Measurements of the electrical conductivity of silicate perovskite at
25 gigapascals and 1400 degrees to 1600 degrees C show that the conduc
tivity of (Mg,Fe)SiO3 perovskite containing 2.89 weight percent Al2O3
is about 3.5 times greater than that of aluminum-free (Mg0.915Fe0.085)
SiO3 perovskite. The conduction mechanism in perovskite between 1400 d
egrees and 1600 degrees C is most Likely by polarons, because Mossbaue
r studies show that the aluminum-bearing perovskite has about 3.5 time
s the amount of Fe3+ as the aluminum-free sample. A conductivity-depth
profile from 660 to 2900 kilometers based on aluminum-bearing perovsk
ite is consistent with geophysical models.