Answers are grounded in this paper and cite their sources.
The electrical conductivity of periclase and olivine (10.4 and 17.5% fayalite) was measured under uniaxial pressures to 42 kb at temperatures to 1200°K. The activation energy of periclase is about 1 ev and does not change with pressure to 42 kb. Comparison of results from conductivity, thermoelectric-power, transport-number, ion-diffusion, and absorption studies demonstrates the difficulties in deducing the type of charge carriers in periclase. For olivine an increase in fayalite content results in an increase in conductivity, a decrease in activation energy, and a greater pressure dependence for the activation energy; the activation energy decreases with increasing pressure.
No takes yet. Share an insight, caveat, or question.
R.M. Hamilton (1965) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: