21-Mat-B6 Ceramic Materials · December 2015
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.
Given. An etched micrograph (5 μm scale bar) from a hypoeutectoid plain-carbon steel, with two arrows marking regions for phase identification. Fe–Fe3C reference data: eutectoid composition $C_{eu}=0.77$ wt% C at 727 °C; ferrite solvus $C_\alpha=0.022$ wt% C; cementite $C_{\text{Fe}_3\text{C}}=6.70$ wt% C. For part (iv), a second, separate sample at $C_0=0.85$ wt% C is held a long time at a temperature just above the eutectoid temperature.
Find. The constituent at each arrow; an estimate of the micrograph sample's own carbon content; the heat-treatment route that produced this microstructure; and the equilibrium weight fraction of austenite in the second (0.85 wt% C) sample.
[Figure not reproduced: Micrograph of a hypoeutectoid steel showing proeutectoid ferrite and pearlite, with two arrows. See the official exam paper or the cited reference text.]
The steel is hypoeutectoid (below 0.77 wt% C), so on slow cooling from full austenite it must pass through a two-phase $\alpha+\gamma$ field before reaching the eutectoid, and the two constituents visible in the micrograph are exactly the two products of that route. The left arrow points into the fine, dark, mottled texture that occupies most of the field — at this magnification (5 μm scale bar) individual cementite lamellae are too closely spaced to resolve cleanly, so pearlite (alternating ferrite/cementite lamellae) reads as a uniformly dark, finely textured constituent rather than as distinct stripes. The right arrow points to the edge of a large, light, irregularly-shaped region with smooth internal contrast and no lamellar texture — this is proeutectoid ferrite, the soft, nearly carbon-free phase that forms first as the steel cools below $A_3$ and appears bright/featureless under this etch because, unlike pearlite, it contains no cementite to darken it. Proeutectoid ferrite of this kind nucleates preferentially at prior-austenite grain boundaries, which is consistent with the large constituent's blocky, boundary-following outline in the micrograph.
Approach. For a hypoeutectoid steel slow-cooled to room temperature, the room-temperature proeutectoid-ferrite weight fraction is fixed by the lever rule on the $\alpha/\gamma$ tie line at 727 °C (just above the eutectoid reaction), because that is the last temperature at which the ferrite fraction is set before the remaining eutectoid austenite converts to pearlite; reading the ferrite AREA fraction off the micrograph and treating it as the ferrite WEIGHT fraction (reasonable since ferrite and pearlite have very similar density) inverts the lever rule to back out $C_0$.
The ferrite–pearlite structure in Fig. 1.1 is the standard product of slow, near-equilibrium cooling of a hypoeutectoid steel from the austenite field — i.e. a full anneal or normalize, not a quench. The steel is first heated into the single-phase austenite field, above $A_3$, and held long enough to homogenize. On slow cooling (furnace cooling for a full anneal, or still-air cooling for a normalize) below $A_3$, the equilibrium phase diagram requires proeutectoid ferrite to begin nucleating and growing, preferentially at prior-austenite grain boundaries, because ferrite is the phase favoured on the low-carbon side of the $\alpha+\gamma$ two-phase field. As ferrite grows, it rejects carbon into the shrinking austenite, driving the remaining austenite's composition to increase along the $A_3$–$A_1$ boundary. This continues until the temperature reaches $727$ °C ($A_1$), by which point the remaining austenite has been enriched to exactly the eutectoid composition ($0.77$ wt% C); that remaining austenite then transforms by the eutectoid reaction $\gamma\rightarrow\alpha+\text{Fe}_3\text{C}$ into pearlite. The slow cooling rate leaves time for the pearlite lamellae to nucleate and grow at only modest undercooling below $A_1$, giving the finely but not exceptionally coarsely spaced lamellae read as a uniform dark texture at this magnification, alongside the blocky, grain-boundary-decorating proeutectoid ferrite formed in the earlier stage.
Approach. At $0.85$ wt% C the second sample is hypereutectoid, so a temperature just above $727$ °C places it in the $\gamma+\text{Fe}_3\text{C}$ two-phase field immediately above the eutectoid horizontal. Because the hold is "slightly higher" than $727$ °C, the austenite boundary ($A_{cm}$) has moved only infinitesimally away from the eutectoid point, so to an excellent approximation the austenite on the tie line still sits at the eutectoid composition, $C_\gamma\approx C_{eu}=0.77$ wt% C, while cementite remains at its fixed stoichiometric composition. Apply the lever rule on that tie line.
| Item | Result |
|---|---|
| Left-arrow constituent | Pearlite (unresolved fine lamellae) |
| Right-arrow constituent | Proeutectoid ferrite |
| Estimated carbon content of the micrograph sample | ≈0.6 wt% C |
| Heat treatment producing the microstructure | Full anneal / normalize (slow cool from austenite) |
| $W_\gamma$ at 0.85 wt% C, just above 727 °C | 0.9865 (98.65%) |
| $W_{\text{Fe}_3\text{C}}$ at 0.85 wt% C, just above 727 °C | 0.0135 (1.35%) |