Ps. Fiske et al., BONDING AND DYNAMICAL PHENOMENA IN MGO - A HIGH-TEMPERATURE O-17 AND MG-25 NMR-STUDY, Physics and chemistry of minerals, 20(8), 1994, pp. 587-593
We have measured the isotropic chemical shifts (delta(iso)) and the sp
in-lattice relaxation times (T1) for O-17 and Mg-25 in MgO from room t
emperature up to 1300-degrees-C. The O-17 chemical shifts increase lin
early from 47 ppm at room temperature to 57 ppm at 1300-degrees-C, and
over the same temperature range the Mg-25 chemical shift increases li
nearly from 25 to 27 ppm. These changes are not the result of changes
in the bulk magnetic susceptibility of the samples, but may be due to
increased orbital overlap which is the result of the increase in therm
al vibration of the ions with temperature. In the case of Mg-25, the s
hift to lower shielding with increasing temperature is opposite to tha
t expected from simple bond length versus chemical shift trends establ
ished for the oxides at room temperature. If this is a general phenome
non, high-temperature NMR data may be biased to lower shielding. Spin-
lattice relaxation times (T1) were measured in order to study the ener
getics of defect motion. T1's for O-17 and Mg-25 exhibit similar behav
ior over the range of temperatures studied. Up to 800-degrees-C, T1's
decrease gradually, but above 800-degrees-C, T1's drop rapidly, with s
lopes corresponding to apparent activation energies of 192 +/- 9 kJ/mo
l (2.0 +/- 0.1 eV) for O-17 and 151 +/- 6 kJ/mol (1.56 +/- 0.06 eV) fo
r Mg-25. While direct comparison of these activation energies to those
derived from diffusion or conductivity measurements is complicated, t
he similar behavior for both nuclei suggests their relaxation phenomen
a are related.