Nuclear Magnetic Resonance ofB11at the Three Boron Sites in Rare-Earth Tetraborides

Abstract
An experimental study has been made of the B11 Knight shift at the three different crystallographic boron sites in polycrystalline NdB4. The three central transitions strongly overlap and cannot be analyzed, but it was possible to derive three different Knight shifts [+0.33(3), +0.26(4), and +0.23(3)% at 77 K for the sites 4e, 8j, and 4h, respectively, uncorrected for pseudocontact and demagnetization fields] from the satellites, which are separated from each other by their different quadrupole interactions [νQ=420(6) kHz and η=0 for site 4e, νQ=443(10) kHz and η=0.51(2) for site 8j, and νQ=622(6) kHz and η<0.05 for site 4h, at both 296 and 77 K]. A detailed account is given of the method of extracting the various shift and quadrupole parameters from the powder satellite spectra. We first analyzed LaB4, in which the shifts are zero (±0.02%) with respect to Na2 B2 O4 and in which the quadrupole interactions are νQ=343(4) kHz and η=0 for 4e, νQ=412(4) kHz and η=0.53(1) for 8j, and νQ=544(4) kHz and η=0.045(20) for 4h (4-300 K). In NdB4, relatively large anisotropic contributions to the shifts are found to originate mainly from dipolar fields due to the rare-earth magnetic moments. After correction for pseudocontact shifts, the isotropic hyperfine fields at boron per unit spin S are about -2 kG. Preliminary measurements on GdB4 and HoB4 give the same sign for this field. An attempt is made to fit the observed isotropic shifts in Nd