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The content and transport of fluid phases such as water into the deep Earth is of great importance not only to correlate seismological models of the planet’s interior with mineralogical models, but also for the understanding of the evolution of the solid Earth as well as the Earth’s atmosphere. This study reports on the influence of water on the structural and physical properties of olivine, which is known to be the main constituent of the upper mantle.

Compressibility and structural stability of two variably hydrated olivine samples. (FO 97 Fa 3 ) to 34 GPa by X-ray diffraction and Raman spectroscopy