COMPRESSIONAL SOUND-VELOCITY, EQUATION OF STATE, AND CONSTITUTIVE RESPONSE OF SHOCK-COMPRESSED MAGNESIUM-OXIDE

被引:103
作者
DUFFY, TS [1 ]
AHRENS, TJ [1 ]
机构
[1] CALTECH, SEISMOL LAB, PASADENA, CA 91125 USA
关键词
D O I
10.1029/94JB02065
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
Wave profile and equation of state (EOS) data are reported for low-porosity polycrystalline magnesium oxide under shock compression. The Hugoniot equation of state between 14 and 133 GPa is U-S 6.87(10) + 1.24(4)u(p), where the numbers in parentheses are one standard deviation uncertainties in the last digit(s). Reverse-impact wave profiles constrain the compressional sound velocity, V-P, at 10-27 GPa to +/-2%. Measured V-P values are consistent with ultrasonic data extrapolated from 3 GPa. By combining the Hugoniot results with ultrasonic data, the adiabatic bulk modulus and its first and second pressure derivatives at constant entropy are 162.5(2) GPa, 4.09(9), and -0.019(4) GPa(-1). The shear modulus and its first and second pressure derivatives are 130.8(2) GPa, 2.5(1), -0.026(45) GPa(-1) Polycrystalline MgO has a compressive yield strength of 1-1.5 GPa at the elastic limit which increases to 2.7(8) GPa along the Hugoniot and is similar at unloading. Wave profiles for MgO at 10-39 GPa are described using a modified elastic-plastic model. There are significant differences in the dynamic response of single-crystal and polycrystalline MgO.
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页码:529 / 542
页数:14
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