European Journal of Mineralogy · 1990 · 423 citations · 42 references
Natural SciencesMaterials SciencePhysicsMineralogyPhase TransformationsThermodynamicsCrystallization ProcessesNucleationPartial MeltingPhase TransitionsSilicate MineralsThermal DiffusivitySilicate Melt StructureSilicate Phase EquilibriaSilicate Thermodynamics
The glass transition is a kinetic barrier that divides the behavior of silicate melts into two types, liquid and glassy. Liquid behavior is the equilibrium response of a melt to an applied perturbation, resulting in the determination of an equilibrium liquid property. The equilibrium may be stable (superliquidus) or metastable (subliquidus). Glassy behavior occurs when the timescale of the perturbation is too short for melt equilibration. This can occur when the frequency of an applied sinusoidal perturbation is too high or when the observation time of an experiment is too short. The time-or frequency-dependent response of the structure and properties of a melt to a perturbation is termed relaxation. Liquid and glassy behavior are relaxed and unrelaxed behavior, respectively.
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The viscosity of magmatic silicate liquids; a model calculation
D. F. Weill · American Journal of Science · 1972 · 755 citations · Full text
Medicine, Immunology, Oncology +17
Relaxation in glass and composites
D. E. Packham · Composites Science and Technology · 1987 · 558 citations
Natural Sciences, Materials Engineering, Materials Science +10