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21-Mat-A5 Phase Transformations and Thermal Treatment · December 2018

Question 8 of 8: Glass and Glass-Ceramic Processing

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

Paper format. National Exams, December 2018 — 12-Mtl-A5, Phase Transformations of Metals, Glasses and Ceramics. Three hours, closed book, approved Casio or Sharp calculator only. Eight questions of 20 marks each; the rubric states that five questions constitute a complete paper and only the first five appearing in the answer book are marked. All eight are answered here, because this set is a study resource rather than an exam script. Several sub-parts explicitly call for an essay-format answer, and the rubric rewards clarity and organisation, so those answers are written as structured prose with supporting sketches rather than as note form.

Note on the exam code

This December 2018 sitting's printed header reads 12-Mtl-A5, Phase Transformations of Metals, Glasses and Ceramics, covering the Fe-C phase diagram and microstructural design, precipitate solubility, precipitation hardening and spinodal decomposition, interfaces and precipitate-free zones, grain growth and Zener pinning, nucleation mechanisms, classical nucleation theory and constitutional supercooling, and glass and glass-ceramic processing.

Reference texts. The answers below are keyed to the works normally recommended for this syllabus code:


Question 8: Glass and Glass-Ceramic Processing (20 marks)

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.

8.1 — (a) Specific volume vs. temperature: crystalline solid vs. glass

Temperature Specific volume T_m crystalline solid T_g (fast) fast-cooled glass T_g (slow) slow-cooled glass liquid
Specific volume vs. temperature for a crystalline solid and for a glass of the same composition, cooled at a fast and a slow rate. All three curves share the same liquid line above $T_m$.

All three cooling paths follow the SAME liquid curve at high temperature (same composition, same liquid thermal-expansion slope), and diverge only as cooling continues:

  1. Crystalline solid. At the equilibrium melting point $T_m$, the liquid crystallizes ABRUPTLY: specific volume drops discontinuously at constant temperature (a first-order transformation, latent heat released), then the crystalline solid continues cooling along its own, much SHALLOWER slope (crystals have a lower thermal expansion coefficient than the liquid, and the slope is a true equilibrium solid-state value).
  2. Glass (either cooling rate). If crystallization does not occur (cooling too fast for nucleation and growth to keep pace, or the composition is a poor glass-former's opposite — i.e. a GOOD glass-former), the liquid simply continues cooling along (approximately) its OWN liquid-like slope below $T_m$ — there is no discontinuous volume drop, because no first-order crystallization transformation occurs. The supercooled liquid becomes progressively more viscous until, over a narrow temperature range (not a single sharp temperature), the structure can no longer relax fast enough to stay in metastable equilibrium on the timescale of the cooling experiment, and the slope KINKS to a shallower, glass-like value at the glass transition temperature $T_g$.
  3. Fast vs. slow cooled glass, and why $T_g$ differs. A FAST-cooled glass has less time to structurally relax at each temperature, so it falls out of metastable equilibrium (kinks) at a HIGHER temperature and freezes in a slightly MORE OPEN (higher specific volume) structure. A SLOW-cooled glass stays in metastable equilibrium longer, kinking at a LOWER $T_g$, and freezes into a slightly denser (lower specific volume) structure. Both glass curves, once past their respective $T_g$, again have a shallow slope similar to (but not identical to) the crystalline solid's slope — but offset to higher specific volume, since a glass never achieves the crystal's fully close-packed, minimum-volume structure.
Check: $T_g$ is drawn schematically as a single kink point for clarity, following the standard textbook convention; physically it is a narrow transition range (a few tens of degrees wide) rather than a sharp thermodynamic transformation temperature, because it is a kinetic (relaxation-time) phenomenon, not an equilibrium phase transformation like $T_m$.

8.2 — (b) Time-temperature processing cycle for a glass-ceramic

time T melt & form nucleation hold, T_n reheat growth/ crystallization hold, T_c cool nucleate at high Ṅ, low growth rate grow nuclei into fine crystals
Typical glass-ceramic processing cycle: melt and form as an ordinary glass, then a controlled two-stage heat treatment (nucleation hold, then a hotter growth/crystallization hold) converts the glass into a fine-grained, largely crystalline glass-ceramic.

A glass-ceramic is produced by first forming the part as an ordinary, fully amorphous glass (by the normal glass-forming route: melt, then form by casting/pressing/blowing while still workable), and only THEN converting it, in the solid state, into a controlled, fine-grained polycrystalline (glass-ceramic) microstructure via a deliberate two-step heat treatment — NOT by simply cooling more slowly, which would give uncontrolled, coarse, often surface-initiated crystallization instead:

  1. Melt and form. The base glass composition (typically containing a nucleating agent, e.g. $\text{TiO}_2$ or $\text{ZrO}_2$, deliberately added for the next step) is melted and formed into shape by conventional glass-forming methods, then cooled to room temperature as an ordinary, transparent, fully amorphous glass.
  2. Reheat to the nucleation temperature $T_n$ and hold. $T_n$ is chosen where the HOMOGENEOUS nucleation rate $\dot N$ of the nucleating-agent-rich phase (or of the primary crystalline phase itself) is at or near its maximum, which for most glass systems is a temperature just above $T_g$ (nucleation rate and growth rate are not maximised at the same temperature — nucleation rate peaks at a LOWER temperature, i.e. larger undercooling, where the barrier $\Delta G^*$ of Question 7(a) is small but atomic mobility is still adequate, whereas the growth rate peaks at a higher temperature). Holding here for an extended time produces an extremely HIGH NUMBER DENSITY of very small, uniformly distributed nuclei throughout the volume — the single most important step for achieving a fine, uniform final grain size, since every nucleus formed here becomes one crystallite in the final microstructure.
  3. Reheat to the growth (crystallization) temperature $T_c$ and hold. $T_c$ is a higher temperature, chosen where the crystal GROWTH rate is high (growth being a diffusional process, favoured by the higher atomic mobility at higher temperature, in contrast to nucleation rate which needs high driving force/low mobility trade-off). Because nucleation has already been completed in Step 2 (very few NEW nuclei form during this hold), the existing fine population of nuclei simply grows outward and impinges on its neighbours, consuming essentially all of the remaining glassy matrix and converting it (typically 90–98% by volume) into fine crystallites, leaving only a thin residual glassy phase at the grain boundaries.
  4. Cool to room temperature. The now largely-crystalline glass-ceramic is cooled under controlled conditions (avoiding thermal shock, since the crystalline and residual glassy phases can have different thermal expansion coefficients) to give the final product — combining the net-shape formability of a glass with the higher strength, toughness and thermal-shock/creep resistance of a fine-grained polycrystalline ceramic.
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