Phonon density of states of iron up to 153 gigapascals

被引:242
作者
Mao, HK
Xu, J
Struzhkin, VV
Shu, J
Hemley, RJ
Sturhahn, W
Hu, MY
Alp, EE
Vocadlo, L
Alfè, D
Price, GD
Gillan, MJ
Schwoerer-Böhning, M
Häusermann, D
Eng, P
Shen, G
Giefers, H
Lübbers, R
Wortmann, G
机构
[1] Carnegie Inst Washington, Geophys Lab, Washington, DC 20015 USA
[2] Carnegie Inst Washington, Ctr High Pressure Res, Washington, DC 20015 USA
[3] Adv Photon Source, Argonne, IL 60439 USA
[4] UCL, London WC1E 6BT, England
[5] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[6] Univ Paderborn, Fachbereich Phys, D-33095 Paderborn, Germany
[7] High Pressure Collaborat Access Team, Adv Photon Source, Argonne, IL 60439 USA
关键词
D O I
10.1126/science.1057670
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
引用
收藏
页码:914 / 916
页数:3
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