Abstract
The chemical driving force/unit volume ∆Gv for the γ→α.transformation. in pure iron is computed as a function of undercooling. Similarly, the strain δ accompanying the transformation at different temperatures is also calculated from lattice parameter measurements. Shear moduli μα of ferrite and metastable austenite μγ are derived from various sources. At temperatures down to the Curie temperature (768°C), μα and μγ are very similar, and enable the strain energy/unit volume W to be calculated from the expression W=2 (μα+ μγ)δ2. The data give the metastable equilibrium temperature T;′0 for the massive ferrite transformation as 1156 K. The distinction between equiaxed ferrite, massive ferrite, and Widmanstätten ferrite is discussed.
MST/3138
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