Equations of State for Solids in Geophysics and Ceramic ScienceOxford University Press, 12 janv. 1995 - 432 pages Written by a renowned expert in the field, this book is the most comprehensive treatment available on the applications of equations of state (EoS) in geophysics and materials science, a topic of fundamental importance to those studying the physics and chemistry of the Earth. Part one offers comprehensive treatments of thermal properties associated with EoS, thermodynamic and statistical mechanical backgrounds, and thermoelastic properties. Definitions of the physical properties needed for the EoS are provided as well. Part two discusses the isothermal pressure-volume relationship. The ab initio approach--EoS based upon quantum mechanics fundamentals using numerical methods--is utilized to clearly represent and analyze the measured data. Part three offers an advanced treatment of thermal properties at high temperature, and includes discussions of thermal pressure, shocked solids, and EoS applications to materials science topics such as melting and thermodynamic function. Advanced students, researchers, and professionals in geophysics, ceramics science, solid state physics, and geochemistry will want to read this book. |
Table des matières
1 | |
PART II ISOTHERMAL EQUATIONS OF STATE | 157 |
PART III THERMAL PROPERTIES AT HIGH PRESSURE | 241 |
APPENDIXES | 355 |
GLOSSARY OF SYMBOLS | 371 |
379 | |
383 | |
Autres éditions - Tout afficher
Equations of State of Solids for Geophysics and Ceramic Science Orson L. Anderson Aperçu limité - 1995 |
Equations of State of Solids for Geophysics and Ceramic Science Orson L. Anderson Aucun aperçu disponible - 1995 |
Expressions et termes fréquents
acoustic adiabatic anharmonic atoms Boehler Born-Mie bulk modulus calculated Chapter Chopelas compression computed crystal CsCl curve Debye function Debye temperature Debye theory density Earth Planet elastic constants energy entropy equation experimental finite strain forsterite frequency function Geophys geophysics Grüneisen parameter Helmholtz energy high pressure high temperature Hugoniot independent inner core interatomic iron Isaak isobar isochores isothermal Jeanloz lattice Lindemann law linear lower mantle measured melting Mg2SiO4 minerals modes modified from Anderson NaCl olivine oxides and silicates periclase phase Phys physical plot Poisson's ratio potential PREM pressure derivative properties quasiharmonic approximation repulsive seismic Shankland shear constants shock wave shown in Fig silicate perovskite solid sound velocity specific heat Stacey stishovite structure Sumino Table thermal expansivity thermal pressure thermodynamic thermoelastic parameters versus vibrational volume ακτ ӘР бт
Fréquemment cités
Page ix - I shall be telling this with a sigh Somewhere ages and ages hence: Two roads diverged in a wood, and I— I took the one less traveled by, And that has made all the difference.
Page 379 - Therefore if I know not the meaning of the voice, I shall be unto him that speaketh a barbarian ; and he that speaketh shall be a barbarian unto me.
Page vi - Centolella (1995) with kind permission from Elsevier Science, Ltd., The Boulevard, Langford Lane, Kidlington, 0X5 1Gb, UK.