Equation of state tables used in the paper: "Exploring the Catastrophic Regime: Thermodynamics and Disintegration in Head-On Planetary Collisions"

<p>The EoS (Equation of State) tables for iron and forsterite used in the paper "<span>Exploring the Catastrophic Regime: Thermodynamics and Disintegration</span><br><span>in Head-On Planetary Collisions</span>" are available here for use.</p> <p>These tables can be directly integrated into the SPH (Smoothed Particle Hydrodynamics) code <a href="https://swift.strw.leidenuniv.nl/">SWIFT</a> to conduct simulations of planetary giant impacts.</p> <p>The tables were generated using the GitHub repository maintained by Sarah T. Stewart, specifically for <a href="https://github.com/ststewart/aneos-iron-2020">iron</a> and <a href="https://github.com/ststewart/aneos-forsterite-2019">forsterite</a>.</p> <p>All tables were created with the tension regions of the materials removed.</p> <p>Table "ANEOS_iron_S20_100gcc_denseTgrid_NOTension.txt" was generated with denser grid at temperate range 1e5 to 1e6 to using for impacts with target mass above 10 Earth mass.</p> <p>Table "ANEOS_forsterite_S19_80gcc_NOTension.txt" was generated with dense grid in both rho and temperate dimention.</p> <p>"ANEOS_iron_S20_100gcc_denseTgrid_NOTension.txt" and "ANEOS_forsterite_S19_80gcc_NOTension.txt" were generated to deal with extreme cases that impact speeds and target masses are very high.&nbsp;</p> <p>Most of the simulations were run with "ANEOS_forsterite_S19.txt" and "ANEOS_iron_S20.txt".</p> <p>&nbsp;</p>