Japan Geoscience Union Meeting 2018

Presentation information

[EE] Evening Poster

S (Solid Earth Sciences) » S-IT Science of the Earth's Interior & Tectonophysics

[S-IT19] Mineral-melt-fluid interaction and COHN volatile speciation in Earth and planetary

Sun. May 20, 2018 5:15 PM - 6:30 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Bjorn Mysen(Geophysical Laboratory, Carnegie Inst. Washington), Eiji Ohtani(Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University), Jun Tsuchiya(愛媛大学地球深部ダイナミクス研究センター)

[SIT19-P02] Fast water diffusion in silica glass

*Minami Kuroda1, Shogo Tachibana2, Naoya Sakamoto1, Hisayoshi Yurimoto1,3 (1.Hokkaido University, 2.University of Tokyo, 3.JAXA)

Keywords:water diffusion, silica glass, SIMS, diffusion mechanism

Water diffusion in silicate glass is a fundamental process controlling physical and chemical aspects of magmatism, but fundamental aspects of diffusion in silicate glass are not fully understood. In this study, we report one-order of magnitude faster water diffusion than that reported previously, discovered in diffusion experiments of deuterated water in silica glass, and discuss the water diffusion mechanism by considering diffusion pathways in silica glass.
A SiO2 glass sample and deuterated water (2H2O) were enclosed in a silica glass tube and heated in a furnace at 900-750 degree C for 1-20 hours with a water vapor pressure of 50 bar. Deuterated water was used to trace water diffusion at low water-concentration region (<10ppm), where background hydrogen signals obscure a diffusion profile of 1H2O. Diffusion profiles of 2H in samples were measured by secondary ion mass spectroscopy (SIMS: Cameca ims-6f) at Hokkaido University.
The 2H intensity rapidly decreases from rim to core of the sample as observed in the diffusion experiment with 1H2O (Kuroda et al., 2018). This profile shape can be explained by a concentration-dependent water diffusion model in silica glass (Kuroda et al., 2018), where water molecules diffuse through the diffusion pathways formed by breaking Si-O-Si bonds through a hydroxyl formation reaction (H2O + Si-O-Si = 2Si-OH). In this study, we found that the tail of deuterium profile extends further into the deep region of the sample. This suggests that a small fraction of deuterium-bearing species migrates with a faster diffusion rate and that the diffusion has weak concentration-dependence.
It has been known that noble gas diffusion through “free volume sites” in the dry silica glass structure, and that the activation energy and diffusivity depend on the atomic radius. The fast diffusion coefficient of water in the present study can also be explained by the relation between diffusivity and the size of diffusion species observed for noble gases. Therefore, we conclude that water molecules can diffuse through free volume sites, which provide faster diffusion pathways than those formed through a hydroxyl formation reaction. The concentration of free volume sites, estimated from the solubility of noble gases, is much higher than that observed deuterium concentration in a fast diffusion path in this study. This implies that free volume sites are not fully occupied by water molecules at water vapor pressure of 50 bar. The contribution of fast water diffusion may become larger under higher water vapor pressures, where the concentration of water molecules dissolved into free volume sites may increase as noble gases.