We report phonon densities of states (DOS) of iron measured by nuclear resonant inelastic x-ray scattering to 153 gigapascals and calculated from ab initio theory. Qualitatively, they are in agreement, but the theory predicts density at higher energies. From the DOS, we derive elastic and thermodynamic parameters of iron, including shear modulus, compressional and shear velocities, heat capacity, entropy, kinetic energy, zero-point energy, and Debye temperature. In comparison to the compressional and shear velocities from the preliminary reference Earth model (PREM) seismic model, our results suggest that Earth's inner core has a mean atomic number equal to or higher than pure iron, which is consistent with an iron-nickel alloy.
Phonon density of states of iron up to 153 gigapascals / Mao, Hk; J, Xu; Struzhkin, Vv; Shu, J; Hemley, Rj; Sturhahn, W; My, Hu; Alp, Ee; Vocadlo, L; Alfe, D; Price, Gd; Gillan, Mj; Schwoerer-Bohning, M; Hausermann, D; Eng, P; Shen, G; Giefers, H; Lubbers, R; Wortmann, G. - In: SCIENCE. - ISSN 0036-8075. - 292:5518(2001), pp. 914-916. [10.1126/science.1057670]
Phonon density of states of iron up to 153 gigapascals
Alfe D;
2001
Abstract
We report phonon densities of states (DOS) of iron measured by nuclear resonant inelastic x-ray scattering to 153 gigapascals and calculated from ab initio theory. Qualitatively, they are in agreement, but the theory predicts density at higher energies. From the DOS, we derive elastic and thermodynamic parameters of iron, including shear modulus, compressional and shear velocities, heat capacity, entropy, kinetic energy, zero-point energy, and Debye temperature. In comparison to the compressional and shear velocities from the preliminary reference Earth model (PREM) seismic model, our results suggest that Earth's inner core has a mean atomic number equal to or higher than pure iron, which is consistent with an iron-nickel alloy.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.