Dl. Bryce et al., Characterization of tricoordinate boron chemical shift tensors: Definitivehigh-field solid-state NMR evidence for anisotropic boron shielding, J PHYS CH A, 105(14), 2001, pp. 3633-3640
Despite the large known chemical shift (CS) range for boron and the large n
umber of B-11 NMR studies of glasses, no boron CS tensors have been charact
erized to date. We report the application of solid-state NMR techniques at
moderate (9.4 T) and high (17.63 T) applied magnetic field strengths to the
characterization of the boron CS tensors in trimesitylborane (BMes(3)) and
triphenyl berate (B(OPh)(3)). The boron CS tenser of the former compound e
xhibits a remarkably large span, Omega = 121 +/- 1 ppm, which encompasses t
he known range of isotropic chemical shifts for tricoordinate boron compoun
ds. Conversely, the effect of the boron CS tenser on the B-11 NMR spectra o
f B(OPh)(3) is difficult to observe and quantify even at field strengths as
high as 17.63 T; we find Omega less than or equal to 10 ppm. This marked d
ifference in the boron nuclear magnetic shielding tensors is reproduced acc
urately by a series of ab initio and DFT calculations with a range of basis
sets. The difference is rationalized in the context of Ramsey's theory of
nuclear magnetic shielding by considering contributions to the paramagnetic
shielding in the tricoordinate boron plane. Differences in the in-plane sh
ielding tenser components for the molecules considered are a result of vari
ations in the effectiveness of the mixing of occupied a orbitals with virtu
al pi orbitals under the influence of an applied magnetic field. A similar
explanation has been invoked to rationalize C-13 isotropic chemical shifts
in classical and nonclassical carbocations. We also report experimental and
calculated boron nuclear quadrupolar coupling constants and asymmetry para
meters for BMes(3) and B(OPh)(3). A combination of experimental and theoret
ical results provides the orientation of the CS and electric field gradient
tensors in the molecular framework.