21-Mat-B6 Ceramic Materials · May 2013
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
As-quenched, the 860 °C-austenitized, water-quenched SAE 1045 (∼0.45 wt% C) consists of highly strained, carbon-supersaturated BCT martensite (needle/lath morphology) plus a small fraction of retained austenite trapped between the laths (its $M_f$ is not far below room temperature at this carbon level, so retained austenite is present but modest compared with a higher-carbon steel). This structure is hard, brittle and carries large internal (quenching) stresses. On reheating, three overlapping but temperature-separated stages of change occur:
Fine, coherent transition carbide (ε-carbide, Fe2.4C, hexagonal) precipitates directly from the supersaturated martensite. The martensite's own carbon content drops toward ∼0.2–0.3 wt% C, so its tetragonal distortion ($c/a$) relaxes toward 1 and internal strain is partly relieved. Hardness falls only modestly in this stage, since the fine carbide dispersion itself contributes some precipitation strengthening even as the matrix softens.
Any retained austenite present decomposes to a bainite-like mixture of ferrite and cementite. In a mid-carbon steel like 1045 the retained-austenite fraction is small, so this stage is less pronounced than in a higher-carbon (e.g. eutectoid or tool-steel) quench, but it still contributes a further, small hardness change and removes the (otherwise metastable) retained austenite from the structure.
The transition ε-carbide re-dissolves and is replaced by the stable phase, cementite (Fe3C), which now precipitates directly from the (nearly carbon-free) ferrite matrix. As temperature rises further, the cementite particles coarsen (Ostwald ripening — fewer, larger particles at lower total interfacial energy) and the ferrite laths themselves recover and progressively recrystallize into more equiaxed grains. By the top of this range the structure has become a coarse, globular dispersion of cementite in a soft, recovered ferrite matrix (classically termed tempered martensite grading into spheroidite as the temperature approaches 700 °C). Hardness and strength fall essentially monotonically through this stage while ductility and toughness rise; internal (quenching) stresses are progressively relieved throughout all three stages, most completely by the end of Stage III.