Thermal and electrical conductivity of solid iron and iron-silicon mixtures at Earth's core conditions

- Thermal conductivity of inner core 4 times higher than those in use in previous core studies.
- Electrical conductivity 3 times higher than those in use in previous core studies.
- Inner core not thermally convecting.
- Magnetic diffusion time increased to 10 kyr, possible stabilisation of geodynamo and reduction of the frequency of reversals.

We report on the thermal and electrical conductivities of solid iron and iron-silicon mixtures (Fe0.92Si0.08 and Fe0.93Si0.07), representative of the composition of the Earth's solid inner core at the relevant pressure-temperature conditions, obtained from density functional theory calculations with the Kubo-Greenwood formulation. We find thermal conductivities k=232(237) Wm−1K−1, and electrical conductivities σ=1.5(1.6)×106Ω−1m−1 at the top of the inner core (centre of the Earth). These values are respectively about 45-56% and 18-25% higher than the corresponding conductivities in the liquid outer core. The higher conductivities are due to the solid structure and to the lower concentration of light impurities. These values are much higher than those in use for previous inner core studies, k by a factor of four and σ by a factor of three. The high thermal conductivity means that heat leaks out by conduction almost as quickly as the inner core forms, making thermal convection unlikely. The high electrical conductivity increases the magnetic decay time of the inner core by a factor of more than three, lengthening the magnetic diffusion time to 10 kyr and making it more likely that the inner core stabilises the geodynamo and reduces the frequency of reversals.

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