P-V-T equation of state of platinum to 80GPa and 1900K from internal resistive heating/x-ray diffraction measurements

The P-V-T equation of state (EOS) of Pt has been determined to 80GPa and 1900K by in situ x-ray diffraction of a mixture of Pt and MgO using a modified internal resistive heating technique with a diamond anvil cell. The third-order Birch–Murnaghan EOS of Pt at room temperature can be fitted with K0=273.5±2.0GPa, K0′=4.70±0.06, with V0=60.38A3. High temperature data have been treated with both thermodynamic and Mie–Gruneisen-Debye methods for the thermal EOS inversion. The results are self-consistent and in excellent agreement with those obtained by the multianvil apparatus where the data overlap. MgO is taken as the standard because its thermal EOS is well established and based on a wealth of experimental and theoretical data, and because the EOS at room temperature has been determined by a primary method that is completely independent of any assumptions or measurements by other methods. Improvements to previous internal resistive heating methods were made by using a Re gasket that replaces the original g...

[1]  Baosheng Li,et al.  Elasticity of MgO to 11 GPa with an independent absolute pressure scale: Implications for pressure calibration , 2006 .

[2]  W. Nellis,et al.  The ruby pressure standard to 150 GPa , 2005 .

[3]  W. Nellis,et al.  High-pressure equations of state of Al, Cu, Ta, and W , 2005 .

[4]  Takeyuki Uchida,et al.  Pressure calibration to 20 GPa by simultaneous use of ultrasonic and x-ray techniques , 2005 .

[5]  M. Mezouar,et al.  Equations of state of six metals above 94 GPa , 2004 .

[6]  C. Zha,et al.  Rhenium, an in situ pressure calibrant for internally heated diamond anvil cells , 2004 .

[7]  K. Hirose,et al.  A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements , 2004 .

[8]  C. Zha,et al.  Internal resistive heating in diamond anvil cell for in situ x-ray diffraction and Raman scattering , 2003 .

[9]  T. Kikegawa,et al.  Laser heated diamond anvil apparatus at the Photon Factory and SPring-8: Problems and improvements , 2001 .

[10]  D. Andrault,et al.  Synchrotron radiation and laser heating in a diamond anvil cell , 2001 .

[11]  S. Sutton,et al.  Laser heated diamond cell system at the Advanced Photon Source for in situ x-ray measurements at high pressure and temperature , 2001 .

[12]  H. Mao,et al.  Quasi‐hydrostatic compression of magnesium oxide to 52 GPa: Implications for the pressure‐volume‐temperature equation of state , 2001 .

[13]  H. Mao,et al.  Elasticity of MgO and a primary pressure scale to 55 GPa. , 2000, Proceedings of the National Academy of Sciences of the United States of America.

[14]  A. Dewaele,et al.  P‐V‐T equation of state of periclase from synchrotron radiation measurements , 2000 .

[15]  S. C. Parker,et al.  The MD simulation of the equation of state of MgO: Application as a pressure calibration standard at high temperature and high pressure , 2000 .

[16]  O. Anderson The volume dependence of thermal pressure in perovskite and other minerals , 1999 .

[17]  H. Mao,et al.  Brillouin scattering and X-ray diffraction of San Carlos olivine: direct pressure determination to 32 GPa , 1998 .

[18]  I. Jackson,et al.  ANALYSIS OF P-V-T DATA : CONSTRAINTS ON THE THERMOELASTIC PROPERTIES OF HIGH-PRESSURE MINERALS , 1996 .

[19]  A. Jephcoat,et al.  Temperature measurement and melting determination in the laser-heated diamond-anvil cell , 1996, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[20]  R. Cohen,et al.  High pressure effects on thermal properties of MgO , 1995, mtrl-th/9503007.

[21]  G. R. Gathers,et al.  The equation of state of platinum to 660 GPa (6. 6 Mbar) , 1989 .

[22]  O. Anderson,et al.  Anharmonicity and the equation of state for gold , 1989 .

[23]  Peter M. Bell,et al.  Calibration of the ruby pressure gauge to 800 kbar under quasi‐hydrostatic conditions , 1986 .

[24]  Reinhard Boehler,et al.  Melting temperature, adiabats, and Grüneisen parameter of lithium, sodium and potassium versus pressure , 1983 .

[25]  H. L. Johnston,et al.  High Temperature Structure and Thermal Expansion of Some Metals as Determined by X‐Ray Diffraction Data. I. Platinum, Tantalum, Niobium, and Molybdenum , 1951 .

[26]  Russell J. Hemley,et al.  Ultrahigh-pressure mineralogy : Physics and chemistry of the earth's deep interior , 1998 .

[27]  O. Anderson,et al.  A thermodynamic theory of the Grüneisen ratio at extreme conditions: MgO as an example , 1993 .

[28]  L. Gerward,et al.  Application of X-ray energy-dispersive diffraction for characterization of materials under high pressure , 1989 .

[29]  Murli H. Manghnani,et al.  Pressure Measurement at High Temperature in X-Ray Diffraction Studies: Gold as a Primary Standard , 1982 .

[30]  日本学術振興会,et al.  High-Pressure Research in Geophysics , 1982 .

[31]  W. Bassett,et al.  Disproportionation of Fe2SiO4 to 2FeO+SiO2 at pressures up to 250kbar and temperatures up to 3000 °C , 1972 .