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- W1978339998 abstract "Abstract We systematically measured oxygen self‐diffusion coefficients ( D O ) in forsterite along b crystallographic axis at a pressure of 8 GPa and temperatures of 1600–1800 K, over a wide range of water content ( C H2O ) from <1 up to ~800 weight ppm. The experimental results suggest that D O ∝ ( C H2O ) 0.05±0.06 ≈ ( C H2O ) 0 . Thus, water has no significant effect on oxygen self‐diffusion rate in forsterite. Since the C H2O dependence of silicon self‐diffusion rate is also very small, the effect of water on olivine rheology is not significant by assuming the diffusion controlled creep mechanism." @default.
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- W1978339998 date "2014-10-01" @default.
- W1978339998 modified "2023-10-06" @default.
- W1978339998 title "No effect of water on oxygen self-diffusion rate in forsterite" @default.
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- W1978339998 doi "https://doi.org/10.1002/2014jb011141" @default.
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