Abstract:The Earth’s outer core is mainly composed of Fe and Ni. The compositional stratification and geodynamo of the Earth’s core are closely correlated with the transport properties of the fluid in the Earth core. We selected the typical FeNi fluid, and systemically calculated its diffusion coefficient and viscosity under Earth’s core condition by quantum molecular dynamics simulation. The diffusion coefficients and viscosity are almost constant along the core adiabatic curve. The self-diffusion coefficients of Ni a… Show more
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