Abstract
The spin-lattice relaxation time T1 in the ground-state Kramers doublet of Fe1+ in MgO has been measured in a fast travelling-wave-tube X-band spectrometer by pulsed saturation from 10 to 23 K and by line broadening from 23 to 37 K. By simultaneously measuring recovery from pulsed saturation and the relaxation-induced component [ΔH(T)ΔH(0)] of the Lorentzian EPR linewidth at 23 K, the absolute scale for 1T1 from linewidth was determined to be (4.7±0.6)×107 sec1/Oe. The data from 10 to 37 K are accurately described over seven decades of time by 1T1=BT9+C(eΔT1)+C(eΔT1), where B=(1.2±0.1)×107/secK9, C=(2.2±0.4)×1010/sec, C=(2.7±2.3)×1013/sec, Δ=213±4 K, and Δ=450±30 K. The temperature dependence is consistent with the interpretation that spin-lattice relaxation in the ground-state Kramers doublet of MgO: Fe1+ occurs predominantly by resonant phonon scattering involving excited electronic states at ∼150 and ∼310 cm1. Comparison of the excited-state energies with predictions from the crystal-field model for 3d7 ions in cubic MgO indicates a large crystal-field strength parameter or covalent bonding with λλ0=0.57, the orbital reduction factor as low as 0.65, and some evidence for inadequacies in the model.

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