Elasticity of MgO to 11 GPa with an independent absolute pressure scale: Implications for pressure calibration

被引:61
|
作者
Li, Baosheng [1 ]
Woody, Kelly
Kung, Jennifer
机构
[1] SUNY Stony Brook, Inst Mineral Phys, Stony Brook, NY 11794 USA
[2] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
关键词
D O I
10.1029/2005JB004251
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
P and S wave velocities and unit cell parameters (density) of MgO are measured simultaneously up to 11 GPa using combined ultrasonic interferometry and in situ X-ray diffraction techniques. The elastic bulk and shear moduli as well as their pressure derivatives are obtained by fitting the measured velocity and density data to the third-order finite strain equations, yielding K-0S=163.5(11) GPa, K'(0S)=4.20(10), G(0)=129.8(6) GPa, and G'(0)=2.42(6), independent of pressure. These properties are subsequently used in a Birch-Murnaghan equation of state to determine the sample pressures at the observed strains. Comparison of the 300K isothermal compression of MgO indicates that current pressure scales from recent studies are in better than 1.5% agreement. We find that pressures derived from secondary pressure standards (NaCl, ruby fluorescence) at 300K are lower than those from current MgO scales by 5-8% (similar to 6% on average) in the entire pressure range of the current experiment. If this is taken into account, discrepancy in previous static compression studies on MgO at 300K can be reconciled, and a better agreement with the present study can be achieved.
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页数:10
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