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Transport properties of olivine grain boundaries from electrical conductivity experiments

TitleTransport properties of olivine grain boundaries from electrical conductivity experiments
Publication TypeJournal Article
Year of Publication2018
AuthorsPommier A., Kohlstedt D.L, Hansen L.N, Mackwell S., Tasaka M., Heidelbach F., Leinenweber K.
JournalContributions to Mineralogy and Petrology
Volume173
Date Published2018/05
Type of ArticleArticle
ISBN Number0010-7999
Accession NumberWOS:000431440800008
Keywordsasthenosphere; continental-crust; diffusion; Electrical anisotropy; electrical conductivity; forsterite; Geochemistry & Geophysics; Grain boundaries; hydrous olivine; impedance; mineralogy; Olivine; seismic anisotropy; Shear strain; simulations; strain; upper-mantle
Abstract

Grain boundary processes contribute significantly to electronic and ionic transports in materials within Earth's interior. We report a novel experimental study of grain boundary conductivity in highly strained olivine aggregates that demonstrates the importance of misorientation angle between adjacent grains on aggregate transport properties. We performed electrical conductivity measurements of melt-free polycrystalline olivine (Fo(90)) samples that had been previously deformed at 1200 degrees C and 0.3 GPa to shear strains up to gamma = 7.3. The electrical conductivity and anisotropy were measured at 2.8 GPa over the temperature range 700-1400 degrees C. We observed that (1) the electrical conductivity of samples with a small grain size (3-6 mu m) and strong crystallographic preferred orientation produced by dynamic recrystallization during large-strain shear deformation is a factor of 10 or more larger than that measured on coarse-grained samples, (2) the sample deformed to the highest strain is the most conductive even though it does not have the smallest grain size, and (3) conductivity is up to a factor of similar to 4 larger in the direction of shear than normal to the shear plane. Based on these results combined with electrical conductivity data for coarse-grained, polycrystalline olivine and for single crystals, we propose that the electrical conductivity of our fine-grained samples is dominated by grain boundary paths. In addition, the electrical anisotropy results from preferential alignment of higher-conductivity grain boundaries associated with the development of a strong crystallographic preferred orientation of the grains.

DOI10.1007/s00410-018-1468-z
Short TitleContrib. Mineral. Petrol.
Student Publication: 
No
Research Topics: 
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