Ab initio calculations of 29Si solid state NMR chemical shifts of silane and silanol groups in silica

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Abstract

We report the results of first principles density functional theory (DFT) calculations on the 1H and 29Si NMR chemical shifts of silane and hydroxyl groups in silica. The structure of the isolated ≡Si–H and ≡Si–OH or of the geminal =Si(H)2 and =Si(OH)2 defects has been fully optimized from mechanically embedded cluster models derived from crystalline α-quartz and the nuclear magnetic shielding properties have been determined according to the GIAO method. The computed 29Si chemical shifts, δ(29Si) in ppm, are (in parenthesis the experimental values): ≡Si–OH −99 (−99), ≡Si–H −86 (−85), =Si(OH)2 −85 (−89), =Si–(H)2 −55 (−50).

Introduction

Solid state NMR is nowadays routinely used for the structural determination of Si-containing inorganic materials 1, 2. Usually, NMR studies of silicon-related compounds are performed using the magic angle spinning (MAS) technique. Where appropriate, MAS NMR has been combined with high-power proton decoupling and 1H–29Si cross-polarization techniques. 29Si MAS NMR has become a standard method to structurally characterize silicates, aluminosilicates (including zeolites), glasses, minerals, cements, etc. 1, 2, 3, 4. Recently, the technique has been applied to the study of special sites and defects in porous or partially oxidized silicon [5], and to the identification of defects and hydroxyl groups in silicon dioxide 6, 7, 8, 9, 10, 11, 12, 13.

Different from other traditional methods for structural characterization, like diffraction techniques which provide information on type and symmetry of the unit cell and even the atomic positions in the cell, a simple correlation between the measured chemical shifts and the structural parameters of a given Si center is not possible. In 1984 Engelhardt and Radeglia [14]derived a simple relation between the 29Si chemical shift in tetrahedral Si(OSi)4 units (Q4) of the framework silicate and the Si–O–Si angles. This relationship has been extended recently by Sauer and coworkers to include Qn atoms with n<4 [15]. Empirical correlations have been proposed also for bond distances [16]and successfully employed in many cases, although the results are not always satisfactory. Nowadays, however, it is possible to compute NMR chemical shifts of solids by means of ab initio quantum-chemical calculations 15, 17, 18. The local structure around a given Si atom is described by a finite cluster of atoms with more or less refined embedding schemes and the shielding properties in a magnetic field can be computed at various levels of sophistication. This approach opens interesting perspectives for a well grounded assignment of the observed chemical shifts to a given structural model. This is particularly important for point defects where information from diffraction methods is not available.

The study of point defects in SiO2 by solid state NMR is limited by the low concentration of these centers in the material. On the other hand, some defects like the hydroxyl groups (also called silanols) or silane groups may be present in sufficient numbers to make their detection possible. Silanols have been studied by combining 29Si MAS NMR, infra-red (IR) spectroscopy and ab initio theory 19, 20and at least three groups of silanols have been identified in porous silica or at the silica surface [21]: (a) the isolated silanol, ≡Si–OH; (b) the geminal silanol, =Si(OH)2; (c) the vicinal pair, where two silanol groups share an O atom, =Si(OH)–O–(OH)Si=. Infra-red (IR) spectroscopy however is unable to discriminate between isolated and geminal silanols [12]while solid state NMR provides an important source of information [12]. Hydroxyls in silica show a proton chemical shift, δ(1H), of 2.0 ppm while for 29Si chemical shifts, δ(29Si), values of ≈−90 to ≈−110 ppm have been measured depending on the type of silanol 7, 8, 12. In the case of silane groups, IR spectroscopy can be efficiently used to distinguish isolated ≡Si–H from geminal =Si(H)2 species: the corresponding vibrational shifts are in fact around 2250 cm−1 and 2190 cm−1, respectively [22]. Recently, 29Si NMR of these two centers have also been reported for oxidized porous silicon and have been assigned as follows [5]: −50 ppm =Si(H)2, −85 ppm ≡Si–H, and −111 ppm SiO2. To the best of our knowledge, there are no theoretical attempts to compute the shielding properties of silane groups from first principle calculations.

In this paper we report a systematic all electron density functional theory (DFT) study of 1H and 29Si chemical shifts of silane, ≡Si–H, and silanol, ≡Si–OH, groups in SiO2. Both isolated and geminal forms are considered. The structure of the defects has been obtained from cluster models derived from crystalline α-quartz. We will show that the combined use of ab initio theory and cluster models provides quantitative information on the NMR chemical shifts of these defects.

Section snippets

Computational details

In the DFT calculations we used the gradient corrected forms of the exchange and correlation functionals proposed by Becke [23]and by Lee et al. [24], respectively. In particular, for the exchange we used the Becke's three-parameters hybrid approach [23](B3LYP). The Kohn–Sham orbitals have been constructed using Gaussian-type atomic orbital (AO) basis sets. The geometry optimization has been done at the B3LYP level using a 6-311G** basis set on Si, O and H atoms [25]; the determination of the

Results and discussion

All the δ(29Si) and the δ(1H) values have been determined at the DFT-B3LYP level with respect to the isotropic shielding constants computed for tetramethylsilane (TMS), Si(CH3)4, a usual standard, σiso(Si) = 338.5 ppm and σiso(H) = 32.3 ppm. The optimization procedure in three steps described above has the value of showing the importance of geometrical relaxation around the defect in determining the chemical shift. In general, however, the results for the various optimization steps are similar

Conclusions

The ab initio calculation of observable quantities, in particular spectral properties, is of fundamental importance for the identification of defect species at the surface or in the bulk of inorganic materials. In this work we have computed from first principle gradient corrected DFT calculations NMR chemical shifts of a group of point defects in SiO2. Work in this direction has already been reported, in particular in the area of zeolites and other microporous materials 15, 17, 18, 20. Here we

Acknowledgements

We acknowledge the following financial supports: Spanish `Ministerio de Educación y Ciencia' (CICyT PB98-1216-C02-01), `Integrated Action Spain-Italy' (HI1998-0042)', `Generalitat de Catalunya' (1999SGR00040), `Italian MURST' (Cofin, Area 03), `Italian INFM' (Project PAIS). Part of the computer time was provided by the CESCA-CEPBA (TMR program ERB FMGE CT95 0062.M).

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