Manoel Y.
Manuputty
ab,
Jochen A. H.
Dreyer
ab,
Yuan
Sheng
bc,
Eric J.
Bringley
a,
Maria L.
Botero
bd,
Jethro
Akroyd
ab and
Markus
Kraft
*abc
aDepartment of Chemical Engineering and Biotechnology, University of Cambridge, West Site, Philippa Fawcett Drive, Cambridge, CB3 0AS, UK. E-mail: mk306@cam.ac.uk
bCambridge Centre for Advanced Research and Education in Singapore (CARES), CREATE Tower, 1 Create Way, 138602, Singapore
cSchool of Chemical and Biomedical Engineering, Nanyang Technological University, 62 Nanyang Drive, 637459, Singapore
dDepartment of Mechanical Engineering, National University of Singapore, 9 Engineering Drive 1, 117575, Singapore
First published on 14th November 2018
A metastable “high-pressure” phase known as α-PbO2-type TiO2 or TiO2-II is prepared via a single-step synthesis using a laminar premixed stagnation flame. Three other TiO2 polymorphs, namely anatase, rutile and TiO2-B phases, can also be obtained by tuning the oxygen/fuel ratio. TiO2-II is observed as a mixture with rutile under oxygen-lean flame conditions. To the best of our knowledge, this is the first time that this phase has been identified in flame-synthesised TiO2. The formation of TiO2-II in an atmospheric pressure flame cannot be explained thermodynamically and is hypothesised to be kinetically driven through the oxidation and solid-state transformation of a sub-oxide TiO2−x intermediate. In this scenario, rutile is nucleated from the metastable TiO2-II phase instead of directly from a molten/amorphous state. Mixtures containing three-phase heterojunctions of anatase, rutile, and TiO2-II nanoparticles as prepared here in slightly oxygen-lean flames might be important in photocatalysis due to enhanced electron–hole separation.
A key attraction of flame-made TiO2 nanoparticles (TiO2-NPs) is the ability to readily tune properties such as particle size, aggregate morphology, and phase composition by controlling the synthesis conditions. These structural properties in turn control the catalytic activity of the formed TiO2-NPs.6,7 For example, the performance of TiO2 photocatalysts can be greatly enhanced by making use of anatase/rutile heterojunctions when compared to either pristine phase.6 Both anatase and rutile have been shown to form in a flame synthesis.8–10 Under certain conditions brookite has been observed although only in trace amounts.11 Recently, metastable phase TiO2-B12,13 has also been identified to form during flame synthesis.14 Various studies demonstrated that the phase composition of flame-made TiO2-NPs can be controlled by changing the oxygen/fuel equivalence ratio,10,14 TiO2 precursor loading,8,10 presence of an external electric field15 or laser irradiation,16 and dopant concentration.17
Three important factors affecting the stability of various TiO2 polymorphs have been identified, namely particle size, oxidising environment, and temperature. Zhang and Banfield18 demonstrated that for equally sized nanoparticles at 900–1000 K, anatase was the most stable phase for particles smaller than 11 nm, brookite for particles between sizes of 11 and 35 nm, and rutile for particles larger than 35 nm. For particles with similar size, the anatase–rutile composition was shown to be highly sensitive to the oxidant/reductant equivalence ratio, with rutile preferred in oxygen-lean and anatase in oxygen-rich flame environments.8,10 It was suggested that the formation of oxygen vacancies plays an important role in the rutile stabilisation. Recently Liu et al.9 expanded the thermodynamic analysis of Zhang and Banfield18 to include surface oxygen adsorption/desorption, which showed good agreement with their experimental observations. This treatment, however, was only applicable to the anatase and rutile system at thermodynamic equilibrium. Other studies have suggested that kinetically driven processes should be considered in the TiO2 phase transformation. For example, Mao et al.19 demonstrated a sintering-induced anatase-to-brookite transformation in 2–3 nm particles using molecular dynamics simulations.
In addition to the structures mentioned above, crystalline TiO2 can exist in other, less-studied, polymorphic forms such as TiO2-II (columbite) and TiO2-H (hollandite). TiO2-II, an orthorhombic high-pressure phase of TiO2 isostructural with α-PbO2, is of particular interest in this work. Although pure TiO2-II is only thermodynamically stable at high pressure conditions, experiments and first-principles studies have shown that it can be retained at ambient pressure as a metastable phase.20 TiO2-II has been found in nature as a mixture with rutile in ultra-high pressure metamorphic minerals.21,22 Zhao et al.23 suggested that small domains of TiO2-II could be stabilised at a three-phase anatase/TiO2-II/rutile junction. They predicted that such a three-phase junction will lead to a synergistic effect in mixed-phase TiO2 catalysts to enhance the electron–hole separation in photocatalysis. However, the role of TiO2-II as a photocatalyst is still inconclusive as the properties are strongly dependent on the synthesis routes used.24–26
Herein we demonstrate, for the first time, the formation of the TiO2-II phase at atmospheric pressure via stagnation flame synthesis in addition to the commonly observed phases anatase and rutile, as well as the previously reported metastable phase TiO2-B. The relative composition of these phases is strongly dependent on the oxygen/fuel ratio in the synthesis. The formation of metastable phases and their dependence on the oxidising environment give new insights into the phase formation and transformation mechanisms of TiO2-NPs in flames. The role of phase composition in the TiO2 photocatalytic activity is discussed further by Wu et al.27
Two types of stagnation surfaces were located 1 cm under the nozzle to stabilise the flame by flow stretch and to accommodate a substrate for collecting the TiO2 sample. The first one was a rotating (300 rpm), circular stainless steel plate with its rotational axis located 10 cm from the burner centerline (Fig. 1). Slots in the stagnation surface enabled the positioning of glass substrates while the plate rotation convectively cooled the substrate and the deposited particles. In the second configuration, a water-cooled non-rotating plate was used as the stagnation surface. In both cases, a flat flame was stabilised 3–3.5 mm above the stagnation plate depending on the flame equivalence ratio. The equivalence ratio, ϕ, defined as the ratio of O2 required for the complete oxidation of introduced C2H4 divided by the actual amount of available O2, was varied as summarised in Table 1. After 4 min of TiO2 deposition, the sample was carefully scraped off from the glass substrate and used as prepared for further analysis.
Fig. 1 Schematic of the stagnation flame stabilised on a rotating plate (not drawn to scale). A burner nozzle is fixed at H = 1 cm above the rotating plate and at L = 10 cm from the rotational axis. |
ϕ | Mixture mole fractions | T ad (K) | ||
---|---|---|---|---|
C2H2 | O2 | Ar | ||
0.35 | 0.035 | 0.300 | 0.665 | 2073 |
0.50 | 0.035 | 0.210 | 0.755 | 2141 |
0.70 | 0.040 | 0.172 | 0.788 | 2327 |
0.80 | 0.040 | 0.150 | 0.810 | 2336 |
0.90 | 0.045 | 0.150 | 0.805 | 2437 |
1.00 | 0.050 | 0.150 | 0.800 | 2500 |
1.10 | 0.054 | 0.147 | 0.799 | 2518 |
1.30 | 0.061 | 0.141 | 0.798 | 2454 |
1.50 | 0.075 | 0.150 | 0.775 | 2422 |
1.67 | 0.103 | 0.185 | 0.712 | 2542 |
2.00 | 0.130 | 0.195 | 0.675 | 2402 |
2.30 | 0.172 | 0.224 | 0.604 | 2340 |
2.50 | 0.209 | 0.251 | 0.540 | 2309 |
X-ray photoelectron spectra (XPS) were recorded using a Kratos AXIS Ultra photoelectron spectrometer (Kratos Analytical Ltd.) fitted with a monochromatic Al Kα source (1486.71 eV, 5 mA, 15 kV). The photoelectrons were collected at an electron take-off angle of 90°. The binding energy shift was corrected by setting the C–C binding energy to 284.8 eV.
Transmission electron microscopy (TEM) images and selected area electron diffraction (SAED) patterns were acquired with a JEM-2100F FETEM (JEOL Ltd.) with 200 kV accelerating voltage. The TEM samples were prepared by applying a few drops of TiO2 suspension in ethanol on TEM grids followed by air-drying.
The undoped flames were simulated using kinetics®30 as one-dimensional stagnation flows coupled with detailed hydrocarbon chemistry described by the USC-Mech II model.31 The flame standing location was estimated to be 3.5 mm from the stagnation surface. The stagnation surface temperature was taken to be 420 K. A more detailed description of the simulation has been given elsewhere.32 Constant-volume equilibrium simulations at 1 atm and 150 °C were performed using kinetics® to estimate the flame adiabatic temperature (summarised in Table 1). It is noted that the flame adiabatic temperature is usually slightly higher than the actual flame temperature as there is convective heat loss to the colder stagnation plate.
In the lean flame (ϕ = 0.50, Fig. 2(b) and (c)), the major diffraction peaks can be ascribed to anatase (ICSD no. 92363), e.g., A(1 0 1) at 25.3° and A(2 0 0) at 48.1°. The presence of TiO2-B (ICSD no. 41056) can be identified from the smaller peaks at 2θ = 27–34°, i.e. B(0 0 2), B(1 1 1), B(3 1 0). The simulated XRD pattern with a 100:30 intensity ratio of anatase to TiO2-B correctly predicts all the main peaks observed in the experimental pattern. The simulated 2θ-dependent peak broadening due to the crystal size is insufficient to reproduce the broad peaks observed at high angles, e.g., A(2 1 5) and A(2 2 4), suggesting additional peak broadening due to micro-strain.
In the stoichiometric flame (ϕ = 1.00, Fig. 2(e) and (f)), rutile (ICSD no. 16636) was formed in addition to anatase, as is evident from the R(1 1 0), R(1 0 1), R(1 1 1), and R(2 1 1) peaks. The presence of a broad shoulder at 2θ = 31° potentially originates from a third phase, such as a small amount of TiO2-B or TiO2-II. The qualitative agreement observed between the experimental and simulated XRD patterns confirms that rutile and anatase are the main polymorphs formed in the stoichiometric flame (at approximately 2:1 intensity ratio).
In the rich flame (ϕ = 1.67, Fig. 2(h) and (i)), a significant peak at 2θ = 31.5° is observed, which is consistent with II(1 1 1) planes of the TiO2-II polymorph (ICSD no. 158778). It is noted that the peak at 25.5° can either be ascribed to A(1 0 1) or II(1 1 0) but the lack of the A(2 0 0) peak at 48° suggests that the latter is the case. In addition, rutile can be identified from the R(1 1 0) peak at 27.5°. Comparison between the simulated and measured XRD patterns shows slightly broader experimental peaks at low 2θ, indicating that the measured crystals are smaller than the 9 nm assumed for the simulated XRD. The difference in peak broadening increases with 2θ, suggesting the presence of additional micro-strain. Furthermore, it can be observed that some peaks such as II(1 1 2) at 44.5° and II(1 1 3) at 62.5° are significantly smaller and/or broader than expected, most likely due to anisotropy in the crystals. It is interesting to note that similar XRD patterns with strong anisotropy in size and strain-induced broadening were observed in rutile and TiO2-II formed through high-energy milling experiments.24,25
For all three flames, the selected area electron diffraction (SAED) patterns of the agglomerated particles (Fig. 2(c), (f), and (i)) are consistent with the powder XRD patterns. The presence of TiO2 phase mixtures on an aggregate scale suggests intimately mixed crystals at the particle level. For samples prepared in lean flames, the presence of diffraction spots with approximately 0.63 nm lattice spacing corresponding to the B(0 0 1) planes confirms the presence of the TiO2-B phase (Fig. 2(c)).
Fig. 3 presents the HRTEM images and the corresponding structural models which further confirm the presence of the anatase, rutile, TiO2-B and TiO2-II phases as discussed previously. The lattice spacings measured from the HRTEM images agree with those from the ICSD data to within 5% accuracy (a reasonable uncertainty expected from TEM33). In particular, TiO2-B can be readily identified by the large spacing of B(0 0 1) planes as shown in Fig. 3(b) (d = 6.32 Å, ref. dB(001) = 6.24 Å). In Fig. 3(d), lattice planes corresponding to II(1 1 ) (d = 2.86 Å, ref. dII(1 1 ) = 2.85 Å) and II(0 1 0) (d = 5.63 Å, ref. dII(010) = 5.50 Å) are marked. The measured interplanar angle is 60.5° (ref. αII(1 1 )/(0 1 0) = 58.8°).
While Fig. 3 indicates the presence of single crystal primary particles, other TEM images show stacking faults and possibly even multiple crystals within single primary particles (see Fig. S3†). These different crystal domains are especially evident in particles prepared in the fuel-rich flame (ϕ = 1.67), explaining the anisotropy observed in the powder XRD patterns (Fig. 2(h)). Unfortunately, it was not possible to confidently determine the actual crystal phases, orientations and boundaries or their epitaxial relationships, if any, in a single primary particle.
Near the stoichiometric point (ϕ = 0.90–1.00), anatase and rutile are the two main phases observed. The rutile content increases with increasing equivalence ratio as is evident from the R(1 1 0) peak at 27.5°. An anatase/rutile transition near the stoichiometric point was also observed by Liu et al.9 The strong dependence of the anatase/rutile ratio on the equivalence ratio is further in agreement with the study by Kho et al.10
As the equivalence ratio is increased further (ϕ = 1.00–1.30), the XRD results indicate that the anatase content decreases (i.e. A(2 0 0) peak at 48.1°) while TiO2-II is formed. It is noted that the XRD results obtained by Liu et al.9 at ϕ = 1.15 and 1.33 also showed a peak at 2θ = 31.5° but it was attributed to the presence of impurity (Ti3O5). As discussed previously, it is suggested that this peak originates from the II(1 1 1) reflection instead. It should also be noted that Liu et al.9 assigned the reflection at 25.3° to A(1 0 1) but it might also be caused by II(1 1 0), which would explain the absence of the A(2 0 0) reflection in their pattern. The higher intensity of the 2θ = 31.5° peak in the present study is likely caused by differences in the synthesis conditions such as the deposition time, actual gas flow rates, stagnation surface temperature, or burner nozzle diameter.
In the ϕ range of 1.50–1.67, the two main phases identified are rutile and TiO2-II with significant amounts of the latter. The as-synthesised powders appeared slightly blue suggesting the presence of lattice oxygen deficiencies.34 To the best of our knowledge, our work is the first to report a substantial amount of TiO2-II prepared through flame synthesis. A detailed discussion on the possible formation routes is given below.
For the very-fuel-rich flame condition (ϕ = 2.00–2.50), soot is formed together with TiO2 causing the obtained powder to be coloured grey-black. Based on the XRD pattern (Fig. 4(b)), rutile and TiO2-II are still present but with a higher content of rutile. Additionally, anatase is formed as the equivalence ratio increases above 2.0 as evidenced by the A(2 0 0) peak at 48.1°.
The Ti 2p XPS spectra of samples from the lean, stoichiometric, and rich flames (Fig. 5(a)) show very similar binding energies and intensities for Ti4+ 2p3/2 and Ti4+ 2p1/2 peaks with a 2p3/2–2p1/2 splitting value of 5.8 eV, consistent with reported values for TiO2.35 No detectable Ti3+ presence is observed suggesting that the particle surface is completely oxidised regardless of the difference in the oxygen environment (positions of Ti3+ binding energies are marked for reference in Fig. 5(a)).36 The main O 1s peak at around 530.1 eV can be assigned to bulk oxygen in TiO2 (Fig. 5(b)). The smaller peaks at higher binding energies likely belong to surface oxygens, the acidic OH(s) and the basic TiOH, formed from H2O chemisorption on the surface.37
Fig. 5 Ti 2p (a) and O 1s (b) XPS spectra of TiO2 particles synthesised at lean, stoichiometric, and rich flame conditions with normalised intensities. |
Numerous studies have documented solid-state transformations of rutile, anatase, or brookite to TiO2-II but this typically requires high-pressure conditions of up to 5–9 GPa.39,40 Such a high pressure can be achieved through static pressing, shock wave, or high-energy milling experiments. As the TiO2-II in the present study was formed in an atmospheric pressure flame, a solid-state transformation of rutile to TiO2-II is considered unlikely.
In order to elucidate the possibility of direct TiO2-II formation with subsequent phase transformation to rutile, additional XRD patterns (Fig. 6) were recorded for samples collected for different durations on a water-cooled plate (instead of a rotating stagnation plate). Note that the surface temperature of the stationary plate is likely to be higher than that of the rotating plate; thus the results are not directly comparable. Nevertheless, the change of phase composition with prolonged deposition time can give valuable information on the origin of the TiO2 polymorphs. It can be observed in Fig. 6 that the rutile content increases with increasing deposition time and thus prolonged exposure to elevated temperatures. This suggests that TiO2-II is formed first and that rutile originates from a solid-state phase transformation of the already deposited TiO2-II particles. Furthermore, the solid-state transformation is consistent with the observed multiple crystal domains within a single primary particle (Fig. S3†) and the accompanying crystal anisotropy.
A comparison to other ambient pressure TiO2-II synthesis routes might help explain the role of the oxygen/fuel equivalence ratio on the TiO2-II formation and the possible involvement of pre-TiO2-II intermediates. Aarik41 used atomic layer deposition (ALD) to grow TiO2-II solid films from a TiCl4 gas-phase precursor and water as the sole oxygen source. It was observed that TiO2-II grows with some preferred orientation in the pure crystalline phase or in a mixture with rutile at low water doses (i.e. oxygen-lean environment),42 in agreement with our findings for fuel-rich (i.e. oxygen-lean) flames. A preferred growth orientation for TiO2-II was also observed by Grey et al.43 who reacted TiO2 sub-oxide (with composition close to Ti3O5) with boiling sulphuric acid. They proposed that TiO2-II was formed through a solid state transformation of an α-Ti3O5 due to a small long-range misfit between the atomic arrangements of α(1 1 0) and II(1 0 1) layers. Therefore, the results from Aarik et al.42 and Grey et al.43 demonstrate the importance of a non-stoichiometric surface layer42 or solid state transformation from α-Ti3O5 sub-oxide in the formation of TiO2-II crystals. Such sub-oxide species can potentially be formed in the gas phase through clustering of species such as Ti and TiO which have recently been identified as important products in the TTIP decomposition.44 Similarly, sub-oxide structures such as Ti3O5 and Ti5O7 have been reported to form during plasma synthesis of TiO2 from TiC oxidation.45 Therefore, it is possible that during flame synthesis, sub-oxide species form directly from Ti and TiO clustering in the fuel-rich flames. In the high temperature flame environment, these sub-oxide clusters would continue to grow in a liquid-like state and at the same time be oxidised to form stoichiometric TiO2. With high cooling rates, it is possible that the sub-oxide clusters solidify prior to complete oxidation. In this case, diffusion of lattice oxygen can occur to further oxidise the TiO2 bulk, kinetically favouring the formation of TiO2-II over rutile through a mechanism similar to that described by Grey et al.,43i.e. solid-state transformation driven by the close structural match between (1 1 0) α-Ti3O5 and (1 0 1) TiO2-II planes.
If sub-oxide species indeed solidified and later oxidised to TiO2-II through the diffusion of lattice oxygen, some residue of Ti3+ could be expected. Such oxygen deficient titania was reported to be blue in colour,34 similar to the colour of the particles synthesised here with the fuel-rich flames. Notably, the presence of some Ti3+ or oxygen vacancies in the particle core does not contradict the absence of a Ti3+ peak in the surface sensitive XPS spectra (Fig. 5). Rather, it is assumed that the particles have a completely oxidised surface as confirmed by XPS but some oxygen vacancies or Ti3+ exist in the core resulting in the blue coloration of the powder.
Surface modifications could also possibly explain the TiO2-II formation as they can strongly affect the energetics of nanocrystals.9,46 For example, Barnard and Zapol47 show that the anatase-to-rutile phase transition size is significantly affected by surface passivation. The effect of surface hydration has been demonstrated for Y2O3 polymorphic stability where nano-sized particles with a metastable high-pressure polymorph have been prepared at ambient pressure.48,49 The XPS data in Fig. 5(b) suggest that there are some qualitative differences in the shape and intensity of the surface oxygen peaks. However, the interpretation of these peaks is beyond the scope of the present study and will be investigated in future work.
Lastly, the decrease in the relative ratio of TiO2-II to rutile and the onset of anatase formation in very rich flames (ϕ = 2.00–2.50, Fig. 4(b)) is likely connected to the soot formation at these conditions. The formation of soot is evident from the gray-black coloration of the collected powder and is expected to decrease the flame temperature due to radiative heat loss and might further affect the gas-phase chemistry.
Notably, this is the first time that TiO2-II is reported to form in atmospheric pressure flames even though similar XRD patterns were observed in previous flame studies. The mechanism leading to the formation of rutile/TiO2-II mixtures in fuel-rich (i.e. oxygen-lean) flames was elucidated based on the phase composition as a function of collection time and previous reports of TiO2-II formation. It is proposed that rutile is formed through a solid-state transformation of TiO2-II. The TiO2-II formation hereby likely involves some titania sub-oxide intermediate that is subsequently oxidised to stoichiometric TiO2-II. The formation of and transformation between the four different TiO2 polymorphs cannot be explained by the current understanding of TiO2 phase formation and transformation mechanism, and thus requires re-evaluation of the current working hypotheses.
Footnote |
† Electronic supplementary information (ESI) available: (1) Particle size and morphology, (2) FFT analysis of HRTEM images, and (3) XPS C 1s fitting. See DOI: 10.1039/c8sc02969e |
This journal is © The Royal Society of Chemistry 2019 |