A unified N-body and metal-silicate equilibration model demonstrates that Earth and Mars analogs accrete from different redox reservoirs in a narrow ring planetesimal scenario, resulting in distinct core sizes and mantle compositions due to varying impact conditions.
Episodic planetesimal disruptions triggered by dissipation of gas disk
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abstract
Catastrophic disruptions of planetesimals occur in high-velocity collisions. Radioisotope dating of planetesimal disruption events recorded in meteorites confirms frequent catastrophic collisions in the first 10 Myr of the Solar System, reflecting a violent environment of the time. However, the nebula gas can damp the eccentricity of planetesimals and suppress the frequency of planetesimal collisions. Strong dynamical mechanisms that excited the protoplanetary disk are required. Here we show that the sweeping secular resonances of Jupiter and Saturn induced by the nebular gas dissipation, together with the mean motion resonances of Jupiter, can trigger a large number of catastrophic collisions, which occur episodically when the secular resonances are at 2-3 astronomical units and continue thereafter. After the gas dissipation completes, catastrophic collisions decrease in frequency, with scattering by planetary embryos becoming the major driving force of the collisions. Our results suggest that the violent environment excited by secular and mean motion resonances can be ubiquitous in protoplanetary disks during nebula dissipation.
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astro-ph.EP 1years
2026 1verdicts
UNVERDICTED 1representative citing papers
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Coupling dynamical accretion and chemical differentiation: a unified framework for Earth-Mars diversity
A unified N-body and metal-silicate equilibration model demonstrates that Earth and Mars analogs accrete from different redox reservoirs in a narrow ring planetesimal scenario, resulting in distinct core sizes and mantle compositions due to varying impact conditions.