1. Elasticity and sound velocity at high pressures: Geophysics and materials science At ambient pressure, we have determined the elasticity of wadsleyite (b-Mg2SiO4) as a function of water content, and the elasticity of two hydrous olivine compositions. At high pressures, we have studied the elasticity of hydrous forsterite and hydrous Fe-free and Fe-bearing wadsleyite. One surprising result is the existence of a velocity crossover in forsterite whereby compressional and shear velocities of the hydrous phase exceed those of the anhydrous phase at high pressure. We have used our results to model the effects of H on the seismic velocity structure of Earth’s mantle. This work was carried out in collaboration with S. Jacobsen’s group (Northwestern) and J. Smyth (Colorado). Other recent projects include examination of the single-crystal elasticity of MgF2, SiO2 (stishovite), AlOOH (diaspore), ettringite, zoisite, alunite, and brucite. There are many further opportunities for new research projects and further technique development in this area. Selected References: Jiang, F., G. D. Gwanmesia, T. I. Dyuzheva, and T. S. Duffy, Elasticity of stishovite and acoustic mode softening under high pressure by Brillouin scattering, Physics of the Earth and Planetary Interiors, 172, 235-240, 2009. Speziale, S., F. Jiang, Z. Mao, P. J. M. Monteiro, H.-R. Wenk, T. S. Duffy, and F. Schilling, Single-crystal elastic constants of natural ettringite, Cement and Concrete Research, 38, 885-889, 2008
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