The increased refractive index of diopside and albite glass, quenched from liquidus temperatures at pressures to 50 kb, can be accurately calculated from compressibility data on the crystals at 25°C and the Lorentz-Lorenz refraction law. The results indicate that the pressure effect is locked in by ‘configurational trapping’ on cooling through the glass point, but thermal relaxation takes place with the thermal expansion coefficient characteristic of the applied pressure. The resulting permanent compression is therefore that predicted at 25°C and load pressure. Permanent compression of glasses at temperatures below the glass point should be that predicted at load pressure and (1) 25°C, if temperature is released before pressure, or (2) run temperature, if pressure is released before temperature, because thermal relaxation then takes place with the low-pressure thermal expansion coefficient. For SiO2 the glass compressibility is known as a function of temperature, and the overlap field parameter (β = 1.37) can be established from other data. Refractive indices of SiO2 glass compressed at various P and T with varying quenching cycles are consistent with the values calculated for permanent compression when T > ∼500°C. At lower temperatures the compression is partly elastic and the resultant indices are thus lower than expected. In all these glasses, configurational trapping of pressure deformation is adequate to explain the permanent compression. The direct relationship of permanent compression with compressibility shows that the model of H. M. Cohen and R. Roy (1961, 1965), based on second-order structural changes at high P followed by elastic decompression, is not necessary to explain any of the existing data.
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