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Sound velocities for hexagonally close‐packed iron compressed hydrostatically to 136 GPa from phonon density of states
Author(s) -
Gleason A. E.,
Mao W. L.,
Zhao J. Y.
Publication year - 2013
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/grl.50588
Subject(s) - hydrostatic equilibrium , inner core , shear (geology) , adiabatic process , debye model , anisotropy , bulk modulus , scattering , equation of state , physics , materials science , condensed matter physics , thermodynamics , optics , geophysics , composite material , quantum mechanics
The phonon density of states of pure iron ( 57 Fe) was measured under hydrostatic conditions using nuclear resonant inelastic X‐ray scattering (NRIXS) at pressures up to 136 GPa. Extracting shear ( V s ) and compressional ( V p ) wave speeds from the Debye velocity and equation of state, we find the hydrostatic shear wave speed trend above previously collected NRIXS data under nonhydrostatic conditions by roughly 5%–6% in the measured pressure range. Using the Birch Murnaghan finite strain approach to fit pressure‐dependent adiabatic bulk and shear moduli, we extrapolated our velocities to inner Earth core densities and found that our shear wave speeds are 3% higher than those in previous studies. Our results on pure iron provide a more accurate and precise baseline to which added complications (e.g., Ni concentration, inclusion of various light elements, and temperature effects) can be considered when comparing experimental elasticity measurements to inner core seismic data.