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

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arxiv 1106.6084 v3 pith:FBKHLWKN submitted 2011-06-29 astro-ph.EP

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

classification astro-ph.EP
keywords collisioncollisionsbodiesformationimpactlawsoutcomeplanet
verification ladder T0 review T1 audit T2 compute T3 formal T4 reserved
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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)

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Cited by 3 Pith papers

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  1. Thermal and rotational effects of giant impacts during terrestrial planet accretion

    astro-ph.EP 2026-06 unverdicted novelty 6.0

    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.

  2. Can giant impacts be directly detected in other star systems?

    astro-ph.EP 2026-06 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.

  3. The Maximum Density of a Collisionally-Produced Planet is A Function of its Mass and Orbital Period

    astro-ph.EP 2026-06 unverdicted novelty 4.0

    Analysis of SPH simulations and collision velocity models predicts that collisionally-produced super-Mercuries have higher densities at low mass and short period, identifying GJ 367b as the strongest observed candidate.