Takamichi Matsuno*abc,
Gen Koinumaa,
Hiroaki Wadaa,
Atsushi Shimojima
abc and
Kazuyuki Kuroda
ab
aDepartment of Applied Chemistry, Faculty of Science and Engineering, Waseda University, 3-4-1 Okubo, Shinjuku-ku, Tokyo 169-8555, Japan. E-mail: matsuno@aoni.waseda.jp
bKagami Memorial Research Institute for Materials Science and Technology, Waseda University, 2-8-26 Nishiwaseda, Shinjuku-ku, Tokyo 169-0051, Japan
cWaseda Research Institute for Science and Engineering, Waseda University, 3-4-1 Okubo, Shinjuku-ku, Tokyo 169-8555, Japan
First published on 18th August 2025
Zirconia exhibits important properties such as catalytic activity, ionic conductivity, and dielectric properties. Nanoporous zirconia, with its high surface area and large pore volume, is attracting attention for catalysts and separation materials. Precise pore size control is crucial for the applications; however, achieving control within the range of tens of nm remains difficult. In this study, znanoporous carbon was used as a nanoscale scaffold onto which Zr species were deposited with nanometer thickness, followed by calcination for carbon removal and zirconia crystallization, thereby yielding ordered nanoporous zirconias. This process is crucial for forminghighly ordered nanoporous zirconias with improved pore size control and uniformity.
Mesoporous zirconia with pore diameter of several nanometers has been prepared using surfactant micelles11,12 and mesoporous silica13,14 as templates, while the formation of nanopores of several hundred nanometers is achieved using polymer particles as templates.15–17 However, these methods are not suitable for controlling the pore size in the intermediate range from low tens of nanometers to several tens of nanometers, and the preparation of mesoporous zirconia with pore sizes in this region has been limited.20,21 In previous reports, assemblies of silica nanospheres were used as templates to produce mesoporous zirconia. Randomly arranged spherical pores were formed using randomly assembled silica nanospheres,20 while an inverse opal structure was formed using silica colloidal crystals (SCCs) with face-centered cubic (fcc)-packed silica nanospheres.21 However, the smallest size of applied silica nanosphere was 34 nm,21 and the pore size distribution of mesoporous zirconia calculated from N2 adsorption–desorption isotherms was broad. Therefore, nanoporous zirconia with well-controlled pore sizes in the range of low tens of nanometers to several tens of nanometers is still a missing link.
In this study, three-dimensionally ordered nanoporous zirconia with a pore size range from low tens of nanometers to several tens of nanometers was prepared by precipitating zirconia onto the pore walls of nanoporous carbon (Scheme 1). Generally, inverse replicas are obtained when nanoporous materials are used as templates,25 although replication from one inverse opal structure to another has been reported on a larger scale in pore diameter (∼300 nm).17 Using our present method, we succeeded in replicating the template structure across the meso to macro scale by uniformly and thinly coating zirconia on the surface of a carbon template at the nano-level with a simple incipient wetness infiltration method, thereby achieving high porosity and uniform nanopores. The uniform zirconia coating was achieved by using a zirconium butoxide 1-butanol solution as a precursor, which has a relatively low surface tension and is believed to spread thinly on hydrophobic carbon surfaces. The nanoporous zirconia obtained via hydrolysis, condensation, and calcination exhibited narrow pore size distributions, confirming the preparation of nanoporous zirconia with higher regularity over a broader range of pore sizes than previous methods.
TEOSadd = TEOSseed × (Dobj3/Dseed3 − 1) |
The resulting silica nanosphere dispersions were dried and calcined at 600 °C in air for 6 h (temperature rise and fall rate is 1.6 °C min−1) to remove THAM and obtain SCCs (sample names are denoted as SCC-x, where x is the sphere size). The characterization of the SCCs is shown in SI.
The powder XRD pattern of C–ZrO2-66 (Fig. 1a) displays broad peaks derived from amorphous carbon as well as broad peaks similar to those of tetragonal ZrO2 (t-ZrO2, ICDD card no. 00-050-1089), indicating that the sample is poorly crystalline.
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Fig. 1 (a) XRD pattern (bottom: simulated pattern), (b) SAXS pattern, (c) N2 adsorption–desorption isotherms, and (d) BJH pore diameter distributions of C–ZrO2-66 (○: adsorption, ●: desorption). |
In the FT-IR spectrum of C–ZrO2-66 (Fig. S5, SI), a broad C–O stretching28 band around 1200 cm−1 and a CC stretching28 band around 1600 cm−1 were observed, as in the carbon template. The slight absorption band around 500 cm−1 is attributed to the Zr–O vibration18 of the Zr–O–Zr bond. When considered together with the FT-IR spectrum of hydrolyzed-Zr(OBu)4, which was obtained without using a template, the weak absorption intensity of the Zr–O–Zr bond in C–ZrO2-66 may be due to absorption by carbon. In the IR spectrum of hydrolyzed-Zr(OBu)4, absorption bands arising from the –CH2– and –CH3 groups of butanol and butoxy groups, as well as those from C–OH and C–O–Zr groups,29,30 were not observed, suggesting that hydrolysis and polycondensation occurred sufficiently. The absorption bands at 1340 and 1550 cm−1 are attributed to Zr–OH vibrations.31,32 TG-DTA measurements of hydrolyzed-Zr(OBu)4 showed a weight loss of about 27% (Fig. S6a, SI). Considering that a 23% weight loss occurs during the dehydration and condensation of Zr(OH)4 to ZrO2, the observed 27% weight loss is attributed to the dehydration of adsorbed water and additional dehydration condensation, suggesting that the composition is close to ZrO2. Hydrolysis and polycondensation of Zr(OBu)4 are thought to proceed similarly in the carbon template, forming a poorly crystalline zirconium oxide containing Zr–OH.
The SEM image of C–ZrO2-66 (Fig. 2a) shows an increase in the pore wall thickness of the porous carbon (Fig. S3c, SI). The TEM image (Fig. 2b) revealed that the pore wall surface of the inverse opal carbon was coated with a layer several nanometers thick that exhibited different contrast (the region surrounded by the yellow dotted lines). In addition, the contrast was uniform throughout the particles (TEM, Fig. 2c). The HAADF-STEM image of C–ZrO2-66 (Fig. 2d) also showed a porous structure with spherical nanopores similar to that of the inverse opal carbon. EDS elemental mapping of the same view (Fig. 2e–g) shows that carbon and Zr are uniformly present in the pore wall region. In the carbon mapping, the contrast is stronger in the regions where the pore walls are thicker, such as the octahedral and tetrahedral sites in the fcc structure. However, Zr species are uniformly distributed, showing no preference for either octahedral or tetrahedral sites. This is particularly obvious in the overlaid image (Fig. 2g). This result indicates that Zr species uniformly coat the pore wall surface of the nanoporous carbon.
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Fig. 2 (a) SEM image, (b) and (c) TEM images, (d) HAADF-STEM image, and (e–g) EDS elemental mapping of C–ZrO2-66. The yellow dotted lines in (c) visualize the boundary of the contrast. |
The N2 adsorption–desorption isotherms of C–ZrO2-66 (Fig. 1c) were type IV(a), as in the case of the inverse opal carbon (Fig. S4, SI), but the drop in the desorption isotherm from P/P0 = 0.9 to 0.8 was gradual, and a steep drop was observed at a relative pressure of 0.45 due to cavitation. The pore size distribution was calculated by the BJH method (Fig. 1d), and a peak at ∼60 nm was observed from the adsorption isotherm, which is close to that of the inverse opal carbon. Using the desorption isotherm, a broad peak from 18 to 60 nm was observed. These results suggest that the window pores connecting the spherical pores became smaller due to the deposition of zirconia on the pore wall surface. The most important point derived from the N2 adsorption–desorption measurement is that zirconia does not fill the window pores of the inverse opal carbon.
The T-SAXS pattern of C–ZrO2-66 (Fig. 1b) shows peaks at the same q values as those of the inverse opal carbon, confirming that the pore structure is unchanged. However, the peak intensity of the 220 diffraction of the fcc structure decreased, while that of the 311 diffraction increased relatively. This change could be caused by the uniform coating of zirconia on the carbon. The presence of zirconium oxide, with a relatively high electron density, on the carbon surface may have caused a change in the scattering intensity of each diffraction, but the details are uncertain.
The above results collectively confirm that zirconium oxide uniformly coated the pore wall surface of the inverse opal carbon. The factors contributing to the uniform coverage are considered to be the low surface tension of the Zr(OBu)4 1-butanol solution and its affinity for the hydrophobic carbon surface. As a result, the Zr(OBu)4 solution introduced into the pores was able to wet the pore wall surface uniformly, and hydrolysis and polycondensation of Zr(OBu)4 on the pore wall progressed.
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Fig. 3 (a) XRD pattern, (b) SAXS pattern, (c) N2 adsorption–desorption isotherms, and (d) BJH pore diameter distributions of P-ZrO2-66 (○: adsorption, ●: desorption). |
SEM and TEM images (Fig. 4a–d) show that the porous structure of the inverse opal carbon with regularly arranged spherical pores was replicated. The pore size was ∼40 nm, approximately a 40% decrease from that of the inverse opal carbon (66 nm). The SAED patterns (Fig. 4c) display ring patterns assigned to t-ZrO2. The lattice fringe observed in the high-magnification TEM image (Fig. 4d) confirmed that the pore walls were composed of microcrystalline ZrO2 with sizes of a few nanometers, which is close to the crystallite size estimated from the XRD results.
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Fig. 4 (a) and (b) SEM images and (c) and (d) TEM images of P-ZrO2-66 (insets: SAED pattern and FFT pattern). |
The T-SAXS pattern of P-ZrO2-66 (Fig. 3b) shows peaks attributable to an fcc structure, confirming that the porous structure of IOC-66 was replicated. In addition, peak shifts to higher angles compared to IOC-66 were observed, confirming a ∼40% shrinkage of the structural period. This volume shrinkage is likely caused by the removal of the scaffold carbon and is consistent with shrinkage estimates from electron microscopy observations. Similar to C–ZrO2-66, the 220 diffraction intensity was weaker than that of IOC-66, suggesting that the porous structure deviates from an ideal inverse opal structure. Since the volume of tetrahedral and octahedral sites was observed to be significantly smaller than that of the IOC-66 from the TEM image (Fig. 4c), it is possible that the scattering intensity derived from these sites is changed, resulting in the characteristic SAXS pattern.
Based on the N2 adsorption–desorption measurement (Fig. 3c), an uptake near P/P0 = 0.9 on the adsorption isotherm and a steep drop near P/P0 = 0.8 on the desorption isotherm were observed. The BET specific surface area and pore volume were calculated to be 133 m2 g−1 and 0.64 cm3 g−1, respectively. Although the BET area is not particularly high compared to that of previously reported mesoporous ZrO2, the pore volume is larger14 because of the porous structure similar to the inverse opal structure. The BET area and pore volume are much larger than the calculated values for the ideal inverse opal structure (70 m2 g−1 and 0.47 cm3 g−1). This is because the mesoporous zirconia produced is composed of small crystallites, resulting in high surface roughness and thin pore walls. The BJH method (Fig. 3d) confirmed that the pore size distribution was relatively narrow, indicating the formation of uniform nanopores. Peaks were observed at around 33 nm from the adsorption isotherm and at 11 nm from the desorption isotherm. The 33 nm pore is several nanometers smaller than the spherical pore size observed by electron microscopy, suggesting that the pore size was underestimated. The 11 nm pore is thought to originate from window pores connecting spherical pores.
Based on the above results, the preparation of three-dimensionally ordered mesoporous zirconia with regularly arranged spherical pores of ∼40 nm in diameter was confirmed. The mesopores are more uniform compared to those reported previously using SCCs as a template.21 This difference may be due to variations in the formation process of mesoporous zirconia. In previous studies using SCCs as templates, zirconia microcrystals were formed by thermal decomposition of the precursor in the confined nanospaces of a rigid template, resulting in poor contact between crystallites due to volume shrinkage, and the structure may have collapsed when the template was removed (Fig. 5, top) (the experimental results are shown later). On the other hand, in the present system using nanoporous carbon as a scaffold, the volume decreases by carbon removal, resulting in the formation of three-dimensional continuous pore walls composed of poorly crystalline zirconia. The subsequent crystallization process facilitates the formation of well-connected zirconia crystallites (Fig. 5, bottom).
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Fig. 5 Schematic image of the presumed crystallization and template removal process using silica or carbon templates. |
The above results are expected to be useful in investigating the correlation between pore size and catalytic activity in the future. This synthesis method is also considered effective for compositions that are difficult to prepare using silica as a template. For example, this method can be applied to silica and titania (TEOS and Ti(O-iPr)4 were used instead of Zr(OBu)4) to prepare three-dimensionally ordered mesoporous materials (Fig. S7, SI). Because it is difficult to control the pore size in the range of several tens of nanometers in both cases, this method is expected to extend the scope of ordered nanoporous metal-oxide materials. In previously, control over pore size and pore wall thickness using persistent micelle templates or block copolymer templates has been reported for aluminosilicate, TiO2, Nb2O5 and niobium tungsten oxide.34,35 These methods offer advantages in that mesostructures can be formed through the mixing of templates and precursors, followed by self-assembly, and a variety of pore architectures can be achieved. In contrast, the present method offers several advantages. First, it does not require the synthesis of block copolymers and instead relies on a simple sol–gel reaction followed by heating and calcination. Second, it eliminates the need to adjust the interactions between precursors and block copolymers or micelles in solution depending on composition, which may allow broader applicability to various inorganic oxides. Furthermore, because the structure of monodispersed silica nanospheres is replicated, precise control over the pore size distribution and the structural order can be achieved.
After calcination, both samples, P-ZrO2-28 and P-ZrO2-109, were obtained as white powders. Powder XRD patterns (Fig. S10a and b, SI) show that the major peaks are assigned to t-ZrO2, and the crystallite sizes of P-ZrO2-28 and P-ZrO2-109 are 6.8 nm and 7.5 nm, respectively, which are similar to the crystallite size of P-ZrO2-66 as calculated by the Scherrer equation. Peaks attributable to m-ZrO2 were also observed as a minor phase.
The SEM (Fig. 6a and c) and TEM (Fig. 6b and d) images of both samples show regularly arranged spherical nanopores, indicating successful replication of the porous structure of the template. The SAED patterns are ring patterns assignable to t-ZrO2 in both samples. The respective pore diameters estimated from the TEM images were 14 nm (P-ZrO2-28) and 74 nm (P-ZrO2-109), indicating shrinkage of the structure. For P-ZrO2-28, although the ordered porous structure derived from the template carbon was observed, some regions exhibited less regularity (SEM, Fig. S11, SI).
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Fig. 6 (a) SEM image and (b) TEM image of P-ZrO2-28 and (c) SEM image and (d) TEM image of P-ZrO2-109 (inset: SAED pattern). |
In the T-SAXS patterns of P-ZrO2-28 and P-ZrO2-109 (Fig. S9, SI), retention of the fcc structure was confirmed. The calculated distances between nanopore centers in P-ZrO2-28 and P-ZrO2-109 are 16 nm and 82 nm, respectively, which are about 43% and 25% smaller than the pore sizes of the template carbon, respectively. These results are consistent with the SEM and TEM observations.
N2 adsorption–desorption measurements of P-ZrO2-28 and P-ZrO2-109 show type IV(a) isotherms, and the BJH pore size distributions confirmed the presence of uniform mesopores (Fig. S10c–f, SI). Steep uptake and drop were observed in both samples as well as in P-ZrO2-66. BET area and pore volime were calculated to be 121 m2 g−1 and 0.3 cm3 g−1 (P-ZrO2-28), and 90 m2 g−1 and 0.7 cm3 g−1 (P-ZrO2-109). The BET area and pore volume of P-ZrO2-28 were smaller than those of P-ZrO2-66 (133 m2 g−1 and 0.64 cm3 g−1), suggesting that partial collapse of the porous structure occurred.
According to the above results, ordered nanoporous zirconia with fcc-arranged spherical pores ranging from about 16 nm to 82 nm was successfully prepared. The less regular structure observed in P-ZrO2-28 may be due to the large crystallite size relative to the structural period. The crystallite sizes calculated from XRD patterns using the Scherrer equation were approximately 7 nm for P-ZrO2-28, 66, and 109, showing no significant difference. On the other hand, as the structural period decreases, the number of crystallites constituting the pore wall of each spherical pore also decreases. Therefore, in P-ZrO2-28, the reduced number of contact points between crystallites may have resulted in regions where the pore structure could not be maintained.
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Fig. 7 (a) SEM image, (b) TEM image (inset: SAED pattern), (c) XRD pattern (bottom: simulated patterns), and (d) SAXS pattern of P-ZrO2-66-SiO2. |
Preparation of ordered nanoporous zirconia using a ZrOCl·8H2O precursor was also attempted according to a previous report,21 but a regular structure was not obtained (Fig. S13, SI). Some regions replicated the porous structure of the template (SEM, Fig. S13c and d, SI), but these were minor. It is possible that unclarified factors in the experimental conditions or the use of silica nanospheres with a size of 28 nm—slightly smaller than the previously reported size (34 nm)21—limit the formation of porous structures.
These results show that inverse opal zirconia was not obtained when SCCs were used as a template, supporting the aforementioned discussion on the influence of the templates. Therefore, the present method using carbon as a nanoscale scaffold is significant for controlling porous structures.
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