In the quest for the ideal transformation model describing the austenite de
composition in steel, emphasis shifts from empirical to physical models. Th
is has resulted in the widely used description of the transformation by mea
ns of the interface velocity between the parent phase and the newly formed
phase, a description which yields reliable predictions of the transformatio
n behavior only when combined with a realistic austenite geometry. This art
icle deals with a single-grain austenite geometry model applied to transfor
mations in which the interface velocity is constant throughout the transfor
mation, e.g., certain types of massive transformations. The selected geomet
ry is a regular tetrakaidecahedron, combining topological features of a ran
dom Voronoi distribution with the advantages of single-grain calculations.
The simulations show the influence of the ferrite-nucleus density, the rela
tive positions of the ferrite nuclei inside the austenite grain, and the gr
ain-size distribution. From simulations with a constant interface velocity,
the transformation behavior for a tetrakaidecahedron is in agreement with
transformation kinetics in terms of the Johnson-Mehl-Avrami (JMA) model. Us
ing the tetrakaidecahedron geometry, one can simulate transformation curves
that can be experimentally obtained by calorimetry or dilatometry, in orde
r to study the quantities affecting the transformation behavior.