Temperature dependence of the elastic moduli of ringwoodite |
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| Institution: | 1. Department of Earth Sciences, Faculty of Science, Okayama University, Okayama, Okayama-ken 700-8530, Japan;2. Department of Earth Sciences, Ehime University, Matsuyama, Ehime-ken 790-8577, Japan;3. Institute for Study of the Earth''s Interior, Okayama University, Misasa, Tottori-ken 682-0193, Japan |
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| Abstract: | The elastic moduli of polycrystalline ringwoodite, (Mg0.91Fe0.09)2SiO4, were measured up to 470 K by means of the resonant sphere technique. The adiabatic bulk (KS) and shear (μ) moduli were found to be 185.1(2) and 118.22(6) GPa at room temperature, and the average slopes of dKS/dT and dμ/dT in the temperature range of the study were determined to be ?0.0193(9) and ?0.0148(3) GPa/K, respectively. Using these results, we estimate seismic wave velocity jumps for a pure olivine mantle model at 520 km depth. We find that the jump for the S-wave velocity is about 1.5 times larger than that for the P-wave velocity at this depth. This suggests that velocity jumps at the 520 km discontinuity are easier to detect using S-waves than P-waves. |
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