Water diffusion in synthetic iron-free forsterite

By S. Demouchy, S. Mackwell. 2003

154 citations recorded by the source corpus.

Subfields: Biomaterials, Geophysics, Renewable Energy, Sustainability and the Environment

View Paper: https://www.semanticscholar.org/paper/98e176a210d8ad67049353090c3154a2e1900d9b

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In Biomaterials

1. S. Demouchy
2. S. Mackwell

In Geophysics

1. S. Demouchy
2. S. Mackwell
3. P. Asimow
4. J. Mosenfelder

In Renewable Energy, Sustainability and the Environment

1. S. Demouchy
2. S. Mackwell

Citations in the corpus

• Mechanisms of hydrogen incorporation and diffusion in iron-bearing olivine (2006, methodology): “The diffusivity of hydrogen in olivine can be determined from the plots of water content versus distance across the samples, as in previous studies on olivine and forsterite (Mackwell and Kohlstedt 1990; Kohlstedt and Mackwell 1998, 1999; Demouchy and Mackwell 2003 ).”
• 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).”