Abstract
A theory is developed for the evolution of bainite as a function of time, temperature, chemical composition and austenite grain size. The model takes into account the details of the mechanism of transformation, including the fact that nucleation begins at the austenite grain surfaces, and that the growth of a sheaf occurs by the repeated nucleation of small platelets. Predictions made using the model are shown to compare well against published isothermal and continuous cooling transformation data.
Royal Society Login
Sign in for Fellows of the Royal Society
Fellows: please access the online journals via the Fellows’ Room
Not a subscriber? Request a free trial
Log in using your username and password
Log in through your institution
Pay Per Article - You may access this article or this issue (from the computer you are currently using) for 30 days.
Regain Access - You can regain access to a recent Pay per Article or Pay per Issue purchase if your access period has not yet expired.
Volume 460, issue 2046
Learn about displayed equations in Proceedings A