Masato
Machida
*,
Kiyotaka
Kawamura
,
Tomoatsu
Kawano
,
Donjie
Zhang
and
Keita
Ikeue
Department of Applied Chemistry and Biochemistry, Graduate School of Engineering Sciences, Kumamoto University, Kumamoto, 860-8555, Japan. E-mail: machida@chem.kumamoto-u.ac.jp; Fax: +81-96-342-3651; Tel: +81-96-342-3651
First published on 23rd June 2006
Surfactant-assisted synthesis of the oxysulfate Pr2O2SO4 with a large oxygen-storage capacity was studied with the aim of increasing the rate of redox cycles at lower temperatures. From an aqueous solution of nitrate, Pr-based surfactant mesophases templated by dodecyl sulfate anion (DS = C12H25OSO3−) were synthesized using ammonia or urea as precipitants. The precipitated mesophases, Pr-DS-NH3 and Pr-DS-N2H4CO, exhibited ordered layered structures with interlayer spacings of 2.63 and 3.68 nm, respectively, suggesting alternative stacking of a Pr hydroxide layer and a DS layer. The different interlayer spacing can be explained by the fact that Pr-DS-NH3 with the composition Pr2(OH)5(DS)·2.5H2O contains monolayers of DS, whereas Pr-DS-N2H4CO contains bilayers of DS. As was revealed by EXAFS and FT-IR results, the sulfate head group of each DS is strongly bound to uncoordinated Pr3+, so that heating of Pr-DS-NH3 could directly yield single-phase Pr2O2SO4 at a low temperature (500 °C). In contrast to the macropores (≥12 nm in size, 8 m2 g−1) of Pr2O2SO4 prepared by calcining Pr2(SO4)3, Pr-DS-NH3 after calcination showed pores of 2–3 nm in size and a larger surface area (28 m2 g−1). The microstructure is very effective in accelerating the solid–gas reaction in oxygen release as well as storage processes, which enables the present system to work at temperatures ≤600 °C, compared to ≥700 °C required for Pr2O2SO4 prepared from Pr2(SO4)3.
| Ln2O2SO4 ⇄ Ln2O2S + 2O2 |
Such oxygen-storage/release cycles between oxysulfate and oxysulfide are characteristic of the lanthanides. Ln oxysulfates (Ln = La, Pr, Nd and Sm) can be prepared from the corresponding sulfates and are thermostable up to 1000 °C. However, the primary drawback is that a higher operation temperature (ca. 800 °C) is necessary, whereas CeO2–ZrO2 can work even below 400 °C. Our study has therefore been focused on structural modification to achieve a lower redox temperature. Among Ln oxysulfates, the Pr system has the lowest possible operational temperature,10 probably because the redox between Pr3+ and Pr4+ at the surface can promote the redox of sulfur. Impregnation of noble metals, which activate reducing agents as well as oxygen, can further accelerate the redox cycles.9 These modifications can reduce the temperature to less than 700 °C, but further improvement may be achieved by microstructural modification, because Pr oxysulfate obtained from the sulfate has a low surface area (<10 m2 g−1). The creation of pores to increase the specific surface area would thus be essential to reduce the redox temperature.
In this work, we have studied the preparation of porous Pr oxysulfate by applying the surfactant-assisted synthesis of layered mesophases consisting of Pr hydroxide and dodecyl sulfate (DS = C12H25OSO3−). Since the discovery of the mesoporous silicas known as MCM-41,11,12 various surfactant mesophases have been synthesized as precursors to yield mesoporous materials including Ln oxides.13,14 In such a surfactant-assisted pathway, part of the surfactant headgroup is known to be incorporated into the final material after heat treatment.13 In the present study, we therefore expected the surfactant to act not only as a template, but also as a reagent to yield stoichiometric Pr oxysulfate by using the interaction between a DS sulfate head group and a Pr hydroxide. The structure and its evolution to the oxysulfate by thermal decomposition were studied by means of XRD, FT-IR, TG, EXAFS, SEM, and adsorption measurement. Finally, dynamic redox cycles were carried out to evaluate the effect of the porous structure on the oxygen-storage characteristics.
The precipitate thus obtained was collected by centrifugal separation, washed thoroughly with ion-exchanged and distilled water, dried by evacuation at room temperature, and finally heated in air. Pr2O2SO4 was also synthesized by heating commercial Pr2(SO4)3·nH2O at 900 °C for 5 h in air (Pr-SO4). The Pr2O2SO4 thus obtained was impregnated with an aqueous solution of hydrogen palladium nitrate and then calcined at 450 °C to produce Pd-loaded samples (1 wt% loading).
The crystal structure was identified by use of a powder X-ray diffractometer (XRD, Rigaku Multiflex) with monochromated CuKα radiation (30 kV, 20 mA). Energy dispersive X-ray fluorescence analysis (XRF, Horiba MESA-500W) was used to determine the S/Pr ratio. The thermal decomposition of the as-prepared samples was studied by thermogravimetry (TG, Rigaku 8120). FT-IR spectra were recorded on a Jasco FTIR-610 spectrometer using a KBr method. The microstructure was observed by scanning electron microscopy (SEM, JEOL JSM6060LV). The BET surface area and pore size distribution were calculated from N2 adsorption isotherms measured at 77 K (Bel Japan, Belsorp).
X-Ray absorption spectra of the Pr LIII-edge were recorded on a BL-7C instrument at the Photon Factory of the High Energy Accelerator Research Organization at Tsukuba (Proposal #2004G088), with a ring energy of 2.5 GeV and a stored current of around 300–450 mA. A Si(111) double-crystal monochromator was used. The incident X-ray was focused and the higher harmonics were removed by the total reflection on a Rh–Ni composite mirror. Pr LIII-edge spectra were recorded at room temperature in transmission mode. The incident and transmitted X-rays were monitored by ionization chambers filled with N2/He (30 : 70) and N2 gases, with lengths of 17 and 31 cm, respectively. A sample was pressed into a disk (diameter 10 mm) after its volume was adjusted by boron nitride powder to give an appropriate absorbance at the edge energy for the XAFS measurement. The XAFS data were processed by a REX 2000 program (Rigaku). The EXAFS oscillation was extracted by fitting a cubic spline function through the post-edge region. The k3-weighted EXAFS oscillation in the 3.0–10.8 Å−1 region was Fourier-transformed. Phase shifts and backscattering amplitudes were obtained from EXAFS data of Pr2O2SO4 and Pr2(SO4)3 for Pr–O, Pr–S, and Pr–Pr. Data analysis was performed by the multiple shell fitting in r-space (1.4 < r < 4.7 Å, 3.0 < k < 10.8 Å−1).
Dynamic oxygen-release and storage cycles for Ln2O2SO4 were studied by the use of a microbalance (Rigaku 8120) connected to a dual-gas supplying system. The oxysulfate sample (ca. 10 mg) was firstly heated in a stream of N2 up to 600 °C, where a constant weight was attained within 30 min. Then, the gas feed to the sample was switched between 5% H2/He and 20% O2/He, balanced by N2 supplied at 20 cm3 min−1, and the sample weight recorded at this temperature. During the measurement, N2 was passed through the balance chamber to protect the weighing mechanism.
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| Fig. 1 XRD patterns of a) as-prepared Pr-DS-NH3 and b) as-prepared Pr-DS-N2H4CO. | ||
Precipitation using urea (Pr-DS-N2H4CO) also yielded a layered structure, but the periodicity (3.68 nm) was much larger (Fig. 1b). The intensity of diffraction peaks were 8 times larger than those of Pr-DS-NH3, suggesting higher structural ordering in the mesophase composite. However, the purity of as-prepared Pr-DS-N2H4CO must be low due to the co-precipitation of PrCO3OH, which would originate from the CO2 evolved during the hydrolysis of urea. In the following experiment, Pr-DS-NH3 was therefore used as a precursor of the oxysulfate (Pr2O2SO4). The crystallinity of the Pr-DS-NH3 was dependent on the time and temperature of the post-precipitation aging; the mesophase resulting from aging at 40 °C for 30 h exhibited the highest X-ray diffraction intensities.
Fig. 2 shows the XRD patterns of Pr-DS-NH3 after heating in air. The disappearance of the (00l) peaks at ≤200 °C indicates that the layered structure had totally collapsed to yield a non-crystalline phase. Nevertheless, the S/Pr ratio remained almost constant at ca. 0.5 at elevated temperatures, suggesting that DS head sulfates are strongly bound to Pr. The non-crystalline phase remained up to 400 °C, but single-phase Pr2O2SO4 was finally formed at 500 °C. Fig. 3 compares TG profiles of Pr-DS-NH3 and Pr-SO4 in a stream of 20% O2/N2. The hydrous phase of Pr-SO4 (Pr2(SO4)3·nH2O) exhibited several endothermic weight losses due to dehydration (≤300 °C) and decomposition of 2 mol-sulfate mol−1 to form Pr2O2SO4 (800–950 °C) that was stable up to 1100 °C. By contrast, Pr-DS-NH3 exhibited dehydration (≤100 °C), elimination of organic moieties (200–250 °C), and final dehydroxylation (300–400 °C). Another weight loss with an exothermic peak at ca. 600 °C would seem to result from the combustion of carboneous deposits originating from organic moieties. A final product of Pr-DS-NH3 was also a single phase of Pr2O2SO4, the thermal stability of which was as same as that from Pr-SO4. These results show that Pr-DS-NH3 can produce Pr2O2SO4 at the very low temperature of 500 °C, compared to the heating above 900 °C required for the decomposition of Pr2(SO4)3 to Pr2O2SO4. With each weight loss and the S/Pr ratio taken into consideration, a possible chemical formula of Pr-DS-NH3 could be as Pr2(OH)5(DS)·2.5H2O. The calculated total weight loss to Pr2O2SO4 should be 38%, which is in good agreement with the experimental value (36%).
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| Fig. 2 XRD patterns of a) as-prepared Pr-DS-NH3, and after heating at b) 100 °C, c) 200 °C, d) 400 °C and e) 500 °C. | ||
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| Fig. 3 TG profiles of a) Pr-SO4 and b) Pr-DS-NH3 measured at 10 °C min−1 in 20% O2/N2. | ||
Fig. 4 compares the infrared spectra of a) SDS and b) Pr-NH3-DS in the sulfate headgroup band region of 1400–700 cm−1. The sulfate headgroup with the C3v point group showed characteristic absorption bands due to the asymmetric and symmetric S–O stretching mode (νas(E): 1250 cm−1, νas(A): 1220 cm−1 and νs(A): 1085 cm−1).16 Here, the directions of the transition dipole moment for the E and A vibrational modes are orthogonal to each other. For Pr-DS-NH3, the positions of the νas(E) mode (1250 cm−1) were almost unchanged, but the other νas(A) and νs(A) modes were significantly shifted to lower wavelengths, 1204 and 1066 cm−1, respectively. The band shift is likely associated with an electrostatic effect involving coordination of the sulfate headgroup oxygen atom to Pr3+. Similar shifts of these infrared bands have been reported for DS bound to Fe3+,17 TiO2,18 and Al2O3.19 Li and Tripp18 have reported spectral changes of admicellar DS adsorbed onto a positively charged TiO2 surface with a DS-chain axis near normal to the surface. According to their interpretation, the two A absorptions (νas and νs) shifted, because the transition dipole moments for the vibrations are near normal to the TiO2 surface, and thus would directly be affected by coordination of the sulfate headgroups onto the positively charged site. By contrast, the change in the E vibration of the νas absorption would not be significant, because the transition dipole moment for the vibration in the lateral direction would not be affected by the surface charge. By applying this consideration, the Pr-DS-NH3 phase should contain admicellar DS moieties, the headgroups of each DS being bound to Pr3+ located in the two-dimensional Pr hydroxide layer.
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| Fig. 4 FT-IR spectra of a) SDS and b) Pr-DS-NH3. | ||
On the basis of the chemical formula, Pr2(OH)5(DS)·2.5H2O, and structural analysis, we have proposed a structural model of Pr-DS-NH3 as shown in Fig. 5, which consists of two different layers of Pr hydroxide and DS. The Pr hydroxide moiety appears to be similar to the hexagonal form of the Pr trihydroxides in the space group P63/m with lattice parameters, a0 = 0.646 nm and c0 = 0.377 nm.15 The S/Pr ratio of 0.5 suggests that a 2
×
c0 thick Pr hydroxide layer is stacked alternately with a DS moiety. This is consistent with the fact that the XRD peaks due to (h0l) and (00l) of Pr(OH)3 were too weak to be observed. The periodicity along (hk0) would only be preserved in the Pr-DS-NH3 mesophase. Pr3+ in Pr(OH)3 is 9-coordinate, but Pr3+ exposed on the surface of each Pr hydroxide layer is coordinated by a sulfate terminus, –OSO3, instead of 3
×
OH; their electrostatic interaction is supported by the shift of infrared bands ascribable to S–O stretching modes. This interaction is so strong that the S/Pr ratio of Pr-DS-NH3 remains constant even after calcination, allowing the facile formation of Pr2O2SO4 at low temperatures.
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| Fig. 5 A structural model of Pr-DS-NH3. | ||
Subtracting the thickness of a Pr hydroxide layer (2
×
c0 = ca. 0.75 nm) from the interlayer distance, 2.63 nm, gives the thickness of the DS layer, ca. 1.9 nm. Considering the molecular length of DS (ca. 2.1 nm),20,21 the thickness of the DS layer is attributable to the alternating monolayer arrangement, in which each alkyl chain is tilted at an angle of ca. 64° to the Pr hydroxide layer. The average area per DS sulfate group in Fig. 5 can be estimated to be 0.18 nm2 from the density of Pr3+ exposed at the surface of a Pr hydroxide slab. This value is very close to that of anhydrous SDS (0.19 nm2).22 Another possibility for the molecular packing is DS bilayers being tilted to the [hk0] direction, but the estimated tilt angle with respect to the (00l) plane of Pr hydroxide would then be too small (ca. 30°), compared to more than 55° observed for various phases of sodium dodecyl sulfate (SDS). Such a bilayer model may instead be adopted for the Pr-DS-N2H4CO mesophase (S/Pr = ca. 1), because the larger interlayer distance of 3.68 nm is rationalized by the sum of a 1
×
c0 thick Pr hydroxide layer (0.377 nm) and thickness of DS bilayer tilting by ca. 60° with respect to the Pr hydroxide layer (3.30 nm). It should be noted that the monolayer arrangement of DS molecules in the present Pr-DS-NH3 system is in striking contrast to the bilayer arrangement widely observed for anhydrous and hydrous SDS. The bilayer composite should be more stable and more structurally ordered, and thus preferentially formed when the precipitation is carried out slowly, as in the case of the homogeneous precipitation method using urea (Pr-DS-N2H4CO). This is confirmed by very intense X-ray reflections, as shown in Fig. 1b. In contrast, the faster precipitation caused by using ammonia would yield the metastable monolayer phase (Pr-DS-NH3), which exhibited much weaker X-ray reflections (Fig. 1a).
×
OH (Pr–O(1) and Pr–O(2)), whereas the other is coordinated by 6
×
OH and 3
×
O of the sulfate termini, –OSO3 (Pr–O(3)). Therefore, Pr–O bonds with three different lengths should be present in the first shell. In the second shell, the Pr–S and Pr–Pr bonds should be considered. According to the crystallographic data of Pr(OH)3,15 two Pr–Pr bonds with different lengths (3.79 and 4.18 Å) are present. The FT-EXAFS spectrum was fitted by considering the contribution from the first and second shells to determine the structural parameters, including coordination numbers (N), bond distances (r), and Debye–Waller factors (σ) as summarized in Table 1. The present six-shell fitting revealed the best fit (see Fig. 6), with an R factor of 0.78. The peaks at 2.0, 3.5 and 4.0 Å can be attributed to Pr–O, Pr–S and Pr–Pr, respectively. For the first shell, two bonds of 2.52 and 2.57 Å with N = 2.9 and 4.7, respectively, can be assigned to Pr–OH (Pr–O(1) and Pr–O(2)), whereas the shorter bond of 2.38 with N = 1.7 to the Pr–O–SO3 (Pr–O(3)). These atomic distances are in agreement with the crystallographic data of Pr(OH)3 and Pr2(SO4)3·8H2O, respectively. The obtained coordination numbers correspond to average values for two different Pr sites in Pr-DS-NH3 (Fig. 5), because half of the Pr atoms possess 3
×
Pr–O(1) and 6
×
Pr–O(2) bonds and the other half possess 3
×
Pr–O(1), 3
×
Pr–O(2) and 3
×
Pr–O(3) bonds. For the second shell, the Pr–Pr(1) and Pr–Pr(2) coordination numbers were found to be 1.0 and 5.0, respectively. These values may also be explained by considering that half of the Pr atoms, located inside the Pr hydroxide slab, possess 2
×
Pr–Pr(1) and 6
×
Pr–Pr(2) bonds, whereas the other half, located at the surface, possess 1
×
Pr–Pr(1) and 3
×
Pr–Pr(2) bonds. Other attempts to fit the experimental data with the other structural models could not improve the fit. For instance, a model for the alternative stacking of a single Pr hydroxide layer (1
×
c0) and a DS monolayer gave rise to an R factor more than 7.
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| Fig. 6 (a) Pr LIII-edge k3-weighted EXAFS and (b) Fourier transform of Pr-DS-NH3. The solid and dotted lines represent the experimental and fitted oscillations, respectively. | ||
| Shell | Δk/Å−1 a | Δr/Å b | N c (±0.2) | r/Å d (±0.03) | σ 2/10−2 Å2 e (±0.02) | R factor |
|---|---|---|---|---|---|---|
| a Interval of k-space to r-space of FT. b r-Space interval selected to perform reverse FT into k-space. c Coordination number. d Atomic distance. e Debye–Waller factor. | ||||||
| Pr–O(1) | 3.0–10.8 | 1.41–4.73 | 2.9 | 2.52 | 2.13 | 0.78 |
| Pr–O(2) | 4.7 | 2.57 | 2.13 | |||
| Pr–O(3) | 1.7 | 2.38 | 0.72 | |||
| Pr–S | 1.1 | 3.48 | 0.37 | |||
| Pr–Pr | 1.0 | 3.81 | 0.14 | |||
| Pr–Pr(2) | 5.0 | 4.10 | 1.27 | |||
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| Fig. 7 SEM photographs of a) Pr2O2SO4 prepared by heating Pr-SO4 at 900 °C, b) as-prepared Pr-DS-NH3 and c) Pr2O2SO4 prepared by heating Pr-DS-NH3 at 500 °C. | ||
A marked contrast can also be observed for the N2 adsorption isotherm and pore size distribution (Fig. 8 and Fig. 9). The N2 adsorption–desorption isotherm of Pr-SO4 after heating at 900 °C looks like type III (IUPAC), which was flat up to p/p0 = ca. 0.9 and then sharply increased near the saturation of vapor pressure, indicating the presence of macropores. This is contrast to the isotherm for Pr-DS-NH3 after calcination at 500 °C, in which a gradual increase of adsorption with hysteresis in the range p/p0 ≥ 0.5 suggests the contribution of textural mesopores. In both cases, negligible adsorption near p/p0 = 0 suggests the absence of micropores. Pore size distribution calculated from the adsorption isotherms presents peak maxima at pore radii of ca. 18 nm and ≤5 nm for Pr-SO4 and Pr-DS-NH3, respectively. The small surface area as well as macropores in the range ≤20 nm is in accord with the SEM micrograph. The surface area and pore structure of Pr2O2SO4 synthesized from Pr-DS-NH3 were stable up to 900 °C.
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| Fig. 8 N2 adsorption isotherms of Pr2O2SO4 prepared from a) Pr2(SO4)3 and b) Pr-DS-NH3. | ||
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| Fig. 9 Pore size distribution of Pr2O2SO4 prepared by a) Pr2(SO4)3 and b) Pr-DS-NH3. | ||
To evaluate the effect of preparation method on the oxygen-storage/release performance, the dynamic redox behavior of Pr2O2SO4 was evaluated under oscillating feed stream conditions, where reducing (5% H2/He) and oxidizing (20% O2/He) atmospheres were cycled, by the use of a flow microbalance. Fig. 10 exhibits the change of weight during oxygen release/storage cycles at 600 °C for 1 wt% Pd/Pr2O2SO4 prepared from Pr-SO4 (Fig. 10a) and Pr-DS-NH3 (Fig. 10b), obtained after heating at 900 °C and 600 °C, respectively. First, the sample was heated in flowing 20% O2/He up to 600 °C, where on approaching a constant weight, the gas feed was switched to a mixture of 5% H2 in N2. The oxygen release to form Pr2O2S in for Pr-SO4 proceeded very slowly, taking about 10 h to complete, whereas the subsequent oxygen storage was complete within only 10 min. The different rate reflects the slower reduction of Pr2O2SO4, compared to the thermodynamically favorable oxidation of Pr2O2S. In contrast, the weight change due to oxygen release in Pr-DS-NH3 took place very smoothly, and approached the stoichiometric value. Table 2 summarizes the rates of oxygen release/storage, which were estimated from the slope of weight change in Fig. 10. Clearly, both oxygen release and storage for Pr-DS-NH3 was much faster; the calculated rate was more than 7 times faster than that for Pr-SO4. Reversible oxygen release/storage cycles were obvious from stable weight changes. In accord with the surface area and pore structure, which are thermostable up to 900 °C, the oxygen release/storage properties were not affected by further heating at 600–900 °C.
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| Fig. 10 Oxygen release/storage cycles in a microbalance at 600 °C of 1 wt% Pd loaded Pr2O2SO4 prepared from a) Pr2(SO4)3 and b) Pr-DS-NH3. Dotted lines correspond to the ideal weight change due the redox between Pr2O2SO4 and Pr2O2S. | ||
| Precursor | Release/mol-O2 mol−1 min−1 | Storage/mol-O2 mol−1 min−1 |
|---|---|---|
| Pr-SO4 | 0.004 | 0.074 |
| Pr-DS-NH3 | 0.033 | 0.530 |
The observed acceleration of oxygen release/storage can be considered to be a simple particle size effect caused by the microstructural change, but it is considerably larger than expected from the difference of BET surface area (8 m2 g−1 for Pr-SO4, 28 m2 g−1 for Pr-DS-NH3). This would indicate that mass transfer in the solid and/or pores are essential as well as solid/gas interface reactions. As is indicated by SEM images (Fig. 7), Pr2O2SO4 derived from Pr-SO4 is composed of large crystals, with several being 100 µm in size, in which the reaction rate should be determined by the slow diffusion of oxide ions in the solid. In this regard, the nanostructured Pr2O2SO4 particles obtained by the surfactant-assisted syntheses give rise to a much shorter diffusion distance, and thus contribute to the rapid oxygen release and storage.
In summary, we have successfully performd a surfactant-assisted synthesis of a stoichiometric layered Pr2(OH)5(DS)·2.5H2O mesophase, which can yield porous Pr2O2SO4 after heating. Based on the structural and compositional analysis, DS was found to act as a reactive template to yield the Pr oxysulfate. A significant advantage of this novel synthetic route is to achieve the large oxygen-storage capacity of 2 mol-O2 mol−1 at the relatively low temperature of 600 °C, which may have broad significance for various practical applications.
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