Abstract
To test our previous conclusions about the appearance of two separate peaks in the neighbourhood of the Verwey transition in single-crystal magnetite, we have measured the specific heat and magnetization around the Verwey transition of Fe3-x CoxO4, and Fe3-yO4 single crystals. Our present results confirm our previous conclusions: for Fe3-xCo4O4 with 0 ≤ X ≤ 0·04, two transitions appear in the vicinity of the Verwey transition, and, for Fe3-yO4 with y ≥ 0·037 no transition is observed. The driving forces for the two anomalies are not connected.