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Detailed Reference Information |
Duffy, T.S. and Ahrens, T.J. (1995). Compressional sound velocity, equation of state, and constitutive response of shock-compressed magnesium oxide. Journal of Geophysical Research 100: doi: 10.1029/94JB02065. issn: 0148-0227. |
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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 US =6.87(10)+1.24(4)up, where the numbers in parentheses are one standard deviation uncertainties in the last digit(s). Reverse-impact wave profiles constrain the compressional sound velocity, VP, at 10--27 GPa to ¿2%. Measured VP 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. ¿ American Geophysical Union 1995 |
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Abstract |
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Keywords
Mineral Physics, Equations of state, Mineral Physics, Elasticity and anelasticity, Mineral Physics, High-pressure behavior, Mineral Physics, Shock wave experiments |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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