First-principles molecular-dynamics simulations based on density-functional
theory and the projector augmented wave (PAW) technique have been used to
study the structural and dynamical properties of liquid iron under Earth's
core conditions. As evidence for the accuracy of the techniques, we present
PAW results for a range of solid-state properties of low- and high-pressur
e iron, and compare them with experimental values and the results of other
first-principles calculations. In the liquid-state simulations, we address
particular effort to the study of finite-size effects, Brillouin-zone sampl
ing, and other sources of technical error. Results for the radial distribut
ion function, the diffusion coefficient, and the shear viscosity are presen
ted for a wide range of thermodynamic states relevant to the Earth's core.
Throughout this range, liquid iron is a close-packed simple liquid with a d
iffusion coefficient and viscosity similar to those of typical simple liqui
ds under ambient conditions.