Katsura's High-Pressure Earth
  • Home
  • CV
  • Publications
  • Research
    • Technologies
      • UHP generation
      • UHT generation
      • Homogeneous temperature
      • In situ X-rays observation
      • Rapid quench
    • Phase relations
      • Akm-Brg transition
      • Curved post-garnet transition
      • Sharp post-spinel transition
      • Post-spinel pressure
      • Binary ol-wd transition
      • Psp transition in Mg2SiO4
      • H2O in majorite
    • Mineral chemistry and structure
      • P dependence of Fe3+ in Brg Mg-rich
      • Brg is dry
      • T dependence of Fe3+ in Brg Mg-rich
      • Al in Brg at 3000 K
      • T dependence of MgAlO2.5
      • MgAlO2.5 vs bulk Mg/Si
      • Clustering of O vacancies
      • MgSiO3-Al2O3 at P-T
      • MgAlO2.5 in Brg with P
      • High H2O in Rw
      • H+ substitution mechanism in Fo
      • LiNbO3-type Mg3Al2Si3O12
      • LiNbO3-type (Mg,Fe3+)(Al3+,Si)O3
    • Melt
      • Zero-temperature gradient
      • Rapid quench
    • Electrical conductivity
      • H2O enhancement of ionic conductivity
    • Rheolgical properties
      • E-type slip
      • P-dependence of [100](010) and [001](010) dislocations
      • T-dependence of [100](010) and [001](010) dislocation mobility
      • Si and O diffusion mechanism
      • Si grain-boundary diffusion in Fo
      • H2O Effect of O diffusion in Fo
      • H2O effect on Si lattice diffusion in Fo
    • Thermoelastic properties
      • PVT measurement
      • Adiabatic temperature profile
      • Re-evaluation of T at D410
      • Adiabat
    • Developement of HPT technology
      • SPEED-Mk.II
      • Ultrahigh-pressure MAP
    • Material Science
  • Lecture Note
    • Mineral Physics 2021-22
    • Thermodynamics
      • 1st law and internal energy
    • Thermochemistry
      • G change of ideal gas with P
      • multi-comonent chemical potential
      • Standard pressure, single-component
      • Standard pressure, multi-component
      • High pressures, multi-component
    • Equation of state
      • What is EOS?
      • Isothermal EOS
      • Simplest EOS
      • Finite Strain
      • BM2 EOS
      • Proof a in BMEOS
      • BM3 EOS
      • Proof 3b/2a in BMEOS
      • Vinet EOS
      • Murnaghan EOS
      • Comparison of EOS's
      • Why squared length
      • Why not L but E
      • Thermal EOS
      • Thermal expansion
      • Path HC
      • Grüneisen parameter
      • Path CH
      • A-G parameter
    • Physics of the Earth's interior
    • Mineral Physics 2020
      • Background of thermodynamics
      • Heat capacity
      • Bulk modulus
      • Adiabat
      • Grüneisen paramter
      • Background for elasticity
      • Strain
      • Linear elasticity
      • Stress
      • Elastic constants of crystals
    • Geotherm Table
  • Home
  • CV
  • Publications
  • Research
    • Technologies
    • Phase relations
    • Mineral chemistry and structure
    • Melt
    • Electrical conductivity
    • Rheolgical properties
    • Thermoelastic properties
      • PVT measurement
      • Adiabatic temperature profile
      • Re-evaluation of T at D410
      • Adiabat
    • Developement of HPT technology
    • Material Science
  • Lecture Note

Thermoelastic properties


Past projects

Adiabatic temperature profile in the mantle

Return to Research

 

Tomoo Katsura, Ph.D.

Professor of Structure and Dynamics of Earth Materials

Bayerisches Geoinstitut, University of Bayreuth
95440 Bayreuth, GERMANY
TEL: +49-921-55-3791
FAX: +49-921-55-3769
E-mail: [email protected]

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