Vitreous forsterite (Mg2SiO4): Synthesis, structure, and thermochemistry

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Abstract

Here we report the first synthesis of a forsterite (Mg2SiO4) composition glass as an essentially phase-pure bulk material. Under containerless conditions, with heterogeneous nucleation sites minimized, glass forms by cooling ca. 1 mm liquid Mg2SiO4 droplets in oxygen at 700 K/s. 29Si NMR spectroscopic data indicate that the SiO4 tetrahedra and MgO6 octahedra exist in a corner sharing arrangement in the glass, but upon crystallization the polyhedral units reorganize to form edge-sharing linkages. Transposed temperature drop calorimetry shows that the glass is 61.4 ± 1.3 kJ/mol higher in enthalpy than the crystal.

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Tangeman, J. A., Phillips, B. L., Navrotsky, A., Weber, J. K. R., Hixson, A. D., & Key, T. S. (2001). Vitreous forsterite (Mg2SiO4): Synthesis, structure, and thermochemistry. Geophysical Research Letters, 28(13), 2517–2520. https://doi.org/10.1029/2000GL012222

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