By Hideo Aoki, Yasuhiko Syono, Russell J. Hemley
Condensed topic physics results in a "first-principles" manner of crystals, permitting physicists and mineralogists to check the wealthy and occasionally unforeseen habit that minerals express below the extraordinary stipulations in the earth. This quantity absolutely info the intriguing interplay among geophysics and condensed subject physics. top overseas researchers from either geosciences and condensed subject physics element this leading edge, interdisciplinary box. the quantity is a wonderful precis for experts and graduate scholars studying mineralogy and crystallography.
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Extra info for Physics Meets Mineralogy: Condensed Matter Physics in the Geosciences
Bragg, Atomic Structure of Minerals, Oxford Univ. Press, 1937, Chap. 12. Y Matsui and Y Syono, Geochem. J. 2,51(1968). Y Matsui, Y Syono, S. Akimoto, and K. Kitayama, Geochem. J. 2,61 (1968). Y Syono, S. Akimoto, and Y Matsui, J. Solid State Chem. 3, 369 (1971). O. Nishizawa and Y Matsui, Phys. Earth Planet. Inter. 6, 377 (1972). Y Matsui and O. Nishizawa, Bull. Soc. Fr. Mineral. Cristallogr. 97, 122 (1974). T. Kawasaki and Y Matsui, Earth Planet. Sci. Lett. 37, 159 (1977). H. Higuchi, N. Onuma, H.
78, 2413 (1998).  L. Nagel and M. O'Keeffe, Mater. Res. Bull. 6, 1317(1971).  K. Kusaba, Y. Syono and Y. Matsui, in Shock Compression of Condensed Matter -1989, by S. C. Schmidt, J. N. Johnson, and L. W. Davidson, eds. (Elsevier, New York, 1990), p. 135.  Y. Tsuchida and T. Yagi, Nature (London) 340, 217 (1989).  Y. Matsui and S. Tsuneyuki, in High-Pressure Research: Application to Earth and Planetary Sciences, Y. Syono and M. H. Manghnani, eds. , 1992), p. 433.  K. J. Kingma, R.
This is important for two related reasons. First, it allows us to determine groundstate crystal structures very effectively. This has become possible only recently for relatively complex structures such as MgSiO3 perovskite . 3 Computation 31 has been the development of a structural optimization strategy based on a pseudoLagrangian that treats the components of the strain tensor and the atomic positions as dynamical variables . The optimization is performed at constant pressure. At each step of the dynamical trajectory, the Hellman-Feynman forces and stresses  acting on the nuclei and the lattice parameters, respectively, are evaluated and used to generate the next configuration.
Physics Meets Mineralogy: Condensed Matter Physics in the Geosciences by Hideo Aoki, Yasuhiko Syono, Russell J. Hemley