Abstract
Ab initio two-phase molecular dynamics simulations were performed on silica at pressures of 20–160 GPa and temperatures of 2 500–6 000 K to examine its solid-liquid phase boundary. Results indicate a melting temperature (T m) of 5 900 K at 135 GPa. This is 1 100 K higher than the temperature considered for the core-mantle boundary (CMB) of about 3 800 K. The calculated melting temperature is fairly consistent with classical MD (molecular dynamics) simulations. For liquid silica, the O-O coordination number is found to be 12 along the T m and is almost unchanged with increasing pressure. The self-diffusion coefficients of O and Si atoms are determined to be 1.3×10−9–3.3×10−9 m2/s, and the viscosity is 0.02–0.03 Pa·s along the T m. We find that these transport properties depend less on pressure in the wide range up of more than 135 GPa. The eutectic temperatures in the MgO-SiO2 systems were evaluated and found to be 700 K higher than the CMB temperature, though they would decrease considerably in more realistic mantle compositions.
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This study was supported by the Japan Society for the Promotion of Science (No. 21740330) to Yusuke Usui, (No. 19740331) to Taku Tsuchiya, and a fellowship from the Global-COE program “Deep Earth Mineralogy” to Yusuke Usui.
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Usui, Y., Tsuchiya, T. Ab initio two-phase molecular dynamics on the melting curve of SiO2 . J. Earth Sci. 21, 801–810 (2010). https://doi.org/10.1007/s12583-010-0126-9
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DOI: https://doi.org/10.1007/s12583-010-0126-9