Abstract
Heat capacity Cv and entropy S for pyrope and grossular are calculated using a statistical thermodynamic approach and a density of states derived from previous single-crystal infrared and Raman spectra obtained for natural, nearly end-member garnets. Preferred values of thermodynamic properties in J/mol K at 298.15 K are Cp(Py)=326.0±0.5, S(Py)=256±1, Cp(Gr)=333.5±0.5, and S(Gr)=265±2. Excess entropy of grossular compared to pyrope results from the larger mass of the Ca ion; however, its magnitude is limited by the large size of the Ca ion, which dilates the Si-O bond through edge sharing of the larger dodecahedra with the tetrahedra, leading to changes in the force constants that raise the frequency of the lowest lying translations of the SiO4 tetrahedron. This type of compositional dependence of bonding is inferred to regulate mixing properties of garnets. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 880-891 |
| Number of pages | 12 |
| Journal | American Mineralogist |
| Volume | 76 |
| Issue number | 5-6 |
| State | Published - 1991 |
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