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Table 1

Three catalogues used in this study (top) and catalogues used in LS12 for gravity-dominated bodies (bottom).

Reference SPH algorithm Nsim Mt/M Mp/Mt Composition EoS
Denman et al. (2020) GADGET() 122 3.27, 6.26, 10.5 0.04-0.92 Fe, silicate and H (gas) MANEOS
Gabriel et al. (2020) SPHLATCH(⋆) 1401 6 × 10−3–0.9 0.1-0.7 Fe, quartz and H20 not specified
Timpe et al. (2020) Gasoline(•) 10662 0.05-1.8 0.1-1 Fe and granite Tillotson
Burger et al. (2020) miluphcuda(∗) 9980 6 × 10−4–1.8 7 × 10−5–1 Fe, silicate and H20 Tillotson
Crespi et al. (2021) miluphcuda(∗) 858 1.6 × 10−4–1.8 0.1, 0.5, 1 80-90% basalt, 10-20% H20 Tillotson
Winter et al. (2023) miluphcuda(∗) 10164 2.6 × 10−4–1.9 0.05-1 Fe, silicate and H20 Tillotson

Benz et al. (2007) generic SPH(‡) 17 0.1375 1/10, 1/6, 1/5 33% Fe, 66% dunite ANEOS
Marcus et al. (2009) GADGET(†) ~60 1, 5, 10 1/4, 1/2, 3/4 33% Fe, 66% fosterite MANEOS
Marcus et al. (2010) GADGET(†) ~100 0.5-5 1/4, 1/2, 1 50% serpentine, 50% H20 MANEOS

Notes. The columns show (from left to right) the reference paper in which the dataset is presented, SPH algorithm used to perform the simulations, total number of simulations (Nsim), sampled masses of the target body in Earth mass (Mt/M), mass of the projectile scaled by the target mass (Mp/Mt), composition of the colliding bodies, and the equation of state (EoS) used in the simulations. In particular, for the EoS column, the following labels are used: Tillotson for the nonlinear equations of state formulated by Tillotson (1962), ANEOS for the set of analytical equations of state developed by Thompson & Lauson (1972), and MANEOS for the set of analytical equations of state that also account for the energetic effects of the formation of molecular clusters, as developed by Melosh (2007) based on the work of Thompson & Lauson (1972). (†)Springel (2005). (⋆)Reufer (2011) and Emsenhuber et al. (2018). (•)Wadsley et al. (2004), Chau et al. (2018) and Reinhardt et al. (2020). (‡)Monaghan (1992). (∗) Schäfer et al. (2016) and Schäfer et al. (2020).

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