A systematic investigation of the dependence of the Verwey phase transition in magnetite on the metal-to-oxygen ratio, by thermomagnetic analysis of the initial permeability, reveals that the transition temperature is a maximum for pure stoichiometric Fe3O4 and is strongly depressed by departures from ideal stoichiometry. Homogeneous single crystalline samples were prepared by subsolidus controlled oxygen fugacity annealing at 1400 °C. Heat capacity measurements by relaxation calorimetry techniques indicate a drastic reduction in the entropy, as well as temperature, of the transition with departures from ideal stoichiometry. For high levels of cation deficiency, a second, instead of a first-order, transition is observed.
We describe a simple analog electronic circuit to measure the voltages of a thermocouple and solid electrolyte sensor and calculate and diplay the temperature and log fO2. This circuit monitors conditions in a simple annealing system where the oxygen atmosphere is controlled by continuous flow of a gas buffer.
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