface area, and catalytic activities towards water oxidation. This method involves the synthesis of an octahedron-shaped cobalt alkoxide (denoted as Co-PDO) by the solvothermal self-assembly of Co2+ and 1,3-propanediol (PDO), followed by a simple thermal treatment (200 °C) of the resulting Co-PDO in air to remove organic component in it as well as to form porous Co3O4-1 directly (Fig. 1, see experimental details in ESI†). Previously, some Co3O4 materials with an octahedral morphology were reported, but they had a non-porous structure (or low surface area), and were not used for catalytic water oxidation reaction.13
The Co-PDO precursor used herein was prepared by a solvothermal reaction between cobalt acetate tetrahydrate and 1,3-propanediol (PDO), which served as both a solvent and a reactant. It is worth noting here that the Co-PDO precursor could be formed over wide ranges of both Co2+ concentration (3.1–31 mmol L−1) and reaction temperature (140–200 °C), while the crystal structure and morphology of Co-PDO remained unchanged (see Fig. S1 in ESI†); and this also ensures that the synthesis of Co-PDO is easily controllable and reproducible. Hereafter, Co-PDO denotes the product with Co2+ concentration of 15.5 mmol L−1 and reaction temperature of 160 °C, if not particularly indicated. The structure of the Co-PDO precursor was further characterized by FT-IR spectroscopy, X-ray photoelectron spectroscopy (XPS), and thermogravimetric analysis (TGA) (see Fig. S2–S4†). All the results suggested that the Co-PDO precursor was a crystalline cobalt(II) alkoxide with a cobalt content of ∼22.6 wt% (see ESI† section for detailed discussion of the characterization results); however, its accurate crystal structure has not been resolved yet.
The morphology of the Co-PDO precursor was observed by scanning electron microscopy (SEM). The low-magnification SEM images (Fig. 2A) show that the product consists of octahedron-like particles with a side length of ∼7 μm. The TEM image of the Co-PDO precursor (Fig. 2B) appears as a regularly hexagonal shape, which is in agreement with the Co-PDO's octahedron-like morphology (Fig. S5,† please see a simulation of how an octahedral particle can show a hexagonal shape during TEM measurement).
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| Fig. 2 (A) SEM and (B) TEM images of the Co-PDO precursor, and (C) SEM, (D) TEM, (E) HTEM images and (F) XRD pattern of Co3O4-1. SEM image of a broken Co3O4-1 particle was shown in the inset of (C). | ||
Fig. 2C and S6† show typical SEM images of Co3O4-1, which was synthesized by thermal treatment of Co-PDO at 200 °C. The SEM images reveal that Co3O4-1 maintains the morphology and size of the Co-PDO precursor. However, different from the Co-PDO precursor with a solid structure, the Co3O4-1 material possesses a unique core–shell-type structure with a shell thickness of ∼300 nm, as shown by a broken particle (Fig. 2C, inset and S7†). The TEM image of Co3O4-1 (Fig. 2D) shows a darker hexagonal region at the center and a continuous lighter hexagonal region around the edge of the Co3O4-1 microparticle, indicating again the formation of an octahedron-in-octahedron core–shell-type structure. The HRTEM images (Fig. 2E and S8†) clearly show that nanoparticles with a size of <5 nm are randomly arranged and interconnected in the whole visible area. The observed lattice spacing is about 0.24 nm, which corresponds to the distance between the (311) crystal planes of the cubic Co3O4 phase.
The morphology evolution from Co-PDO's solid structure to Co3O4-1's core–shell-type structure could be explained based on a thermal-driven chemical transformation process, in which the decomposition of Co-PDO and the formation of Co3O4 occur simultaneously. Upon the heat treatment, there would be a large contraction force (Fc) induced by the decomposition of organic components in the Co-PDO precursor (Fig. 1). At the same time, there is also an opposite adhesion force (Fa) that could be attributed to the formation of Co3O4 crystallites, especially at/near the precursor particle–air interface. The synergy of Fc and Fa finally results in the separation of the core and the shell (or the formation of the core–shell-type structure). Similar explanation was also reported by Zhang et al. in a study that showed the formation of ZnMn2O4 ball-in-ball microspheres.14
The complete conversion of Co-PDO into Co3O4 was further confirmed by XRD (Fig. 2F) and FT-IR (Fig. S9†) measurements. It is seen in Fig. 2F that the XRD peaks of Co3O4-1 are perfectly indexed to cubic Co3O4 (JCPDS no. 42-1467). In the IR spectrum of Co3O4-1 (Fig. S9†), those IR absorption bands related to the organic component in Co-PDO completely disappeared (Fig. S2†); and the characteristic IR absorption related to Co3O4 appeared.
The porous structure and surface area of Co3O4-1 were studied by N2-adsorption measurement. The N2 adsorption–desorption isotherms (Fig. 3A) of Co3O4-1 are characteristic of type-IV with H3-type hysteresis loops, demonstrating the presence of a highly porous texture in the material. The corresponding BJH pore-size distribution (Fig. 3B) derived from the desorption isotherm shows a narrow pore-size distribution ranging from 1 nm to 4 nm. It is presumable that the formation of porous structure in Co3O4-1 might be originated from the thermal-driven removal of organic components in Co-PDO and some related structural rearrangement. Furthermore, the BET surface area of Co3O4-1 is ∼190 m2 g−1, demonstrating that Co3O4-1 is a high-surface-area material.
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| Fig. 3 (A) N2 adsorption–desorption isotherms of Co3O4-1 and (B) the corresponding pore size distribution derived from the desorption isotherm. | ||
Next, we investigated the visible-light-driven water oxidation activity of the as-obtained Co3O4 material using the established [Ru(bpy)3]2+/persulfate system (bpy = 2,2′-bipyridine) in a Na2SiF6–NaHCO3 buffer solution (pH = 5.8).15 In this system, [Ru(bpy)3]2+ and persulfate were used as sensitizer and sacrificial electron acceptor, respectively. In addition, [Ru(bpy)3]2+ was reported previously to have the lowest decomposition rate in the Na2SiF6–NaHCO3 buffer solution (pH = 5.8).9,10
For comparative purpose, two more Co3O4 samples were prepared by thermal treatment of Co-PDO at 300 and 400 °C, respectively, and correspondingly they are labeled as Co3O4-2 and Co3O4-3 (see material characterization in Fig. S10†). Furthermore, the catalytic activities of Co3O4-1, Co3O4-2, Co3O4-3 and a commercially available Co3O4 sample (Com-Co3O4) were measured under the same condition by keeping the same weight of samples in each case. Before photocatalytic experiments, several control experiments such as without a catalyst, light, [Ru(bpy)3]2+, or persulfate were performed, and in these cases no O2 evolution was detected. The results demonstrate that in such a visible-light-driven water oxidation system, each of these components is required.
As shown in Fig. 4A, all the four Co3O4-based materials exhibit obvious catalytic activities towards WOR (or oxygen evolution) under visible-light irradiation. The catalytic activities of the materials towards WOR increase in the order of Com-Co3O4 ≪ Co3O4-3 < Co3O4-2 < Co3O4-1. To be precise, Co3O4-1, Co3O4-2, Co3O4-3 and Com-Co3O4 afford O2 evolution rates of 211.5, 134.5, 68.1 and 12.2 μmol g−1 min−1, respectively. Thus, the activity of Co3O4-1 (the most active catalyst in our work) can be roughly said to be ca. 17.3 times as high as that of Com-Co3O4. This trend in the catalytic activity of the materials would correlate with the materials' surface areas, as the BET surface area of Co3O4-1 is 190 m2 g−1, which is much larger than those of Co3O4-2 (61 m2 g−1), Co3O4-3 (20 m2 g−1) and Com-Co3O4 (<10 m2 g−1). To further compare the catalytic activities of the three Co3O4 materials we synthesized, their BET surface areas were used to normalize the O2 evolution rates. The normalized O2 evolution rates are 1.1, 2.2 and 3.4 μmol m−2 min−1 for Co3O4-1, Co3O4-2, Co3O4-3, respectively. This result clearly demonstrates that the surface area of Co3O4 material is not the only factor affecting its catalytic activity. Considering the structural difference of the three materials, the crystallinity of Co3O4 might be the other important factor affecting the catalytic activity. A higher crystallinity, which is generally achieved at a higher reaction temperature, could decrease the recombination of photo-generated electron–hole pairs, and thus improve the catalytic activity. The above results indicate that simultaneous achievement of high surface area and high crystallinity in a Co3O4 material might be a feasible strategy to enhance its catalytic activity towards water oxidation.
To further assess the catalytic activity of the Co3O4-1 material, its turnover frequency (TOF) was calculated based on the assumption that all the Co ions present in the material were catalytically active (this method was also used previously3). The as-obtained TOF might be a gross underestimation, because not every Co in the material is catalytically accessible or active. The TOF of Co3O4-1 was found to be 2.86 × 10−4 S−1 (Table S1†), which is comparable with those of the existing Co3O4-based catalysts for photochemical water oxidation (e.g., 2.4 × 10−4 S−1 for a mesoporous Co3O4 material;12a 2.12–4.05 × 10−4 S−1 for porous silica/carbon-supported Co3O4 nanoclusters10). However, the TOF value of Co3O4-1 is lower than those of Co3O4 materials that were used for electrochemical water oxidation (e.g., 7.8 × 10−3 for Co3O4 film;16a 2.76 × 10−2 for Co3O4 electrode;16b 9.3 × 10−3 for Co3O4 nanoparticle6).
The stability of the Co3O4-1 catalyst was demonstrated by a recycling experiment (Fig. 4B). Although Co3O4 is known to be unstable at neutral and lower pH,17 our results indicate that our material Co3O4-1 is stable for up to 30 minutes (six cycles) under our experimental conditions. But further catalytic experiment shows that the catalytic activity of Co3O4-1 starts to decrease. To find out the reason behind the decrease of catalytic activity, the sample after catalytic reaction was carefully characterized (Fig. S11†). After the catalytic water oxidation reaction, the material, e.g., Co3O4-1, did not show any change in its crystal structure (see XRD pattern in Fig. S11A†). The octahedron-like morphology of Co3O4-1 was also largely maintained after catalytic reaction (see SEM in Fig. S11B†). But there seemed be some impurities that were deposited on the Co3O4-1 particles' surface (Fig. S11B†). Further XPS characterization (Fig. S11C and D†) demonstrated that a considerable amount of silica were present in the sample after catalytic reaction. The formation of silica may be due to the hydrolysis of Na2SiF6 in the buffer during photolysis.12a Silica on the surface of Co3O4-1 particles will reduce the surface reactive sites of the material, leading to the decrease of the catalytic activity.
Footnote |
| † Electronic supplementary information (ESI) available: Experimental details and supporting results. See DOI: 10.1039/c4ra02134g |
| This journal is © The Royal Society of Chemistry 2014 |