Effect of mass disorder on the lattice thermal conductivity of MgO periclase under pressure
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/srep02400.pdf
Reference37 articles.
1. Manthilake, G. M., de Koker, N., Frost, D. J. & McCammon, C. A. Lattice thermal conductivity of lower mantle minerals and heat flux from Earth's core. Proceedings of the National Academy of Sciences 108, 17901–17904, 10.1073/pnas.1110594108 (2011).
2. de Koker, N. Thermal conductivity of MgO periclase at high pressure: Implications for the D'' region. Earth Planet Sc Lett 292, 392–398 (2010).
3. Haigis, V., Salanne, M. & Jahn, S. Thermal conductivity of MgO, MgSiO3 perovskite and post-perovskite in the Earth's deep mantle. Earth Planet Sc Lett 355–356, 102–108 (2012).
4. Stackhouse, S., Stixrude, L. & Karki, B. B. Thermal Conductivity of Periclase (MgO) from First Principles. Phys Rev Lett 104, 208501 (2010).
5. Ohta, K. et al. Lattice thermal conductivity of MgSiO3 perovskite and post-perovskite at the core–mantle boundary. Earth Planet Sc Lett 349–350, 109–115 (2012).
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