21-Mat-B6 Ceramic Materials · May 2016
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.
In conventional gray cast iron, essentially all of the carbon above the matrix's own solubility limit is present as FREE, elemental graphite — not combined as a carbide. Morphologically it forms as coarse, interconnected flakes: during eutectic solidification, graphite (which is thermodynamically favoured over cementite at the slow cooling rates and moderate-to-high silicon levels typical of gray iron) nucleates and grows preferentially along its own basal (0001) plane, so each graphite particle grows fast in two directions and only slowly in the third, producing thin, curved, interconnected flakes radiating out from a common nucleus rather than a compact (spheroidal) particle. It is this flake morphology — sharp-tipped, plate-like graphite acting as an internal stress-raiser/crack-initiator network running through an otherwise ductile ferrite or pearlite matrix — that gives gray iron its characteristic brittleness (essentially zero tensile ductility) despite the matrix itself being reasonably ductile; the flakes are also what gives gray iron its name (a fracture surface exposes the graphite and looks visually gray).
In white cast iron essentially NONE of the carbon exists as free graphite: it is instead entirely COMBINED, chemically bonded as iron carbide, cementite (Fe3C), following the metastable Fe–Fe3C system rather than the stable Fe–graphite system. Morphologically, the eutectic cementite solidifies as a continuous, interconnected network (ledeburite: cementite plus a pearlite/austenite-derived matrix) rather than as isolated particles, so the microstructure is a hard, brittle, continuous carbide skeleton enclosing islands of the transformed matrix. Because cementite is colourless/white and reflects light strongly, a fracture surface through this carbide network looks bright white — the origin of the name "white" cast iron — and the same continuous hard-carbide network that gives the name is also what makes white iron extremely hard and wear-resistant but essentially non-machinable and very brittle.
White iron formation means SUPPRESSING graphitization, i.e. keeping carbon combined as cementite rather than letting it precipitate as free graphite during solidification and cooling. The competition between the stable (graphite) and metastable (cementite) eutectics is governed by cooling rate and composition, so white iron is produced by pushing BOTH levers toward cementite:
In practice the two levers are combined: a low-silicon iron poured into a chilled mould reliably solidifies white, while the same composition poured into a thick sand mould (slow cooling) may solidify gray — which is also why the SAME casting can be deliberately chilled locally (e.g. mill rolls, jaw-crusher liners) to be white and wear-resistant at a working surface while staying gray (tougher, machinable) through the bulk.