Abstract
The magnetic permeability of ferrimagnetic normal-spinel-type FeV2O4 and inverse-spinet-type TiFe2O4 at high pressures has been measured in a piston-cylinder apparatus. The Curie temperature and the Hopkinson temperature of FeV2O4 increase with increasing pressure at rates of 4·8 ± 0·4 to 3·4 ± 0·2K GPa−1 and 1·9 ± 0·1 to 1·1 ± 0·1 K GPa−1 respectively, and those of TiFe2O4 increase with pressure at rates of 3·7 ± 0·7 to 4·8 ± 0·1 K GPa−1 and 2·2 ± 0·3 to 3·3 ± 0·3 K GPa −1 respectively. A condition for the occurrence of the NEPCO effect (i.e. a negative pressure derivative of the Curie temperature for magnetic oxides) in the samples studied to date is full Co2+ occupancy of the tetrahedral site.