Hydrogen incorporation in olivine from 2–12 GPa

By J. Mosenfelder, N. Deligne, P. Asimow, G. Rossman. 2006

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Electrical conductivity anisotropy of dry and hydrous olivine at 8 GPa (2010, background): “178 Differences between the spectra of synthetically hydrated and natural olivine specimens 179 illustrate that hydrogen incorporation in olivine is a complex function of oxygen 180 fugacity and silica activity in addition to water fugacity (Mosenfelder et al., 2006).”
Quantitative absorbance spectroscopy with unpolarized light: Part II. Experimental evaluation and development of a protocol for quantitative analysis of mineral IR spectra (2008, unknown): “…against values calculated by Equation 7 using the integrated principal polarized absorbances, normalized to 1 cm thickness. literature (Fletcher 1892; Pancharatnam 1955; Ramachandran and Ramaseshan 1961; Szivessy 1928), there has been only limited adaptation of that knowledge to spectroscopy…”
Mechanisms of hydrogen incorporation and diffusion in iron-bearing olivine (2006, background): “More recently and using the improved calibration by Bell et al. (2003), Mosenfelder et al. (2006) reported higher hydrogen concentration around � 2,000 wt ppm H2 Oa t� 6 GPa and 1,000� C. The incorporation of hydrogen by this coupled proton-vacancy process occurs at � 10 -12 m 2 s -1 in olivine at”