Melting of iron under Earth's core conditions from diffusion Monte Carlo free energy calculations.

Abstract

The temperature of Earth's core is a parameter of critical importance to model the thermal structure of Earth. Since the core is mainly made of iron, with a solid liquid boundary (the inner core boundary) at 1220 km from the center of the Earth, the melting temperature of iron at the pressure of the ICB provides constraints on the temperature of the core… (More)

Topics

3 Figures and Tables

Slides referencing similar topics