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Detailed Reference Information |
Mashimo, T., Kondo, K., Sawaoka, A., Syono, Y., Takei, H. and Ahrens, T.J. (1980). Electrical conductivity measurement of fayalite under shock compression up to 56 GPa. Journal of Geophysical Research 85: doi: 10.1029/JB085iB04p01876. issn: 0148-0227. |
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The electrical conductivity measurements of single-crystal fayalite are performed under shock wave compression in the pressure range 19.5--56 GPa. The electrical conductivity under shock compression increases by a factor of more than 1010 from 0 to 40 GPa. Over the range 19.5--42 GPa the specific conductivity &sgr; can be closely described by log10 &sgr; (S/m) =-4.65+0.15P (GPa). The conductivity versus pressure relation at room temperature is calculated by suing measured values of the activation energy to correct the high-temperature shock data to room temperature. After the effect of temperature is removed, the increase in conductivity with pressure approximatley agrees with that measured under static pressure using a diamond anvil cell by Mao and Bell. Above pressures of ~42 GPa the conductivity remains at a relatively high level of ~100 S/m from 40 to 55 GPa. |
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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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