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Low frequency electrical response of polycrystalline olivine compacts: Grain boundary transport
Author(s) -
Tyburczy James A.,
Roberts Jeffery J.
Publication year - 1990
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl017i011p01985
Subject(s) - grain boundary , grain boundary diffusion coefficient , grain size , olivine , electrical resistivity and conductivity , crystallite , mineralogy , materials science , conductivity , grain growth , geology , condensed matter physics , composite material , metallurgy , electrical engineering , microstructure , physics , engineering , quantum mechanics
The complex electrical impedance of sintered, polycrystalline compacts of San Carlos olivine (grain size 75–180 μm) has been determined over the frequency range 10 4 to 10 −4 Hz, at temperatures between 800 and 1400°C, at the f O 2 of the wustite‐magnetite buffer. Complex plane plots (Im Z vs. Re Z) show separate effects of grain interior and grain boundary conductivity. Grain interior transport controls the response above ∼10 2 Hz, whereas grain boundary transport dominates between ∼10 2 and 10 −2 Hz. Overall response of the compacts is modeled with an equivalent circuit in which parallel RC circuit elements representing grain interior and grain responses act in series . Bulk DC conductivity is lower than either grain interior or grain boundary conductivity alone. Inversion of magnetotelluric profiles that employ lower bulk conductivities of the grain interior‐grain boundary system yield upper mantle temperature estimates 30 to 50°C higher than those based on single crystal values.