The divacancies involving a tetrahedral iron vacancy (denoted by * in Figure ) exhibit an interesting trend in divacancy core charge for all four classes of divacancies.
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Density Functional Theory Study of Iron-Oxygen Divacancies in Magnetite (Fe<sub>3</sub>O<sub>4</sub>) and Hematite (Fe<sub>2</sub>O<sub>3</sub>).
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