TY - JOUR
T1 - Temperature dependence of elastic moduli of β-(Mg, Fe )2SiO4
AU - Mayama, Norihito
AU - Suzuki, Isao
AU - Saito, Toshiaki
AU - Ohno, Ichiro
AU - Katsura, Tomoo
AU - Yoneda, Akira
N1 - Copyright:
Copyright 2018 Elsevier B.V., All rights reserved.
PY - 2004/2/28
Y1 - 2004/2/28
N2 - The elastic moduli of polycrystalline wadsleyite, β(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 165.72(6) and 105.43(2) GPa at room temperature. The average slopes (dKs/dT and dμ/dT) in the range were determined to be the -0.0175(3) and -0.0159(1) GPa/K. We estimated that the P-, S-wave velocity and density jumps for the α- to β-phase transformation at the 410-km depth condition were 9.5, 11.2 and 5.4%, respectively. These results suggest that the olivine component at the depth should be 52 and 42 volume % for P- and S-waves.
AB - The elastic moduli of polycrystalline wadsleyite, β(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 165.72(6) and 105.43(2) GPa at room temperature. The average slopes (dKs/dT and dμ/dT) in the range were determined to be the -0.0175(3) and -0.0159(1) GPa/K. We estimated that the P-, S-wave velocity and density jumps for the α- to β-phase transformation at the 410-km depth condition were 9.5, 11.2 and 5.4%, respectively. These results suggest that the olivine component at the depth should be 52 and 42 volume % for P- and S-waves.
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U2 - 10.1029/2003GL019247
DO - 10.1029/2003GL019247
M3 - Article
AN - SCOPUS:2542449036
SN - 0094-8276
VL - 31
SP - L04612 1-4
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 4
ER -