Changes in structure and distribution of carbon in austenite were measured quantitatively of spheroidal graphite cast irons quenched at different stages of heat treating. The austenitizing reaction rate rises significantly with increasing pearlite in the initial structure of the iron. Austenitization of ferritic ductile cast iron is controlled by diffusion of carbon through austenite. Homogenizing results in continued transfer of carbon from nodules until carbon saturates in austenite. Pearlitic ductile iron transforms to austenite in which carbon almost saturates. The bainite transformation of ductile iron proceeds in the mechanism similar to that in high carbon and high silicon steel except that transformation of the former delays and larger volume of austenite (
γ pool) remains in intercellular regions even at the final stage of reaction. Austenite transforms at first to ferrite, and carbon supersaturated in ferrite diffuses to surrounding austenite at high temperatures, while it precipitates in the form of carbide at low temperatures. Carbon distiributes nonuniformly in untransformed austenite with the lowest carbon in
γ pool. Changes in amount of retained austenite and nonuniform microhardness of the matrix reflect heterogeneous distribution of carbon in austenite at isothermal transforming temperatures.
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