Dynamical orbital evolution of asteroids and planetesimals across distinct chemical reservoirs due to accretion growth of planets in the early solar system

TL;DR

This study uses N-body simulations to explore how early planetary growth affected asteroid orbital dynamics and the mixing of different spectral types, shedding light on the origin of meteorite diversity.

Contribution

It introduces a new simulation framework to analyze the orbital evolution of asteroids during planet formation and its impact on spectral type distribution.

Findings

Initial planetary eccentricities influence asteroid orbital mixing.

Massive Jupiter and Saturn significantly affect planetesimal eccentricities.

Accretion timescales correlate with meteorite parent body formation.

Abstract

N-body numerical simulations code for the orbital motion of asteroids/planetesimals within the asteroid belt under the gravitational influence of the sun and the accreting planets has been developed. The aim is to make qualitative, and to an extent a semi-quantitative argument, regarding the possible extent of radial mixing and homogenization of planetesimal reservoirs of the two observed distinct spectral types , viz., the S-type and C-type, across the heliocentric distances due to their dynamical orbital evolution, thereby, eventually leading to the possible accretion of asteroids having chemically diverse constituents. The spectral S-type and C-type asteroids are broadly considered as the parent bodies of the two observed major meteoritic dichotomy classes, namely, the non-carbonaceous (NC) and carbonaceous (CC) meteorites, respectively. The present analysis is performed to understand the evolution of the observed dichotomy and its implications due to the nebula and early planetary processes during the initial 10 Myrs (Million years). The homogenization across the two classes is studied in context to the accretion timescales of the planetesimals with respect to the half-life of the potent planetary heat source, 26Al. The accretion over a timescale of ~1.5 Myr. possibly resulted in the planetary-scale differentiation of planetesimals to produce CC and NC achondrites and iron meteorite parent bodies, whereas, the prolonged accretion over a timescale of 2-5 Myrs. resulted in the formation of CC and NC chondrites. Our simulation results indicate a significant role of the initial eccentricities and the masses of the accreting giant planets, specifically, Jupiter and Saturn, in triggering the eccentricity churning of the planetesimals across the radial distances......