Abstract
It has been demonstrated that an approximately quantitative relationship exists between oxygen content and the rate of precipitation of alpha from beta in a Ti + 11% Mo alloy. The presence of oxygen was correlated with the occurrence of sub-grain boundary structures and abnormal variations in precipitation rates from grain to grain. An explanation of the transformation rate effects was suggested in terms of polygonization concepts.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
