Answers are grounded in this paper and cite their sources.
The impurity ion O− has been introduced into KCl, RbCl, and KBr and detected at 4°K by EPR spectroscopy. The center has orthorhombic symmetry. A quantitative understanding of the g factor and of the O17 hyperfine structure was obtained with the aid of equations derived in a recent analysis of the an-alogous S− impurity. The hyperfine splitting was described by the atomic parameters ψ2(0), 〈r−3〉l, and 〈r−3〉s. The present results indicate that in an earlier investigation of O− trapped in alkali iodide crystals erroneous values were obtained for these parameters.
No takes yet. Share an insight, caveat, or question.
Brailsford et al. (1969) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: