Pierrick Gaudina,
Yohann Vuillemardb,
Florian Jonasa,
Sabine Bouguet-Bonnet‡
*b and
Jean-Luc Blin§
*a
aUniversité de Lorraine, CNRS, L2CM, F-54500 Nancy, France. E-mail: Jean-Luc.Blin@univ-lorraine.fr
bUniversité de Lorraine, CNRS, CRM2, F-54500 Nancy, France. E-mail: Sabine.Bonnet@univ-lorraine.fr
First published on 24th July 2025
In this study, water confinement in hierarchical porous silica and titania is investigated using NMR relaxometry techniques. Results show a greater interaction of water with the TiO2 surface than with the SiO2 one. However, regardless of the matrix, the porosity shows no effect on water relaxation. For silica-based materials, two regimes are observed. The first one at low frequency corresponds to a surface diffusion phenomenon and the second one at high frequency is due to the motion of molecules located in a layer of water further from the surface. Concerning mesostructured titania, water relaxation is governed by very slow surface diffusion.
With the goal of improving catalyst and/or adsorbent efficiency, much effort was devoted to the introduction of hierarchized porosity aiming to favor the diffusion of reactants toward the internal porosity of materials.19,20 The resulting materials exhibit multi-modal porosities ranging from several angstroms to hundreds of micrometers.21 Over the past few years, the development of these hierarchically porous structures at multiple length scales has attracted much attention. Meso–macroporous materials have been synthesized, using multiple templates, such as latex spheres, solid lipid nanoparticles and emulsions based on soft or hard templating methods.22–28 For example, we reported the preparation of macro–mesoporous silica based on fluorinated emulsions.29 In that case, we start from oil-in-water emulsion where the oil droplets are dispersed in the continuous phase that is a direct microemulsion. The oil droplets are stabilized using surfactant molecules. Upon the addition of the inorganic precursor, its polymerization occurs around the oil droplets but also around the swelled micelles by oil, which constitute the microemulsion. After hydrothermal treatment and organic removal, the obtained material exhibits porosity at two levels: the macropores (from 1.0 to 3.0 μm), which are the imprints of the emulsion oil droplets, and the mesopores (7.5 nm) which are formed by the micelles according to the cooperative templating mechanism.29 We have also reported the synthesis of dual mesostructured titania templated by a mixture of hydrogenated (Pluronic P123) and fluorinated [RF8(EO)9] porogens. These materials present two mesopore size distributions, one centered around 7.7 nm and the second around 2.3 nm.30
Some of the applications mentioned above impose critical conditions on the materials; for instance, in catalysis, the regeneration of catalysts is often realized at high temperatures under steam and in the presence of water or even moisture; due to the hydrolysis by water adsorbed on the surface OH groups, a structure collapse is possible. Therefore, it is essential to investigate in detail the behavior of water confined in porous networks. To reach this goal, NMR relaxometry is a powerful technique. Indeed, it can determine the relaxation rate of nuclear spins in fluid molecules within the porous medium to study both the pore characteristics (dimensions and surface properties) and the confined fluid.31 In this study, we have used this technique with the aim of understanding the effect of both surface properties and porosity on the diffusion and interaction of water with the surface in porous materials. To investigate the influence of the inorganic framework nature, both porous SiO2 and TiO2 have been prepared. To study the effect of porosity, mesostructured SBA-15, macro–mesoporous silica, and mesostructured titania having small, large and dual mesopores have been considered.
Proton transverse relaxation times T2 were measured at 25 °C using a Bruker Minispec MQ20 analyzer operating at 20 MHz (1H Larmor frequency). The CPMG (Carr Purcell Meiboom Gill) pulse sequence was used with an echo time of 85 μs and an acquisition of 2000 echoes. 16 scans were performed with a recycle delay of 5 s. The full magnetization decay profile was then Laplace inversed with the UPEN-WIN software.33
1H NMRD profiles (i.e., the longitudinal relaxation rate R1 as a function of the proton Larmor frequency) were acquired between 5 kHz and 10 MHz using a Stelar Smartracer fast-field-cycling relaxometer (Stelar company, Medde, Italy). The temperature was fixed at 25 °C. For all R1 measurements, magnetization recovery curves were found to be monoexponential within the experimental errors. 32 different values of the static magnetic field were sampled, with a fixed acquisition field of 7.2 MHz (1H Larmor frequency). Pre-polarized measurements were done between 5 kHz and 4 MHz with a polarization duration of 0.6 s at a 1H frequency of 8 MHz, and the non-polarized sequence was used between 4 MHz and 10 MHz. The field-switching time was 3 ms. For each B0 value, R1 values were obtained from the magnetization monoexponential evolution as a function of the time, sampled with 16 values between 0.01 and 4 times the longitudinal relaxation time. 32 accumulations were used for all measurements and a recycle delay of 3 s was applied.
Nitrogen physisorption isotherms and BJH pore size distribution (insert) are reported in Fig. 2.
![]() | ||
Fig. 2 Nitrogen adsorption–desorption isotherms and BJH mesopore size distributions (insert) of the prepared materials. |
The porous features of prepared materials are shown by manometry nitrogen adsorption/desorption experiments (Fig. 2). Indeed, SBA-15 shows a type IV isotherm according to the IUPAC classification32 with a well-defined hysteresis loop with two parallel and vertical branches, the characteristic of a narrow pore size distribution. The pore size is narrow (insert of Fig. 2) and centered on 9.5 nm. The L-TiO2-A and L-TiO2-SC materials exhibit similar type IV isotherms, but with a more extended capillary condensation zone (as compared to SBA-15) that reveals a broader pore size distribution (insert of Fig. 2) centered on 7.7 and 6.5 nm, respectively. The isotherms of S-TiO2-A and of S-TiO2-SC suggest supermicroporous materials, i.e., the pore size is located at the limit between the micro and mesoporous domains.34 This is confirmed by the pore size distributions, in which maxima are at around 2 and 2.4 nm for S-TiO2-A and S-TiO2-SC, respectively. The isotherms of S&L-TiO2-A and S&L-TiO2-SC show two inflection points on their adsorption branch (Fig. 2). Since the pore diameter is related to the relative pressure via the Kelvin equation, it indicates the presence of mesopores with two different diameters. The dual mesoporosity of these mesostructured titania is also shown by their mesopore size distributions, for which two maxima at around 2.4–9.0 nm and 2.5–9.1 nm are clearly observed (the inset of Fig. 2). Finally, the adsorption–desorption isotherm of the MM-SiO2 material can be defined as the combination of type II and type IV isotherms featuring the dual macro–mesoporosity of this silica material. The mesoporous pore size distribution ranging from approximately 4 to 16 nm is broader than that for the SBA-material and its maximum is located at 9.0 nm (the inset of Fig. 2). Mercury intrusion results (Fig. 3A) confirm the presence of macropores centered on 120 nm and 4 μm. The macropores are also observed on the SEM micrographs, which show silica particles with a sponge-like structure (Fig. 3B) and having macropores with a size ranging from <1 μm up to ∼3 μm, which does not exhibit any organization.
The values of the specific surface area, the pore volume and the mesopore diameter (∅) of the prepared materials are gathered in Table 1.
Material | SBET (m2 g−1) | Vp (cm3 g−1) | ∅ (nm) |
---|---|---|---|
SBA-15 | 868 | 1.24 | 9.5 |
MM-SiO2 | 931 | 2.71 | 9.0 |
L-TiO2-A | 371 | 0.70 | 7.7 |
L-TiO2-SC | 337 | 0.56 | 6.5 |
S&L-TiO2-A | 387 | 0.48 | 2.4–9.0 |
S&L-TiO2-SC | 308 | 0.48 | 2.5–9.1 |
S-TiO2-A | 490 | 0.27 | 2.0 |
S-TiO2-SC | 180 | 0.19 | 2.4 |
After calcination of the titania materials at 380 °C, the specific surface area decreases due to the condensation of the OH groups. Indeed, the walls of the extracted mesostructured titania are composed of the amorphous phase, which contains Ti–OH groups. Upon calcination, the condensation of these hydroxyl groups occurs.
The T2 values on the order of ms clearly show the effect of confinement in these materials. Indeed, in comparison, bulk water, which is highly mobile, has relaxation times on the order of s at the same temperature and same magnetic field. Because long T2 values come from large pores and short T2 values come from small pores, this T2 distribution is a model of the pore size distribution in the material. Indeed, relaxometry uses the enhanced relaxation of molecules at a pore surface to estimate the pore diameter. A rapid exchange between molecules at the surface and in the pores is assumed,35 and the inverse spin–spin relaxation rate (1/T2) is then proportional to the surface to volume ratio of the porous media.36,37 The proportionality factor is called relaxivity. By fitting a distribution of relaxation times to the raw measured relaxation data, a pore size distribution can be estimated. In the case of SiO2 materials, Fig. 4a shows a clear distinction between the monomodal SBA-5 and the MM-SiO2, which has two T2 distributions, reflecting two pore size distributions, i.e., a bimodal network. This confirms the macro–mesoporous structure detected by nitrogen adsorption–desorption isotherms and mercury porosity. For TiO2, however, it is more difficult to distinguish the meso from the meso–meso structures (Fig. 4), due to the fact that the pore sizes are of the same order of magnitude between the L-TiO2 and S&L-TiO2 samples (see Table 1). On the other hand, both samples show a narrowing of the T2 distribution after calcination (Fig. 4b and c), confirming the organization of the pores and the appearance of a semi-crystalline network. Finally, it appears that the surface relaxivity of TiO2 is greater than the one of SiO2, as the mean T2 is shorter in TiO2 for similar pore sizes in the mesoporous network between silica and titanium samples (comparing particularly silicate and S&L-TiO2). This can be attributed to a greater interaction of water with the TiO2 surface.
Fast field cycling (FFC) NMR relaxometry was then used to further understand the water dynamics in these pores. FFC NMR relaxometry is a low-field NMR technique which measures the longitudinal relaxation rate, R1 = 1/T1, as a function of magnetic field strength over a wide range of frequencies.38,39 No distribution can be measured with T1 here because it is mainly influenced by slow molecular motions and the efficiency of energy exchange with the lattice. The latter is still sensitive to confinement, but often less dramatically than T2, which is typically more sensitive to local magnetic field inhomogeneities and surface interactions, making it very sensitive to pore size distributions. The FFC technique allows the information to be obtained about the molecular dynamics of water embedded in various porous materials studied here, and is particularly useful in the case of slow molecular dynamics, which can only be accessible at very low magnetic field strengths.40
Fig. 5 and 6a show the dispersion curves obtained on the hydrated porous samples in log–log scale. A significant variation of the longitudinal relaxation rate with the measurement frequency is observed, clearly indicating a water confinement effect in these media, and a strong interaction between water and the porous surface.41 A first comparison of the material type shows that the relaxation rates of TiO2 are about ten times greater than those of silica, irrespective of the frequency. The water–surface interactions are therefore greater for TiO2 than for SiO2, as expected from the transverse relaxation values. All dispersion curves can be described by power laws (R1 ∝ ω(−α) = (2πνH)(−α)) characteristic of fluids confined in rigid porous structures.41–44 In these systems, the dispersion originates from the reorientation of the adsorbed molecular phase. The most commonly proposed mechanism is the “reorientation by translational displacements” (RMTD),31,41,45,46 which is governed by intramolecular dipolar interactions. In this case, molecular reorientation occurs via surface diffusion, i.e., water molecules are adsorbed on and desorbed from the surface and move on the surface by translational diffusion resulting in changes in their orientation at the same time.45–51 The power-law exponent of the R1 dispersion could be linked to surface dimensionality for molecules like dimethylsulfoxide and malononitrile confined in porous glass B10.51 Regarding confined water, whose unique properties arise from its high polarity, previous studies have shown that stronger water–surface interactions lead to a steeper R1 dispersion.41,42,52 Consequently, it is assumed that the exponent α of the resulting dispersions power-law dependence can vary depending on the average adsorption time at the surface: the shorter the adsorption time is, the weaker the dispersion will be (i.e., the smaller the value of α).47,52 Two regimes can be clearly identified for the silica-based materials (Fig. 5). The low frequency part (<0.1 MHz) corresponds to a very slow motion resulting from a surface diffusion phenomenon, identical for both samples, SBA-15 and MM-SiO2. The higher frequency part shows less dispersion, which may indicate the superposition of a second, faster, motion, corresponding to a water layer further from the surface and therefore less sensitive to surface interactions. This second population, in exchange with the first one, could also be ascribed to water molecules interacting with different surfaces.50,53
![]() | ||
Fig. 5 1H longitudinal R1 NMRD profiles in silicate porous materials at 25 °C in the frequency range of 0.005–10 MHz. |
For titanium-based materials, the dispersion is very large and a single straight line is visible above 50 kHz in the log–log plot (Fig. 6a), indicating that water relaxation in these materials is largely dominated by surface diffusive motions. A rapid exchange between molecules at the surface and in the pores is assumed.35 The fact that this rate is much higher than the usual value of 0.4 s−1 observed for water alone shows that this fast exchange persists at a frequency of 10 MHz. Moreover, the expected plateau at high frequency54 is not reached here because of the spectrometer limitation. The differences between the curves obtained with the three morphologies are minimal (α = 0.85 ± 0.05 for the three samples). Although the RMTD model foresees the occurrence of a plateau at low frequency,41,50,54,55 it should be noted that the plateau of the R1 data obtained below 50 kHz is not taken into account here, since the T1 values obtained (of the order of 1 ms) are lower than the field switching time used during the measurements (3 ms). Thus, the dynamics of water in TiO2 materials seems to be dominated by very slow surface diffusion, which is only slightly influenced by the morphology of the material. More interestingly, calcination affects the materials S&L-TiO2 and S-TiO2: α increases slightly (from 0.85 to 0.90), but above all, the values of R1 increase on average by 70% (Fig. 6b); however, the material L-TiO2 shows no significant change after calcination. The very small variation in the α coefficient, combined with an increase in relaxation homogeneously along the range of measurement frequencies, could indicate that calcination mainly causes a change in the surface properties of the materials. Indeed, the change in the interaction of water with the surface may be due to condensation of surface OH groups. Please note that the increase in R1 values after calcination could also be explained by a decrease in the pore size of the system, as evidenced by SAXS. However, this shrinkage would mainly affect one of the mesoporous networks in the bimodal system, as there is no visible change in relaxation for the monomodal mesoporous sample.
Silica and titania are commonly used as supports or catalysts in heterogeneous catalysis. For instance, mesoporous SiO2 based catalysts are used for biomass valorization.56 However, they suffer from low hydrothermal stability and leaching of the acid groups, necessary for the catalytic reactions, occurs because of the presence of large amounts of water in biomass feedstock.56 Concerning titania, it is a semiconductor widely used for applications not only in electronics and electrochemical systems but also as catalysts, promoters or carriers for metals and their complexes.57–59 In particular, it is one of the most commonly used photocatalysts.60,61 Water molecules are involved in almost all of these applications, and their interactions with the surface of TiO2 strongly affect the efficiency of the titania materials.62 More generally, since photocatalysis and catalysis are surface processes, the determination of how a molecule interacts with the surface and the quantification of the strength of these interactions are key parameters to develop efficient catalysts. Results obtained here, concerning the interaction of water with the silica and the titania matrix, will contribute to shed some lights on their hydrothermal stability upon the catalytic reaction such as the photodegradation of dyes using mesostructured TiO2. The methodology can also be adapted to gas reactions, such as the oxidation of volatile organic compounds, to characterize the hydrocarbon gas dynamics as reported for methane within various solids such as carbons or zeolites.63,64
Moreover, the transport of the reactant and product to and from the active sites is another parameter that will affect the efficiency of the catalyst, and the characterization of the motion of the fluid molecules in the pores is needed. The latter will be facilitated by introducing a second level of porosity. Indeed, the hierarchal combination of pores can reduce transport limitations and blockage, resulting in higher activities and better control over selectivity.65 Therefore, the information obtained concerning the surface diffusion is important to better study the reactivity of the hierarchical catalysts.
The dispersion curves are described by power laws (straight lines in log–log representation), the characteristic of fluids confined in rigid porous media. The longitudinal relaxation rates R1 determined for titania are greater than those obtained for silica, indicating that water–surface interactions are more important in the case of mesostructured TiO2.
Concerning porous silica, the dispersion curves obtained on the hydrated porous samples show at low frequency a first very slow diffusive surface movement, on which is superimposed a faster movement visible above 0.1 MHz. The latter is attributed to a water layer further from the surface. Regarding titania, water relaxation is dominated by surface effects and no significant difference between materials with monomodal and those with dual mesoporosity could be noted. Results obtained in this article are of potential interest in the field of heterogeneous catalysis, where NMR relaxometry can allow further insights into surface dynamics to be obtained. This technique can provide useful information for elucidating mechanistic influences of solvents on catalyst activity and stability during the reaction.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5nj02729b |
‡ Université de Lorraine, CRM2, UMR7036, Faculté des Sciences et Technologies, BP 702309, F-54506 Vandoeuvre-lès-Nancy cedex, France |
§ Université de Lorraine, L2CM UMR CNRS 7053, Faculté des Sciences et Technologies, BP 70239, F-54506 Vandoeuvre-lès-Nancy cedex, France. |
This journal is © The Royal Society of Chemistry and the Centre National de la Recherche Scientifique 2025 |