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An electron spin resonance (ESR) spectrum induced in magnesium oxide crystals by pile irradiation has been interpreted as arising from F centers. After an oxide ion is displaced from its normal position by neutrons, an electron donated by ever-present divalent impurities may become trapped at the vacancy. Those centers having only Mg²⁴ and Mg²⁶ neighbors give a single ESR line with $g=2.0023$, while those with one or more Mg²⁵ neighbors give hyperfine patterns corresponding to the nuclear spin value of 5/2. The magnitudes of the isotropic and anisotropic parts of the hyperfine interaction show strong localization of the electron in the vacancy.
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Wertz et al. (1957) studied this question.
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