The effects of Ti substitution for Fe on octahedral sites in magnetite has been investigated through electrical resistivity measurements. In a manner analogous to zinc ferrites, the Verwey transition temperature is depressed with increasing Ti content. The Verwey transition is of first order in Fe_3-y{Ti}yO₄ in the concentration range 0{≤}y{≤}yc=0.012; for yc{≤}y{≤}3yc the transition is of second order, and for y>3yc the phase transformation is completely eliminated. The data are correlated with comparable work on dilute zinc ferrites and nonstoichiometric magnetite, and the implications of the findings are discussed.
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Kąkol et al. (1992) studied this question.
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