Solubility of hydrogen in olivine: dependence on temperature and iron content

By Y. Zhao, S. Ginsberg, D. Kohlstedt. 2004

214 citations recorded by the source corpus.

Subfields: Electronic, Optical and Magnetic Materials, Geophysics

View Paper: https://www.semanticscholar.org/paper/0bdbbdd053a2ae197bf9a6e29794939812110089

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Citations in the corpus

Implications of grain size evolution on the seismic structure of the oceanic upper mantle (2008, methodology): “In the case of water content, this would require values well above 460 the solubility of water in olivine (Zhao et al., 2004; Figure 10B&D).”
Hydrogen incorporation in olivine from 2–12 GPa (2006, background): “Second, experiments by different groups have yielded highly varying estimates for OH solubility in nominally Fe-free forsterite (Kohn 1996; Keppler and Rauch 2000; Locke et al. 2001; Demouchy and Mackwell 2003; Lemaire et al. 2004; Zhao et al. 2004).”
Intercalibration of FTIR and SIMS for hydrogen measurements in glasses and nominally anhydrous minerals (2007, background): “…and Kohlstedt 1992, 1993; Bell 1992; Bell et al. 2003; Beran and Putnis 1983; Berry et al. 2005; Freund and Oberheuser 1986; Khisina and Wirth 2002; Kitamura et al. 1987; Kohlstedt et al. 1996; Lemaire et al. 2004; Matsyuk and Langer 2004; Matveev et al. 2001; Miller et al. 1987; Zhao et al. 2004).”
Pressure and temperature-dependence of water solubility in Fe-free wadsleyite (2005, background): “More recently, experimental calibrations of water solubility in these minerals became available (Kohlstedt et al. 1996; Lu and Keppler 1997; Rauch and Keppler 2002; Mierdel and Keppler 2004; Bromiley and Keppler 2004; Zhao et al. 2004).”
A new analysis of experimental data on olivine rheology (2008, methodology): “is met, then one can calculate the water content in the sample from the experimental results of water solubility [e.g., Kohlstedt et al., 1996; Zhao et al., 2004].”
Anisotropy Versus Heterogeneity in Continental Solid Earth Electromagnetic Studies: Fundamental Response Characteristics and Implications for Physicochemical State (2005, methodology): “(1995), but using newer estimates of solubility and anisotropic defect diffusivities (Kohlstedt and Mackwell, 1998; Simpson, 2002; Bell et al., 2003; Zhao et al., 2004; Simpson and Tommasi, 2005).”
Mechanisms of hydrogen incorporation and diffusion in iron-bearing olivine (2006, result): “From our data (Fig. 1) and previous experimental studies (Mackwell and Kohlstedt 1990; Bai and Kohlstedt 1992, 1993; Zhao et al. 2004 ), it is clear that, in contradiction to the claims of Matveev et al. (2001, 2004), experimentally hydrated olivine buffered using orthopyroxene does show IR feature”