We report phonon densities of states (DOS) of iron measured by nuclear reso
nant inelastic x-ray scattering to 153 gigapascals and calculated from ab i
nitio theory. Qualitatively, they are in agreement, but the theory predicts
density at higher energies. From the DOS, we derive elastic and thermodyna
mic parameters of iron, including shear modulus, compressional and shear ve
locities, heat capacity, entropy, kinetic energy, zero-point energy, and De
bye temperature. In comparison to the compressional and shear velocities fr
om 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.