The electrical conductivity of H2O in solid and liquid phases has been
measured at 0.21-4.18 GPa and 20-355 degrees C. The results indicate:
(i) different phases of H2O in solid have different relations between
electrical conductivity and temperature and pressure. The conductivit
y changes continuously with temperature, but discontinuously with the
pressure between 2.11 and 2.58 GPa, which corresponds to the transform
ing pressure between ice (VI) and ice (VII); (ii) the conductivity of
H2O in liquid all increases with temperature and pressure, but there a
re discontinuities at pressures between 0.57 and 0.9 GPa, and between
2.11 and 2.58 GPa, which are also consistent with the polymorph of ice
(ice (V), ice (VI) and ice (VII)). This reflects that H2O in liquid a
t different pressures has quite different properties of electron chemi
stry. It is probably the important reason that causes the layers with
high electrical conductivity and low velocity in the earth's crust and
upper mantle.