Recent contributions to the debate on the detailed nature of austenite decomposition processes in steels have focussed on the character of the Widmanstatten ferrite/austenite transformation interface (1,2) and on the nature of the bainite reaction in steels (3,4). The arguments presented concerning Widmanstatten ferrite formation have been exhaustive, and have served to define rather precisely the opposing positions. In this sense, they have been of considerable value. However, the discussors have not made reference to a body of experimental evidence, derived from in-situ high voltage electron microscopic studies, which has bearing on the subject, and which has the virtue of being somewhat more direct than certain of the observations quoted in the debate. Physical and instrumental factors limit the resolution of the method to a level inferior to that of present day high resolution microscopy (5,6); for the present discussion, however, it has the significant advantage of permitting the imaging of structural defects by diffraction contrast, at temperature. Access to thicker regions of the specimen also alleviates sampling problems inherent in wedge foil studies, and increases the probability that the local phenomena observed are closely similar to those which occur in bulk specimens. The purposes of this letter are two: The first is to review existing HVEM studies of ferrite/austenite interface migration, particularly as they relate to the question of Widmanstatten ferrite growth; the second is to add some new observations of high and intermediate temperature interface migration, which were prompted by a study of the published debate. The new observations of interest duplicate and augment some of the previously published findings. (They were obtained using somewhat different materials.) They also relate to possible differences between high and lower temperature interface migration modes for the Widmanstatten ferrite/austenite interface, a topic which has been the subject of recent suggestion (3).
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