Toward a unified hydrous olivine electrical conductivity law
Abstract
It has long been proposed that water incorporation in olivine has dramatic effects on the upper
mantle properties, affecting large scale geodynamics and triggering high electrical
conductivity. But the laboratory-based laws of olivine electrical conductivity predict
contrasting effects of water, precluding the interpretation of geophysical data in term of
mantle hydration. We review the experimental measurements of hydrous olivine conductivity
and conclude that most of data are consistent when errors in samples water contents are
considered. We report a new law calibrated on the largest database of measurements on
hydrous olivine oriented single crystals and polycrystals. It fits most of measurements within
uncertainties, and is compatible with most of geophysical data within petrological constraints
on mantle olivine hydration. The isotropic conductivity (S/m) is
where CH2O is the water concentration in olivine (wt.ppm) and T the temperature (K). The
conductivity anisotropy of hydrous olivine might be higher than dry olivine, but preferential
orientation should produce moderate anisotropy (~0–0.8 log unit). In the oceanic mantle, the
enhancement of olivine conductivity is limited to ~1 log unit in the maximum range of mantle
olivine water concentrations (0–500 wt.ppm). Strongest enhancements are expected in colder
regions, like cratonic lithospheres and subduction settings. High conductivities in melt-free
mantle require great depths and high water concentrations in olivine (>0.1 S/m at >250 km
and >200 wt.ppm). Thus, the hydration of olivine appears unlikely to produce the highest
conductivities of the upper mantle.
Domains
Volcanology
Origin : Publisher files allowed on an open archive
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