Accretion disk's magnetic field controlled the composition of the terrestrial planets
William F. McDonough (1,2), Takashi Yoshizaki (2) ((1) University, of Maryland, College Park, (2) Tohoku Univeristy)

TL;DR
This paper proposes a model linking the magnetic field strength in the protoplanetary disk to the compositional differences of terrestrial planets, explaining variations in core size and density based on their distance from the Sun.
Contribution
It introduces a novel model connecting magnetic field variations during disk accretion to planetary composition and core size distribution.
Findings
Core mass fractions decrease with distance from the Sun.
Planetary densities correlate with their heliocentric distance.
Magnetic field strength influences iron distribution and oxidation states.
Abstract
Chondrites, the building blocks of the terrestrial planets, have mass and atomic proportions of oxygen, iron, magnesium, and silicon totaling 90\% and variable Mg/Si (25\%), Fe/Si (factor of 2), and Fe/O (factor of 3). The Earth and terrestrial planets (Mercury, Venus, and Mars) are differentiated into three layers: a metallic core, a silicate shell (mantle and crust), and a volatile envelope of gases, ices, and, for the Earth, liquid water. Each layer has different dominant elements (e.g., increasing Fe content with depth and increasing oxygen content to the surface). What remains an unknown is to what degree did physical processes during nebular disk accretion versus those during post-nebular disk accretion (e.g., impact erosion) influence these final bulk compositions. Here we predict terrestrial planet compositions and show that their core mass fractions and…
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Taxonomy
TopicsAstro and Planetary Science · High-pressure geophysics and materials · Stellar, planetary, and galactic studies
