SPH simulations find that disk mass and size after a Uranus-forming impact are robust to EOS choice while rock fraction is highly sensitive.
Monthly Notices of the Royal Astronomical Society , volume=
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SPH simulations produce a scaling relation showing giant impacts heat the core by ~3000 K on average with strong thermal stratification, allowing the core to reach an adiabatic state 290 Myr later consistent with geodynamo evidence.
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