Nature of the Verwey transition in magnetite (Fe3O4) to pressures of 16 GPa

Abstract
The relative conductivity of Fe3 O4 single crystals very close to ideal stoichiometry has been measured as a function of pressure up to P=16 GPa and in the temperature range of 4.2 to 300 K. The pressure dependence of the Verwey transition TV and the mechanism of conductivity below TV were the main issues addressed. Three pressure regimes were assigned, based on the different behavior of the temperature derivative (DT) of the conductivity curves through TV: (1) In the range 0–6 GPa the DT curves show sharp minima at TV consistent with a first-order phase transition. In this range TV decreases linearly with pressure from 122 to 107.5 K. (2) At P≳6 GPa the DT minima broaden considerably, consistent with a second- or higher-order transition. At P≊6 GPa TV changes discontinuously from 107.5 to 100 K and between 6 and 12.5 GPa decreases linearly to 83 K. (3) At P≳12.5 GPa no DT minima are detected; TV becomes indiscernible. It was shown that the variation of TV with rising P is in close analogy to TV changes with chemical composition (δ, x, y) of Fe3(1δ) O4, Fe3x Znx O4, and Fe3y Tiy O4 as compiled from previous studies. This information is rationalized in terms of phase transitions associated with ‘‘Wigner structures.’’ Changes in the band gap with rising P are discussed. Below 16 GPa and at 30 K<T<TV the conductivity σ is typical of the variable-range hopping (VRH) mechanism [σ=σ0 exp(T0/T)1/4] with T0 decreasing with increasing pressure. Below 30 K σ(T) deviates from the T1/4 law at all pressures. © 1996 The American Physical Society.