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Chapter 7 • Theory & Derivations

Glasses, glass-ceramics and optical properties

**Guiding question:** What changes when a disordered glass is formed, tempered or crystallized?

§7.1 Why this unit matters to ceramic engineering

Guiding question: What changes when a disordered glass is formed, tempered or crystallized?

A heat-treated panel becomes mechanically harder but loses clarity and displays small edge cracks. This is a question about glass structure and crystallization and the distinction between optical absorption versus scattering and residual stress. A defensible answer identifies feedstock composition, chemistry, processing path and microstructure before comparing measured properties. It also names the potentially controlling failure mode: a recipe that optimizes density, dielectric response or simple bend strength can still worsen thermal cycling, porosity topology, lifetime or chemical compatibility. The technical sections below connect simplified mathematics to the kinds of measurements that would justify a practical claim.

Glasses differ from crystals in long-range order and their properties depend strongly on cooling history. Controlled crystal precipitation can create useful glass-ceramics but may reduce transparency through scattering.

Track viscosity, annealing condition, diffraction phase fraction and optical spectrum separately. Surface compression may protect shallow flaws while deep scratches bypass the strengthening profile.

§7.2 Measurement and conservation checkpoints

Write down the starting composition, defect-sensitive atmosphere and powder or glass history; define whether reported fractions are by area, mass, moles or volume; and record the process history that could alter cooling history, composition and finish. For any local observation, describe why its sampling plan represents the part. Treat microcrystallites or edge damage as an explicit rival explanation and plan spectral transmission and diffraction as an independent check.

§7.3 Glass networks, modifiers and intermediate oxides

Scientific foundation

Silicate glasses are disordered network structures characterized by local bonding and a distribution of ring and modifier configurations, not one repeating long-range crystal lattice. Network modifiers alter nonbridging oxygen populations and often change viscosity, chemical durability and expansion together. Alkali-rich recipes may melt conveniently yet be vulnerable to aqueous corrosion; borosilicate mixtures offer other thermal and chemical tradeoffs. Composition cannot be optimized by assuming every oxide addition improves all properties.

Governing relationship or decision rule: Oxide-basis compositions must sum to unity in a declared molar or mass basis; a glass-forming tendency is not determined solely by any one component. Read every term in the equation as part of a declared specimen condition. In glass networks, modifiers and intermediate oxides, a valid calculation requires the state of the ceramic, unit system and physical or geometrical meaning of each quantity. A nominally identical oxide composition can conceal different dopant distributions, porosity, grain-boundary glass and processing damage. Equal bulk density does not guarantee equivalent fracture, transport or thermal stability. Interpret measurements only after identifying which feature of the state they can support.

Worked ceramic investigation

Create a molar batch recipe from silica, boron-containing and alkali raw materials, converting between mass and mole fraction correctly and accounting for gas released during decomposition. Compare an alkali-rich and a low-alkali glass in a proposed water-leaching experiment. Predict trends qualitatively but require measured dissolution profiles before specifying container suitability.

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 771.4286 K, the declared formula returns 7.7692308 log10(Pa·s); at Absolute forming temperature = 842.8571 K, it returns 6.0322581 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.024317618 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

The browser expression is -3+4000/(T-400). Model validity is limited to: Synthetic VFT-like equation A=-3, B=4000 K, T0=400 K, 700<=T<=1200 K; not calibrated to any glass. Reproduce the first result with a calculator using the expression and units stated here. Before accepting the number, check the units analytically and identify what is being held constant. If a result looks realistic, that coincidence does not establish physical validation. Try an extreme permitted slider input and ask whether the computed change is physically interpretable or an artifact of the simplifying assumptions.

Evidence, uncertainty, and a competing mechanism

Batch chemistry may differ from final glass chemistry because of volatilization and refractory contamination. Small glass samples can appear homogeneous while large melts contain cords, stones or bubbles.

Exercises and self-assessment

Exercise 7.1A — Physical mechanism. Why can lowering melt viscosity worsen environmental durability? State one plausible explanation, one competing explanation and the material-state observation that separates them. Relate the claim to the governing relationship written above rather than merely repeating definitions.

Exercise 7.1B — Numerical cross-check. Recalculate 7.7692308 log10(Pa·s) from the companion formula at 771.4286 K and compare with 6.0322581 log10(Pa·s) at 842.8571 K. State the sign of the sensitivity and explain whether the changed input would reasonably be controlled independently in a real ceramic specimen.

Exercise 7.1C — Test design. Propose a preparation or test matrix that addresses microcrystallites or edge damage. Give the specimen orientation, spatial sampling scheme, temperature-time record and principal instrument calibration. Explain which observation would falsify your first hypothesis and name a condition under which your model should not be used.

§7.4 Glass transition, relaxation and viscosity

Scientific foundation

Glass transition is a kinetic range dependent on observation time and thermal history, not a single first-order equilibrium melting point. During heating, viscosity and structural relaxation change continuously, while fictive temperature records aspects of the cooling history. Viscosity generally falls strongly with increasing temperature; common empirical fits describe a limited temperature interval and must not be extrapolated across crystallization or decomposition.

Governing relationship or decision rule: Illustrative VFT form log10 eta=A+B/(T-T0) is empirical and valid only within the fitted range above T0. Read every term in the equation as part of a declared specimen condition. In glass transition, relaxation and viscosity, a valid calculation requires the state of the ceramic, unit system and physical or geometrical meaning of each quantity. A nominally identical oxide composition can conceal different dopant distributions, porosity, grain-boundary glass and processing damage. Equal bulk density does not guarantee equivalent fracture, transport or thermal stability. Interpret measurements only after identifying which feature of the state they can support.

Worked ceramic investigation

Use a teaching Vogel–Fulcher–Tammann-type log-viscosity relation over an explicitly restricted 700–1200 K range. Interpret output as log10(Pa s), convert two points to viscosity units and explain how a forming window would depend on process strain rate and part thickness. Plan a beam-bending or rotational-viscosity measurement suited to the relevant viscosity regime.

A companion calculator called Glass absorption-only transmission supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Optical path length = 6.428571 mm, the declared formula returns 96.836823 % transmitted; at Optical path length = 9.142857 mm, it returns 95.531487 % transmitted. On this interval the modeled value decreases, and the two-point slope is -0.48091339 % transmitted per mm. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

The browser expression is 100Math.exp(-5L/1000). Model validity is limited to: Monochromatic uniform absorption coefficient=5 m^-1; no scattering, interfacial reflection, interference or wavelength dependence. Reproduce the first result with a calculator using the expression and units stated here. Before accepting the number, check the units analytically and identify what is being held constant. If a result looks realistic, that coincidence does not establish physical validation. Try an extreme permitted slider input and ask whether the computed change is physically interpretable or an artifact of the simplifying assumptions.

Evidence, uncertainty, and a competing mechanism

The fit constants are synthetic. At lower temperature a glass may age or relax, and at higher temperature it may crystallize or chemically decompose; the simple equation does not encode these transitions.

Exercises and self-assessment

Exercise 7.2A — Physical mechanism. Why does an annealing temperature that reduces stress in a thin sheet fail to relax a thick block in the same time? State one plausible explanation, one competing explanation and the material-state observation that separates them. Relate the claim to the governing relationship written above rather than merely repeating definitions.

Exercise 7.2B — Numerical cross-check. Recalculate 96.836823 % transmitted from the companion formula at 6.428571 mm and compare with 95.531487 % transmitted at 9.142857 mm. State the sign of the sensitivity and explain whether the changed input would reasonably be controlled independently in a real ceramic specimen.

Exercise 7.2C — Test design. Propose a preparation or test matrix that addresses microcrystallites or edge damage. Give the specimen orientation, spatial sampling scheme, temperature-time record and principal instrument calibration. Explain which observation would falsify your first hypothesis and name a condition under which your model should not be used.

§7.5 Nucleation and controlled crystallization

Scientific foundation

Glass-ceramics form by promoting nuclei and subsequent crystal growth inside a parent glass. The final property depends on crystalline fraction, phase type, precipitate dimensions, residual glass chemistry and thermal expansion mismatch. Classical nucleation arguments highlight the competition between interfacial energy and bulk free-energy driving force, but real nucleants and heterogeneous surfaces change barriers. Excess crystallization or unwanted phases can destroy transparency and strength.

Governing relationship or decision rule: A classical spherical homogeneous barrier scales as DeltaG*=16 pi gamma^3/[3 (DeltaG_v)^2], within strong simplifying assumptions. Read every term in the equation as part of a declared specimen condition. In nucleation and controlled crystallization, a valid calculation requires the state of the ceramic, unit system and physical or geometrical meaning of each quantity. A nominally identical oxide composition can conceal different dopant distributions, porosity, grain-boundary glass and processing damage. Equal bulk density does not guarantee equivalent fracture, transport or thermal stability. Interpret measurements only after identifying which feature of the state they can support.

Worked ceramic investigation

Propose a two-step heat treatment for a model glass-ceramic with one nucleation and one growth stage. Measure crystalline phase fraction by diffraction with a stated calibration, then compare surface and core microstructures to test thermal homogeneity. Use viscosity-versus-temperature only to estimate mobility trends, not to infer a nucleation rate from a single scalar equation.

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 914.2857 K, the declared formula returns 4.7777778 log10(Pa·s); at Absolute forming temperature = 985.7143 K, it returns 3.8292683 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.013279133 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Evidence, uncertainty, and a competing mechanism

A time–temperature–transformation diagram determined for one parent-glass batch may not be transferable after minor composition or thermal-history changes.

Exercises and self-assessment

Exercise 7.3A — Physical mechanism. How might a small nucleant addition improve crystallization uniformity while also raising the number of scattering centers? State one plausible explanation, one competing explanation and the material-state observation that separates them. Relate the claim to the governing relationship written above rather than merely repeating definitions.

Exercise 7.3B — Numerical cross-check. Recalculate 4.7777778 log10(Pa·s) from the companion formula at 914.2857 K and compare with 3.8292683 log10(Pa·s) at 985.7143 K. State the sign of the sensitivity and explain whether the changed input would reasonably be controlled independently in a real ceramic specimen.

Exercise 7.3C — Test design. Propose a preparation or test matrix that addresses microcrystallites or edge damage. Give the specimen orientation, spatial sampling scheme, temperature-time record and principal instrument calibration. Explain which observation would falsify your first hypothesis and name a condition under which your model should not be used.

§7.6 Chemical tempering, residual stress and flaw control

Scientific foundation

Thermally tempered glass obtains surface compression from differential cooling through a viscous-transition range. Chemically strengthened glasses can develop compression from exchanging smaller alkali ions with larger ones under controlled conditions. Surface compression delays opening of surface flaws, but the depth of compression and central tension must be considered because deep damage or edge defects can defeat the benefit. Strengthening does not remove all cracks or make fracture impossible.

Governing relationship or decision rule: Superposition of applied and residual stress controls the opening force on a crack, with depth-dependent residual stress requiring integration in fracture analysis. Read every term in the equation as part of a declared specimen condition. In chemical tempering, residual stress and flaw control, a valid calculation requires the state of the ceramic, unit system and physical or geometrical meaning of each quantity. A nominally identical oxide composition can conceal different dopant distributions, porosity, grain-boundary glass and processing damage. Equal bulk density does not guarantee equivalent fracture, transport or thermal stability. Interpret measurements only after identifying which feature of the state they can support.

Worked ceramic investigation

Prepare a comparison of untreated and ion-exchanged sheets with measured surface stress profiles and flaw-size distributions. Examine failure after both shallow abrasion and deep scratching, while noting that the same nominal stress may be irrelevant when the flaw extends beyond the compressive layer. Measure optical distortion and durability after aging.

A companion calculator called Glass absorption-only transmission supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Optical path length = 11.85714 mm, the declared formula returns 94.243746 % transmitted; at Optical path length = 14.57143 mm, it returns 92.973364 % transmitted. On this interval the modeled value decreases, and the two-point slope is -0.46803559 % transmitted per mm. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Evidence, uncertainty, and a competing mechanism

Ion exchange depends on composition, bath contamination, temperature and time. A surface compression value alone is not a universal device-drop survival prediction.

Exercises and self-assessment

Exercise 7.4A — Physical mechanism. Why can a chemically strengthened glass fail suddenly after damage that penetrates its compression layer? State one plausible explanation, one competing explanation and the material-state observation that separates them. Relate the claim to the governing relationship written above rather than merely repeating definitions.

Exercise 7.4B — Numerical cross-check. Recalculate 94.243746 % transmitted from the companion formula at 11.85714 mm and compare with 92.973364 % transmitted at 14.57143 mm. State the sign of the sensitivity and explain whether the changed input would reasonably be controlled independently in a real ceramic specimen.

Exercise 7.4C — Test design. Propose a preparation or test matrix that addresses microcrystallites or edge damage. Give the specimen orientation, spatial sampling scheme, temperature-time record and principal instrument calibration. Explain which observation would falsify your first hypothesis and name a condition under which your model should not be used.

§7.7 Optical transmission, scattering and weathering

Scientific foundation

Transparent ceramics and glasses may absorb light through electronic transitions, color centers or impurities and scatter light at pores, grain boundaries or crystalline inclusions. The Beer–Lambert relation describes ideal exponential attenuation from a homogeneous absorbing medium; it does not by itself model multiple scattering, Fresnel interface reflections or photoluminescence. Chemical weathering can create surface layers that lower transparency even when bulk absorption is stable.

Governing relationship or decision rule: For absorption alone, I/I0=exp(-alpha x) with absorption coefficient alpha and optical path x in consistent length units. Read every term in the equation as part of a declared specimen condition. In optical transmission, scattering and weathering, a valid calculation requires the state of the ceramic, unit system and physical or geometrical meaning of each quantity. A nominally identical oxide composition can conceal different dopant distributions, porosity, grain-boundary glass and processing damage. Equal bulk density does not guarantee equivalent fracture, transport or thermal stability. Interpret measurements only after identifying which feature of the state they can support.

Worked ceramic investigation

Use the ideal absorption-only slider to compare transmission through two glass thicknesses with a declared absorption coefficient. Then estimate air–glass reflection separately, and propose a haze measurement to identify scattering. Compare polished and weathered surfaces so that absorption and surface roughness are not collapsed into one unqualified optical loss number.

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 1057.143 K, the declared formula returns 3.0869565 log10(Pa·s); at Absolute forming temperature = 1128.571 K, it returns 2.4901961 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.0083546462 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Evidence, uncertainty, and a competing mechanism

Real absorption is wavelength dependent and can be strongly nonuniform. The model intentionally excludes reflectance and microstructural scattering and must not be used for optical component qualification.

Exercises and self-assessment

Exercise 7.5A — Physical mechanism. How can a nominally colorless glass exhibit low total transmission despite a small measured absorption coefficient? State one plausible explanation, one competing explanation and the material-state observation that separates them. Relate the claim to the governing relationship written above rather than merely repeating definitions.

Exercise 7.5B — Numerical cross-check. Recalculate 3.0869565 log10(Pa·s) from the companion formula at 1057.143 K and compare with 2.4901961 log10(Pa·s) at 1128.571 K. State the sign of the sensitivity and explain whether the changed input would reasonably be controlled independently in a real ceramic specimen.

Exercise 7.5C — Test design. Propose a preparation or test matrix that addresses microcrystallites or edge damage. Give the specimen orientation, spatial sampling scheme, temperature-time record and principal instrument calibration. Explain which observation would falsify your first hypothesis and name a condition under which your model should not be used.

§7.8 Integrated investigation: Evaluate a transparent glass-ceramic window

The evidence problem

A heat-treated panel becomes mechanically harder but loses clarity and displays small edge cracks. The problem cannot be solved by selecting the equation that gives the most convenient number. First define which property must be achieved, the physical constraint that could prevent it, and the microstructural condition of the specimen being evaluated. List known facts separately from inferred mechanisms, uncertain constants and quantities not yet measured. The central decision is not simply which powder process or ceramic composition seems attractive: it is what observations would allow a researcher or an engineer to prefer one explanation over competing causes.

Integrated analysis and model workflow

Link nucleation, growth, phase fraction, absorption, scattering and edge stresses to separate measurements. Build a minimal processing–structure–property map linking the material history with observed state and relevant response. Carry the distinction between glass structure and crystallization and optical absorption versus scattering and residual stress through the map. For phase equilibria, show composition conservation and do not infer processing kinetics from a phase diagram. For a densification relation, separate pore disappearance from neck growth and grain coarsening. For electrical function, distinguish ion migration, electronic leakage, electrode polarization and nonlinear ferroelectric switching. Use the actual specimen time–temperature history instead of only a furnace setting. For damage, compare local flaw driving force with the appropriate fracture resistance.

Validation plan, report, and counterfactual

Measure diffraction, optical haze, spectral transmission and surface damage across thickness. Include an alternative interpretation capable of explaining the same first observation and choose a different instrument or held-out processing condition that separates it. State which measurement would cause you to reject the favored hypothesis. Retain raw counts, image scales, processing logs and sample identifiers. If comparing ceramic families, write down the constraints that matter for weight, stiffness, temperature, oxidation and availability rather than reporting only one maximum strength metric.

Known limits: An absorption-only optical slider omits scattering from crystallites and microcracks. A reader should be able to reconstruct the entire inference from original specimen provenance and measured inputs. The synthetic datasets intentionally contain no physical replicate scatter or hidden model mismatch; those omissions would make a real-world confidence interval far wider than a formula plot suggests.

Five cumulative exam questions

  1. Draw a cause-and-effect diagram linking composition, process history, glass structure and crystallization and the decision-controlling property; mark one arrow that cannot yet be established from the observations.
  2. Write a conservation or constitutive relation for optical absorption versus scattering and residual stress with all units and physical validity assumptions; interpret one limiting case.
  3. Propose two mutually exclusive experimental signatures for the favored and competing mechanisms and name the required independent instruments.
  4. Show how microcrystallites or edge damage could reverse a seemingly beneficial result, and design the minimum additional test needed to detect that reversal.
  5. Write a one-paragraph evidence statement specifying what has been demonstrated, what is merely predicted, and which industrial decision is unjustified until qualification.

THREE WORKED QUESTIONS

Step-by-Step Statistical Simulation and Monte Carlo Solutions

Three original questions connect calculations, definitions and interpretation. Open each solution to follow the reasoning.

Solved Problem Example 7.1: Illustrative glass log-viscosity

Create a molar batch recipe from silica, boron-containing and alkali raw materials, converting between mass and mole fraction correctly and accounting for gas released during decomposition. Compare an alkali-rich and a low-alkali glass in a proposed water-leaching experiment. Predict trends qualitatively but require measured dissolution profiles before specifying container suitability.

Step

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 771.4286 K, the declared formula returns 7.7692308 log10(Pa·s); at Absolute forming temperature = 842.8571 K, it returns 6.0322581 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.024317618 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Step

The browser expression is -3+4000/(T-400). Model validity is limited to: Synthetic VFT-like equation A=-3, B=4000 K, T0=400 K, 700<=T<=1200 K; not calibrated to any glass. Reproduce the first result with a calculator using the expression and units stated here. Before accepting the number, check the units analytically and identify what is being held constant. If a result looks realistic, that coincidence does not establish physical validation. Try an extreme permitted slider input and ask whether the computed change is physically interpretable or an artifact of the simplifying assumptions.

Solved Problem Example 7.2: Glass absorption-only transmission

Use a teaching Vogel–Fulcher–Tammann-type log-viscosity relation over an explicitly restricted 700–1200 K range. Interpret output as log10(Pa s), convert two points to viscosity units and explain how a forming window would depend on process strain rate and part thickness. Plan a beam-bending or rotational-viscosity measurement suited to the relevant viscosity regime.

Step

A companion calculator called Glass absorption-only transmission supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Optical path length = 6.428571 mm, the declared formula returns 96.836823 % transmitted; at Optical path length = 9.142857 mm, it returns 95.531487 % transmitted. On this interval the modeled value decreases, and the two-point slope is -0.48091339 % transmitted per mm. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Step

The browser expression is 100Math.exp(-5L/1000). Model validity is limited to: Monochromatic uniform absorption coefficient=5 m^-1; no scattering, interfacial reflection, interference or wavelength dependence. Reproduce the first result with a calculator using the expression and units stated here. Before accepting the number, check the units analytically and identify what is being held constant. If a result looks realistic, that coincidence does not establish physical validation. Try an extreme permitted slider input and ask whether the computed change is physically interpretable or an artifact of the simplifying assumptions.

Solved Problem Example 7.3: Illustrative glass log-viscosity

Propose a two-step heat treatment for a model glass-ceramic with one nucleation and one growth stage. Measure crystalline phase fraction by diffraction with a stated calibration, then compare surface and core microstructures to test thermal homogeneity. Use viscosity-versus-temperature only to estimate mobility trends, not to infer a nucleation rate from a single scalar equation.

Step

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 914.2857 K, the declared formula returns 4.7777778 log10(Pa·s); at Absolute forming temperature = 985.7143 K, it returns 3.8292683 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.013279133 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Solved Problem Example 7.4: Glass absorption-only transmission

Prepare a comparison of untreated and ion-exchanged sheets with measured surface stress profiles and flaw-size distributions. Examine failure after both shallow abrasion and deep scratching, while noting that the same nominal stress may be irrelevant when the flaw extends beyond the compressive layer. Measure optical distortion and durability after aging.

Step

A companion calculator called Glass absorption-only transmission supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Optical path length = 11.85714 mm, the declared formula returns 94.243746 % transmitted; at Optical path length = 14.57143 mm, it returns 92.973364 % transmitted. On this interval the modeled value decreases, and the two-point slope is -0.46803559 % transmitted per mm. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.

Solved Problem Example 7.5: Illustrative glass log-viscosity

Use the ideal absorption-only slider to compare transmission through two glass thicknesses with a declared absorption coefficient. Then estimate air–glass reflection separately, and propose a haze measurement to identify scattering. Compare polished and weathered surfaces so that absorption and surface roughness are not collapsed into one unqualified optical loss number.

Step

A companion calculator called Illustrative glass log-viscosity supplies a separate, deliberately limited numerical experiment. Its controls isolate one effect so a reader can check dimensions and sensitivity instead of guessing the direction of change. At Absolute forming temperature = 1057.143 K, the declared formula returns 3.0869565 log10(Pa·s); at Absolute forming temperature = 1128.571 K, it returns 2.4901961 log10(Pa·s). On this interval the modeled value decreases, and the two-point slope is -0.0083546462 log10(Pa·s) per K. These are worked calculations, not fabricated experimental observations or certified properties of any real ceramic formulation.