It is known that the order of the Verwey transition changes from first
to second, and then to a higher order, as the value of delta increase
s in magnetite, Fe-3(1-delta)O-4. The associated heat capacity anomaly
changes its shape and size, and it eventually becomes a broad hump, i
.e. a higher order transition. An attempt was made, with some success,
at recovering the observed changes in heat capacity anomaly in terms
of the two-state approximation, a generalized extension of the Strassl
er-Kittel treatment. By changing the adjustable parameters as a smooth
linear function of delta, a qualitative trend of the observed changes
in heat capacity anomaly was reproduced.