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ReportsStructure and Freezing of MgSiO3 Liquid in Earth's Lower Mantle![]()
First-principles molecular-dynamics simulations show that over the pressure regime of Earth's mantle the mean silicon-oxygen coordination number of magnesium metasilicate liquid changes nearly linearly from 4 to 6. The density contrast between liquid and crystal decreases by a factor of nearly 5 over the mantle pressure regime and is 4% at the core-mantle boundary. The ab initio melting curve, obtained by integration of the Clausius-Clapeyron equation, yields a melting temperature at the core-mantle boundary of 5400 ± 600 kelvins.
1 Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA. * On leave from Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
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Science. ISSN 0036-8075 (print), 1095-9203 (online)