Magnetic Hyperfine Interaction and Electronic Relaxation in Rare-Earth Ions in Europium Iron Garnet

Abstract
The attenuation and rotation of the integral angular correlation for the 2(1409 keV)2+(122 keV)0+ γγ cascade in Sm152 following K capture in Eu152 and of the 1(1280 keV)2+(123 keV)0+ γγ cascade in Gd154 following beta decay in Eu154 was measured in polycrystalline samples of europium iron garnet from -25°C to above the Néel point with and without magnetizing field perpendicular to the counter plane. These data and differential angular correlation data, have been analyzed using an extension of the theory of Abragam and Pound to time-dependent magnetic hyperfine interactions in magnetic materials. Explicit formulas for the dependence of the angular correlation on the electronic relaxation time, the average effective field acting at the nucleus in the direction of the magnetizing field Hintz, and the mean square fluctuating field Hint2 are given. The sign, magnitude, and temperature dependence of Hintz in Sm152 were in excellent agreement with the expectation value of Hintz calculated from molecular field theory under the assumption that the electronic configuration following K capture in Eu152 is that of the Sm+3 ion. Crystalline field and quadrupole interaction effects have been neglected. The contribution of the magnetic hyperfine interaction arising from the exchange between the 4f and inner core s electrons was small compared with that from the orbital and spin moments of the 4f shell. The value of the root-mean square hyperfine field was found to be 4.7×106 Oe and that of the average effective field was 4×105 Oe at room temperature. The electronic relaxation time was 4×1012 sec at room temperature and varied inversely with absolute temperature. The electronic state in Gd154 following beta decay in Eu154 has as yet not been determined. Hintz was found to be 8×104 Oe at room temperature.