EarthRef.org Reference Database (ERR)
Development and Maintenance by the EarthRef.org Database Team

Detailed Reference Information
Mashimo et al. 1980
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.

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.

BACKGROUND DATA FILES

Abstract

Journal
Journal of Geophysical Research
http://www.agu.org/journals/jb/
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
Click to clear formClick to return to previous pageClick to submit