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Collisions Between Gravity-Dominated Bodies: 1. Outcome Regimes and Scaling Laws

2 Pith papers cite this work. Polarity classification is still indexing.

2 Pith papers citing it
abstract

Collisions are the core agent of planet formation. In this work, we derive an analytic description of the dynamical outcome for any collision between gravity-dominated bodies. We conduct high-resolution simulations of collisions between planetesimals; the results are used to isolate the effects of different impact parameters on collision outcome. During growth from planetesimals to planets, collision outcomes span multiple regimes: cratering, merging, disruption, super-catastrophic disruption, and hit-and-run events. We derive equations (scaling laws) to demarcate the transition between collision regimes and to describe the size and velocity distributions of the post-collision bodies. The scaling laws are used to calculate maps of collision outcomes as a function of mass ratio, impact angle, and impact velocity, and we discuss the implications of the probability of each collision regime during planet formation. The analytic collision model presented in this work will significantly improve the physics of collisions in numerical simulations of planet formation and collisional evolution. (abstract abridged)

fields

astro-ph.EP 2

years

2026 2

verdicts

UNVERDICTED 2

representative citing papers

Can giant impacts be directly detected in other star systems?

astro-ph.EP · 2026-06-24 · unverdicted · novelty 5.0

Simulations of giant impacts between 0.2-4 Earth-mass planets yield post-impact luminosities of 5e-5 to 0.1 L_sun cooling over 1-2000 days, predicting 0-14 detections in Gaia DR4 and a comparable number in LSST.

citing papers explorer

Showing 2 of 2 citing papers.

  • Thermal and rotational effects of giant impacts during terrestrial planet accretion astro-ph.EP · 2026-06-22 · unverdicted · none · ref 191 · internal anchor

    Hydrodynamical simulations of giant impacts find lower post-impact CMB pressures due to thermal and rotational effects, common full mantle melting, and conditions favoring metal-silicate equilibration near the CMB.

  • Can giant impacts be directly detected in other star systems? astro-ph.EP · 2026-06-24 · unverdicted · none · ref 52 · internal anchor

    Simulations of giant impacts between 0.2-4 Earth-mass planets yield post-impact luminosities of 5e-5 to 0.1 L_sun cooling over 1-2000 days, predicting 0-14 detections in Gaia DR4 and a comparable number in LSST.