The effect of water on the electrical conductivity of olivine aggregates and its implications for the electrical structure of the upper mantle

By T. Yoshino, Takuya Matsuzaki, A. Shatskiy, T. Katsura. 2009

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Electrical conductivity anisotropy of dry and hydrous olivine at 8 GPa (2010, methodology): “The values of α from Yoshino et al. (2009) for olivine and from Yoshino et al. 374 (2008) for wadsleyite and ringwoodite range between 9x10-4 to 0.03.”
Laboratory Electrical Conductivity Measurement of Mantle Minerals (2010, background): “Fig. 25 Electrical conductivity of mantle minerals with Mg# = *90; olivine ( Yoshino et al. 2009 ), wadsleyite (Yoshino et al. 2008a), ringwoodite (Yoshino et al. 2008a), silicate perovskite (Al-PV) (Yoshino et al. 2008c), ferro-periclase (FP) (Yoshino et al. 2008c) and postperovskite (PPV) (Ohta et”
Water distribution across the mantle transition zone and its implications for global material circulation (2011, unknown): “However, the magnitude of this effect is small when the appropriate technique (the impedance spectroscopy) is used (Dai and Karato, 2009c; Yoshino et al., 2009).”
On the Causes of Electrical Conductivity Anomalies in Tectonically Stable Lithosphere (2013, background): “diffusion (Yoshino et al. 2009; Wang et al. 2006, 2012; Poe et al. 2010; Karato 2006).”