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NUCLEAR MAGNETIC RESONANCE SPECTRUM OF B<sup>11</sup> IN KERNITE
16
Citations
4
References
1955
Year
Crystal StructureMagnetic PropertiesEngineeringNuclear PhysicsRadio-frequency SpectrumMagnetic ResonanceMagnetic MaterialsB 4MagnetismNuclear Quadrupole ResonanceEnvironmental MagnetismPhysicsAtomic PhysicsCrystallographyCrystal Structure DesignB 11Magnetic Resonance SpectroscopyNatural SciencesResonanceApplied PhysicsCondensed Matter Physics
The radio-frequency spectrum of B 11 in a single crystal of Na 2 B 4 O 7∙ 4H 2 O (kernite) is examined experimentally as the monoclinic crystal is rotated in an external magnetic field of 7060 gauss in turn about each of three axes (b, c crystallographic axes, and a third perpendicular direction) held normal to the magnetic field. A maximum of 21 lines (some of which show small additional splitting) is observed, which reduces to 11 when the b symmetry axis is perpendicular or parallel to the magnetic field. The results are interpreted in terms of four essentially non-equivalent B 11 sites in kernite characterized respectively by quadrupole coupling constants [Formula: see text], 0.588 ± 0.003, 2.563 ± 0.007, 2.567 ± 0.010 Mc./sec, and asymmetry parameters 77 [Formula: see text], 0.60 ± 0.02, 0.163 ± 0.010, 0.116 ± 0.010. The orientations of the principal axes of the four [Formula: see text] tensors are also determined. These observations on boron are consistent with previous X-ray results, but preliminary observations on Na 23 in kernite contradict previous X-ray position assignments.
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