Longxiao
Yang‡
a,
Min
Huang‡
b,
Ningdong
Feng
*a,
Meng
Wang
c,
Jun
Xu
a,
Ying
Jiang
d,
Ding
Ma
*c and
Feng
Deng
*a
aState Key Laboratory of Magnetic Resonance and Atomic and Molecular Physics, National Center for Magnetic Resonance in Wuhan, Wuhan Institute of Physics and Mathematics, Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, University of Chinese Academy of Sciences, Wuhan 430071, Beijing 100049, P. R. China. E-mail: ningdong.feng@wipm.ac.cn; dengf@wipm.ac.cn
bSchool of Physics, Hubei University, Wuhan 430062, P. R. China
cBeijing National Laboratory for Molecular Sciences, New Cornerstone Science Laboratory, College of Chemistry and Molecular Engineering, Peking University, Beijing, China. E-mail: dma@pku.edu.cn
dInternational Center for Quantum Materials, School of Physics, Peking University, Beijing, P. R. China
First published on 26th June 2024
Anatase TiO2 is a widely used component in photo- and electro-catalysts for water splitting, and the (101) facet of anatase TiO2 is the most commonly exposed surface. A detailed understanding of the behavior of H2O on this surface could provide fundamental insights into the catalytic mechanism. This, however, is challenging due to the complexity of the interfacial environments, the high mobility of interfacial H2O, and the interference from outer-layer H2O. Herein, we investigate the H2O/TiO2 interface using advanced solid-state NMR techniques. The atomic-level structures of surface O sites, OH groups, and adsorbed H2O have been revealed and the detailed interactions among them are identified on the (101) facet of anatase TiO2. By following the quantitative evolution of surface O and OH sites along with H2O loading, it is found that more than 40% of the adsorbed water spontaneously dissociated under ambient conditions on the TiO2 surface at a loading of 0.3 mmol H2O/g, due to the delicate interplay between water–surface and water–water interactions. Our study highlights the importance of understanding the atomic-level structures of H2O on the surface of TiO2 in catalytic reactions. Such knowledge can promote the design of more efficient catalytic systems for renewable energy production involving activation of water molecules.
One material that has been extensively studied in this regard is titanium dioxide (TiO2). TiO2 is widely used in various fields, including photocatalysis, solar cells, and sensors.1–3,20–22 The surface of TiO2 is highly hydrophilic, and therefore water molecules readily adsorb onto the surface. However, details of the interaction of water with the surface, the reactivity of the TiO2 surface, the rupture of the water O–H bond and consequently the formation of the water–oxide interface structure are essential for the understanding of the interfacial water behavior on the TiO2 surface.
A number of studies have been conducted to investigate the behavior of water on the TiO2 surface. By using scanning tunneling microscopy (STM), it was reported that water molecules form a highly ordered structure on the TiO2 surface, and depending on the conditions, one/two/three-dimensional water structures (monomer, dimer, trimer, tetramer, chains, and networks) could be formed on the surface.23–27 In other reports, it was suggested that a water molecule could react with the oxygen vacancy/defect or rupture over the low coordination surface Ti sites of TiO2, and forms two hydroxyls.11,28–31 Very recently, by an elegant environmental TEM method, Wang et al. reported that the four-coordinated Ti on a (1 × 4) reconstructed TiO2 (001) surface is highly active for water activation.32 However, water adsorption and dissociation on non-defect TiO2 has been disputed for decades.33–36 For the interfacial H2O on the (101) facet of anatase TiO2, a number of theoretical calculations37–40 and some experimental studies, including temperature-programmed desorption (TPD)41 and STM,23 have concluded an intact molecular adsorption of H2O on the TiO2 surface. In contrast, a partial dissociation of H2O has been inferred through the observation of hydroxyls formed on the TiO2 surface by using spectroscopic techniques, such as X-ray diffraction (XRD), X-ray photoelectron spectroscopy (XPS), sum frequency generation (SFG) and so on.42–49 However, it is challenging to distinguish the OH groups formed by H2O dissociation on the non-defect TiO2 surface from either the OH groups generated by H2O reaction with defect sites or the original OH groups present on TiO2. Therefore, while progress has been made, the atomic-level structures of interfacial H2O and especially its detailed interaction with the TiO2 surface are still to be resolved. Significantly, several challenges need to be addressed50 to get the atomic-level structures of the interplay, including how to reveal the interaction of surface oxygen and titanium atoms with interfacial H2O, how the water splitting and hydroxyl formation occur, and the quantitative evolution of these surface oxygen species at the water/TiO2 interface during the hydration process. All these problems are difficult to solve under working reaction conditions due to the interference from outer-layer H2O, the high mobility of interfacial H2O, and the complexity of interfacial environments.15,51,52
17O NMR has long been a powerful and attractive approach for characterizing the atomic-level structure of various oxygen-containing materials due to the wide 17O chemical shift range.53–63 For nano-oxides, the relatively low gyromagnetic ratio, low 17O abundance (0.037%), quadrupolar nature, and especially low proportion of surface oxygen atoms lead to a great challenge to investigate the detailed structure of surface oxygen atoms. The sensitivity and resolution were still limited despite 17O isotopic enrichment. Recently, Peng and Grey et al. selectively enriched surface oxygen atoms on metal oxides (including CeO2, TiO2, and ZnO) with H217O, and distinguished surface O/OH sites from bulk oxygen by using one-dimensional (1D) 17O MAS NMR spectra combined with DFT calculations.64–66 We identified surface OH groups and (sub-)surface O sites on γ-Al2O3 by using the 2D proton-detected 1H–17O heteronuclear correlation technique to improve the sensitivity and resolution of 17O NMR spectra,67 which would make it possible to study interactions between interfacial H2O and oxide surfaces. To date, the detailed structures of the surface O/OH sites and their interactions with interfacial H2O are still ambiguous, let alone quantitative evolution of the structure of these surface O/OH sites in the presence of interfacial H2O, which should be the key to understand the H2O–oxide interaction.
In this study, we choose anatase TiO2 nanoparticles as the oxide model owing to their wide practical application in photo- and photoelectro-catalysis, on which the most frequently exposed surface is the (101) facet with the lowest energy, and investigated the ability of anatase (101) facet-dominated TiO2 nanoparticles to adsorb and activate water on their surface. By using the 2D 17O MQMAS and 1H{17O} J-HMQC NMR methods and other techniques, we examined the atomic-level structures of interfacial water and surface O/OH sites of TiO2 at different water loading levels, as well as the through-bond interactions between them. Our findings show that due to the delicate interplay between water–surface and water–water interactions, the O–H bond of the adsorbed water is broken through the joint effort of coordination-unsaturated Ti5C and the adjacent surface O2C sites, resulting in a terminal OH group (Ti5C–OH) and a proton accommodated on the surface O2C site to form a bridging hydroxyl (O2CH). By following the quantitative evolution of surface O and OH sites along with H2O loading, it is demonstrated that at a loading of 0.3 mmol H2O g−1, over 40% of the adsorbed water was dissociated spontaneously on the TiO2 surface. The understanding over the structure and behavior of interfacial H2O is helpful for developing more efficient and effective catalytic systems for energy storage and conversion.
To investigate the surface sites on the (101) facet of TiO2 that interact with H2O, one-dimensional (1D) and two-dimensional (2D) 17O MAS NMR experiments were performed on 17O-enriched TiO2 (with the surface layer of TiO2 enriched with 17O, see methods for details) with different H217O loadings. As shown in Fig. 1b, the resonances at 600–800 ppm in the 17O MAS NMR spectrum of bare TiO2 were observed, the chemical shift of which is well above the three-coordinated oxygen in the bulk (around 400–600 ppm, Fig. S6†).65 The signal shows a broad second-order quadrupolar interaction lineshape (11.7 T), with its line width sharply decreasing with the increase of magnetic field (18.7 T, Fig. 1c). We assign the resonance to a surface O2C site without interaction with H2O on bare TiO2, marked as OI. Upon loading 0.03 mmol H217O over 100 mg TiO2 (0.3 mmol g−1), the shape of the signal at 600–800 ppm changes significantly, with a tip appearing at 700 ppm (Fig. 1b). At the same time, two new resonances centered at 0 and 150 ppm emerge. To gain insight into the structure of the surface oxygen sites interacting with H2O, we used the 2D 17O 3Q MAS NMR technique to remove the quadrupolar broadening and enhance the spectral resolution. For TiO2 loaded with 0.3 mmol g−1 H217O, clearly, the 2D 3Q MAS spectrum resolved the overlapped resonances in the 17O MAS NMR spectrum (Fig. S7†), revealing two new two-coordinated O2C sites (OII and OIII). However, the large quadrupolar interaction of the OI site made it hardly observable in the 2D 3Q MAS spectrum. When the H217O loading increased to 1.3 mmol g−1 and then to 3.1 mmol g−1, up to five signals were identified, representing five types of O2C sites (OII, OIII, OIV, OV, and OVI) (Fig. 1d and e). The appearance of new O2C sites at the expense of OI sites demonstrates that a fraction of two-coordinated surface oxygen sites can interact with water molecules, leading to changes in their coordination environments.
The NMR parameters of these O2C sites (OI–OVI) obtained from 1D and 2D 17O 3Q MAS NMR spectra (Table S1†) were used to deconvolute the 1D 17O MAS NMR signals acquired at 11.7 T and 18.7 T (Fig. 1b and S8†). The different oxygen species (OII–OVI) obtained upon water loading indicate different interplays between the O2c sites and water. Notably, the 17O MAS NMR spectrum of bare TiO2 does not exhibit any signals of adsorbed H2O or surface OH groups (usually at −200 to 200 ppm) (Fig. 1b). At a water loading of 0.3 mmol g−1, besides the change in O2C sites, the adsorbed H2O at −50–10 ppm and two new overlapped species of surface hydroxyls at around 150 ppm emerge (Fig. 1b), which can be well resolved by the following 2D 1H{17O} J-HMQC NMR experiments. The appearance of hydroxyls suggests that water splitting occurs, which is also confirmed by 2H MAS NMR (see the following). These results demonstrate that: (1) water can interact with the surface O2C site, resulting in a change in its chemical environment, although the type and strength of the interaction cannot be determined at the present time; and (2), 17O MAS NMR experiments confirm the formation of hydroxyls arising from the dissociation of water on the TiO2 surface.
The spatial relationship between the adsorbed water and the two surface hydroxyls was also investigated. Fig. 2a and b display the 1H–17O correlations between adsorbed H2O and surface OH groups on TiO2 with a 0.5 mmol g−1 H217O loading in different 17O chemical shift ranges. As shown in Fig. 2a, two cross peaks were visible at (5.4, −16) ppm and (5.4, 7.0) ppm in the correlation experiment, indicating the presence of two types of adsorbed H2O on the TiO2 surface. These were ascribed to chemisorbed and physisorbed H2O, respectively, which was validated by variable-temperature 2H static NMR experiments (Fig. S10†). In the 1D 17O MAS NMR spectra (Fig. 1b), when the H2O loading increases from 0.3 to 4.7 mmol g−1, the 17O signal of adsorbed H2O gradually narrows and shifts from −16.0 to 7.0 ppm, suggesting that the H2O molecule is preferentially adsorbed on the unsaturated Ti5C site to form chemisorbed H2O (Ti5C–OH2, 17O signal at −16 ppm), while excess H2O molecules adsorb on the outer layer of chemisorbed H2O and hydroxyls through hydrogen bonds to form physisorbed H2O (17O signal at 7.0 ppm).
Interestingly, the 1H signal (7.0 ppm) of bridging hydroxyl (HO2C) only correlates with the 17O signal of chemisorbed H2O (−16.0 ppm; with the most possible structure illustrated in Fig. 2c MI), while the 1H signal (1.7 ppm) of the terminal hydroxyl (Ti5C–OH) correlates with the 17O signals of both chemisorbed (Fig. 2c MII) and physisorbed H2O (7.0 ppm, Fig. 2c MIII). At the same time, as shown in Fig. 2b, there are two types of oxygen of hydroxyls present at 136 and 158 ppm, respectively. The 1H (7.0 ppm) signal of HO2C is only correlated with the 17O signal at 158 ppm. As such, we assigned the cross peak at (7.0, 158) ppm to the 1H–17O correlation from HO2C, and ascribed the cross peak at (1.7, 136) ppm to the Ti5C–OH correlation. The cross peak at (1.7, 158) ppm represents the correlation between them (Fig. 2c MIV). It is worth noting that the 1H signal of adsorbed H2O (5.4 ppm) correlates with the 17O signals of both bridging OH (158 ppm, Fig. 2c MV) and terminal OH groups (136 ppm, Fig. 2c MVI), leading to two cross peaks at (5.4, 158) and (5.4, 136) ppm. As the H2O loading increases to 1.3 mmol g−1, the cross peaks become more prominent, but the interplay remains the same (Fig. S11†).
These results indicate that water splitting is easy to happen under ambient conditions over the practical TiO2 sample under conditions close to the working catalytic conditions, and more importantly, the interplay mode between the physisorbed or chemisorbed H2O and the different types of hydroxyls is very complicated (Fig. 2c MI to MVI), but it could be well resolved by NMR methods. However, questions remain to answer are, how the O–H bond of water ruptured over the TiO2 surface and whether the vacancy gets involved.
![]() | ||
Fig. 3 Spontaneous dissociation of interfacial H2O on the (101) facet of TiO2 (100 mg) at room temperature. (a) Quantitative evolution of various surface two-coordinated oxygen sites (O2C, including OI–OVI) with the increase of H2O loading. (b) The possible configurations of six O2C sites (OI, OII, OIII, OIV, OV, and OVI) on the (101) facet of TiO2 optimized from theoretically calculations. (c) Quantitative evolution of surface O2C sites and hydroxyls with the increase of H2O loading. (d) The proportion of H2O dissociation with the increase of H2O loading. Quantification of the O2C/OH sites is conducted by fitting the main peaks and their spinning sidebands in the 1D 17O MAS NMR spectra (Fig. 1b). Error bars in a, c, and d represent s.d. for each data point (three independent experiments), and points are the average values. |
The sum of O2c (O2COI + OII + OIII + OIV + OV + OVI) sites shows quantitative information about the surface O2C sites (Fig. 3a and c). It is relatively constant except at the water loading of 0.3–0.5 mmol g−1, where the total content of surface O2C sites is decreased by ca. 20% (see the grey region highlighted in Fig. 3c). Very interestingly, this is just the time for the appearance of OH groups whose content is increased by ca. 40% (Fig. 3c). This, together with the above results (Fig. 2), shows that the chemisorbed H2O molecule on the Ti5C site (H2O–Ti5C) is apt to dissociate into a terminal OH group (Ti5C–OH) and a proton (H+), and the latter protonates an adjacent surface O2C site to form a bridging OH group (HO2C), which “consumes” an adjacent O2C site (see below Fig. 4). The proportion of water dissociation relative to total water loaded was also calculated, as depicted in Fig. 3d. Intriguingly, the highest proportion of H2O dissociation, at 41.2%, was found at a water loading of 0.3 mmol g−1. With increasing the H2O loading from 0.5 to 4.7 mmol g−1, the content of surface O2C sites gradually recovered and that of the hydroxyls decreased (Fig. 3c), The results point to the reaction of HO2C groups with nearby Ti5C–OH groups, leading to the regeneration of H2O–Ti5C and the recovery of surface O2C sites. The schematic diagram of H2O dissociation and regeneration on the TiO2 surface is illustrated in Fig. 4.
The dissociation process of interfacial H2O could be also confirmed by 1D 2H MAS NMR experiments on the TiO2 samples (Fig. 5 and S26†). The dehydrated 2H-enriched TiO2 was prepared by exchanging TiO2 with 4.7 mmol g−1 of 2H2O at room temperature for 2 h, and then the 2H-enriched sample was dehydrated at 160 °C and then loaded with different amounts (0.3–4.7 mmol g−1) of 2H2O at room temperature. Since the proton of the bridging OH group is readily exchanged with 2H of D2O, only the 2H signal of the deuterated bridging OH group (DO2C) is observable at 7.4 ppm in the 1D spectrum of dehydrated TiO2 (Fig. 5a). When 0.3 mmol g−1 D2O is adsorbed on the deuterated TiO2, in addition to the increase of the deuterated bridging OH group, a new signal at 1.6 ppm due to the deuterated terminal OH group (Ti5C-OD) appears, which originates from the dissociation of D2O (Fig. 5a). The broad signal at 4.4 ppm corresponds to adsorbed D2O. With the increase of D2O loading, there is a similar evolution trend for the DO2C and Ti5C-OD groups, especially their signal increment is roughly equal (Fig. 5b), consistent with the theoretical content ratio (1:
1) of the two types of deuterated hydroxyls originating from the D2O dissociation. As shown in Fig. 5b, the content of DO2C and Ti5C-OD groups on the TiO2 surface reaches maximum at a 0.5 mmol g−1 H2O loading, in line with the result of 1D 17O MAS NMR analysis (Fig. 3c).
![]() | ||
Fig. 5 Dissociation of interfacial H2O validated by 1D 2H MAS NMR spectra. (a) 2H MAS NMR spectra of dehydrated 2H-enriched TiO2 samples with 2H2O loading from 0 to 4.7 mmol g−1. (b) Quantitative evolution of the deuterated bridging OH (DO2C, at 7.4 ppm) and terminal OH (Ti5C-OD, at 1.6 ppm) groups with the increase of H2O loading, derived from the simulation of the 1D 2H MAS NMR spectra (Fig. S26†). |
![]() | ||
Fig. 6 Dissociation of interfacial H2O on the TiO2 surface revealed by DFT calculations. (a) Calculated structures of the TiO2 (101) (2 × 2) surface slabs with different H2O adsorption configurations. Titanium and oxygen atoms of TiO2 are plotted in blue (Ti) and red (O), oxygen atoms originating from the adsorbed H2O are plotted in yellow (H2O), and hydrogen atoms are plotted in the pink (H). (b) The average bond angle of interfacial H2O on the (2 × 2) surface slabs with different H2O adsorption configurations, calculated from Table S3.† (c) Dissociation energy of interfacial H2O in the optimized structures of different H2O adsorption configurations on (2 × 2) TiO2 (101) surface slabs. |
Our DFT calculations revealed that water dissociation is a coverage-dependent process. Increasing the H2O loading on the Ti5C site of (2 × 2) surface slabs from 1H2O/1Ti5C to 4H2O/4Ti5C, the H–O–H bond angle of chemisorbed H2O is gradually twisted (Fig. 6b), leading to a decline of the dissociation energy of chemisorbed H2O (Fig. 6c). At the optimal water coverage of 4H2O per TiO2 (101) (2 × 2) surface slab (4H2O/4Ti5C), water splitting is enhanced, with the dissociation energy dropping to as low as −0.03 eV. This suggests that H2O dissociation is both exothermic and spontaneous, aligning with our experimental findings. Obviously, the more chemisorbed H2O on the localized (101) facet of TiO2, the more favorable to the dissociation of H2O to form OH. With the further increase of the H2O loading on the Ti5C site of (2 × 2) surface slabs (5H2O/4Ti5C, 6H2O/4Ti5C, and 8H2O/4Ti5C), the presence of physisorbed H2O causes a recovery in the average bond angle of H2O (Fig. 6b) and an increase in dissociation energy (Fig. 6c), implying that physisorbed H2O impedes the dissociation of chemisorbed H2O.
To further address the importance of the interplay between OH and H2O, we also computed the optimized configurations of the H2O dissociation state on the (101) facet of TiO2 at 40% coverage by using a large (5 × 5 × 1) supercell slab with 300 atoms (100 Ti atoms and 200 O atoms), as presented in Fig. 7 and S27.† It's evident that the OH groups originating from water dissociation have strong interactions with the neighboring chemisorbed H2O in the MI–MVI conformations, corroborating with our 2D 1H{17O} J-HMQC NMR findings (Fig. 2). This robust interaction stabilizes H2O dissociation, serving as the driving force for the event. Therefore, at water loadings ranging from 0.3 to 0.5 mmol g−1 (approximately 28–46% coverage), massive H2O dissociation takes place. At elevated water loadings, physisorbed H2O molecules appear, potentially disrupting the interaction between bridging OH groups (Ti–HO2C–Ti) and chemisorbed H2O. This promotes the reaction of bridging OH groups with nearby terminal OH groups, leading to the reformation of molecular H2O (Fig. S28†). All these findings underscore the crucial role of the interplay between OH–H2O and H2O–H2O interactions in determining the behavior of interfacial H2O on the TiO2 surface.
![]() | ||
Fig. 7 The role of the OH–H2O interactions in the dissociation of interfacial H2O revealed by DFT calculations. The interaction modes of the hydroxyls with chemisorbed H2O on the (101) facet of TiO2 at a 40% coverage of water by using a large (5 × 5 × 1) supercell slab with 300 atoms (100 Ti atoms and 200 O atoms), which highlights the optimized atomic structures (MI–MVI) of hydroxyls and adsorbed H2O molecules on the surface of TiO2 shown in Fig. 2c. Regions 1–4 show side views of those structures (MI–MVI) in the 1–4 regions. Titanium and oxygen atoms of TiO2 are plotted in blue (Ti) and red (O), oxygen atoms originating from the adsorbed H2O are plotted in yellow (H2O), and hydrogen atoms are plotted in pink (H). |
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4sc02768j |
‡ These authors contributed equally to this work. |
This journal is © The Royal Society of Chemistry 2024 |