Small Planetesimals in a Massive Disk Formed Mars

TL;DR

This paper investigates how the initial size of planetesimals and disk mass influence Mars's formation, suggesting small planetesimals in a massive disk best explain Mars's rapid formation and small size.

Contribution

It introduces a model linking initial planetesimal size and disk mass to Mars's final mass and formation timescale, considering collisional fragmentation and radial drift effects.

Findings

Small planetesimals (<10 km) in a massive disk (~0.1 solar mass) best explain Mars's rapid formation.

Radial drift of small fragments reduces solid surface density, affecting embryo growth.

Formation scenarios include small planetesimals in a massive disk or migration-influenced growth arrest.

Abstract

Mars is likely to be a planetary embryo formed through collisions with planetesimals, which can explain its small mass and rapid formation timescale obtained from 182Hf-182$W chronometry. In the classical theory of planet formation, the final embryo mass is determined only by the solid surface density. However, embryos can stir surrounding planetesimals, leading to fragmentation through erosive (cratering) collisions. We find that radial drift of small fragments can drastically reduce the solid surface density. On the other hand, embryo growth is accelerated by fragment accretion. Since collisional fragmentation efficiency depends on the initial size of planetesimals, the final embryo mass and its growth time are determined by the initial planetesimal size and disk surface density. We have investigated the effect of these two parameters on the mass of Mars and the predicted radiogenic excess of 182W in the martian mantle. Two scenarios can explain the rapid formation of small Mars: (i) it formed by accretion of small planetesimals in a massive disk or (ii) it formed from large planetesimals but its growth was arrested by the inward then outward migration of Jupiter. Taking into account all constraints, we conclude that Mars is likely to have formed in a massive disk of about ~ 0.1 solar mass from planetesimals smaller than ~ 10 km in radius. Such small planetesimal size cannot explain core accretion of Jupiter, suggesting that there may have been a heliocentric gradient in planetesimal size in the solar nebula.