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Some Experimental Constraints on the Role of Hydrogen in Oxygen and Hydrogen Diffusion and Al-Si Interdiffusion in Silicates

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Diffusion, Atomic Ordering, and Mass Transport

Part of the book series: Advances in Physical Geochemistry ((PHYSICAL GEOCHE,volume 8))

Abstract

The importance of aqueous fluid in catalyzing mineral reactions and in modifying the physico-chemical properties of minerals has long been recognized. For example, water enhances mineral reactivity by promoting solution-reprecipitation processes (e.g., Matthews et al, 1983). In this study, we are principally concerned with the role of aqueous fluid in modifying solid-state intra-crystalline processes of geological importance, and in particular diffusion. An understanding of the mediating role of water in diffusion processes in minerals is central to the interpretation of petrological and geochemical (e.g., stable isotopic) data relating to thermometry, barometry, and fluid-rock interactions in slowly cooling metamorphic, igneous, and hydrothermal rocks in the Earth’s crust. In addition, the “hydrolytic weakening” effect of water on the strength of quartz discovered by Griggs over 20 years ago (Griggs and Blacic, 1965; Griggs, 1967) may be related to diffusion-controlled processes, although these processes are still controversial (e.g., Kronenberg et al, 1986). Mineral solution in aqueous fluids (e.g., Eugster, 1986) will be considered in detail in this chapter only insofar as it might affect the interpretation of experimental results presented.

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Graham, C.M., Elphick, S.C. (1991). Some Experimental Constraints on the Role of Hydrogen in Oxygen and Hydrogen Diffusion and Al-Si Interdiffusion in Silicates. In: Ganguly, J. (eds) Diffusion, Atomic Ordering, and Mass Transport. Advances in Physical Geochemistry, vol 8. Springer, New York, NY. https://doi.org/10.1007/978-1-4613-9019-0_8

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  • DOI: https://doi.org/10.1007/978-1-4613-9019-0_8

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