Abstract
The electron-paramagnetic-resonance (EPR) spectrum of LaCl3: Eu2+ was observed to obtain the ground-state splitting of Eu2+ in sites of C3h symmetry. A good fit to the observed energy levels in the ground manifold of Eu2+ was provided by the parameters b20=427.20×104 cm1, b40=5.48×104 cm1, b60=0.045×104 cm1, b66=2.97×104 cm1, gII=1.9924, and g=1.9927. The shift in b20 from room temperature to 4.2°K was less than 5%. EPR spectra which could be attributed to europium ions in at least one other inequivalent site were observed but not analyzed in detail. The color centers produced in LaCl3: Eu2+ by ultraviolet radiation appeared to be due to electrons removed by the radiation from Eu2+ ions, which were then trapped at certain crystal defects. The Eu2+ donors were shown to reside in the normal C3h rare-earth sites, and the polarization of the color-center absorption spectrum indicated that the color-center defects had relatively high symmetry. If the color-center defects were due to anion vacancies such as one finds for certain color centers in alkali halide crystals, then the defect was probably a cluster of more than one chlorine vacancy.

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