Answers are grounded in this paper and cite their sources.
The crystal-field-split levels of divalent, trivalent, and tetravalent uranium ions have been studied at 20 ^∘{}K in selected crystals having single charge-compensation sites. Complete calculations have been made for the free-ion energy levels of U⁴⁺, with the pertinent constants determined as F₀=13175, F₂=200, F₄=40, F₆=8.05, ζ5f=1660, and α=26. Also calculated crystal-field-split levels of U⁴⁺ in C₃ᵥ symmetry are compared to experimental values, and the various "best fit" values of the crystal-field constants determined. ESR results on trigonal CaF₂: U⁴⁺ are correlated with predicted values derived from optical measurements. Experimental studies of the U²⁺ ion in calcium fluoride are related to the probable U²⁺ configuration, f³s. Crystal-field splittings of the lower levels of CaF₂: U²⁺ are determined from measurements of absorption and fluorescence at 20^∘{}K. The calculated value of ζ5f for U²⁺, based on approximate L-S coupling conditions for the lowest levels, is 1560 cm^-1, and is compared with a similarly calculated value for U³⁺ of 1520 cm^-1. Experimental crystal-field-split levels of tetragonal CaF₂: U³⁺ are shown to fit symmetry requirements, and various laser wavelengths of CaF₂: U³⁺ are related to the level system derived from absorption and fluorescence measurements. Temperature shifts of crystal-field-split levels of uranium ions are also reported.
No takes yet. Share an insight, caveat, or question.
William A. Hargreaves (1970) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: