Site-specific hydrogen diffusion rates in forsterite
Synthetic hydroxylated titanium-bearing and undoped MgO-buffered forsterite crystals were heated at atmospheric pressure in air at temperatures from 800 to 1200°C to determine hydrogen diffusion as a function of the type of point-defect mechanism by whic
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|Source:||Earth and Planetary Science Letters|
|01_Padron-Navarta_Site-specific_hydrogen_2014.pdf||1.33 MB||Adobe PDF||Request a copy|
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