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The first 200 kyr of the Solar System: making the planetary material diversity

Published online by Cambridge University Press:  13 January 2020

Francesco C. Pignatale
Affiliation:
Muséum national d’Histoire naturelle, UMR 7590, CP52, 57 rue Cuvier, 75005, Paris, France, email: pignatale@ipgp.fr Institut de Physique du Globe de Paris (IPGP), 1 rue Jussieu, 75005, Paris, France
Sébastien Charnoz
Affiliation:
Institut de Physique du Globe de Paris (IPGP), 1 rue Jussieu, 75005, Paris, France
Marc Chaussidon
Affiliation:
Institut de Physique du Globe de Paris (IPGP), 1 rue Jussieu, 75005, Paris, France
Emmanuel Jacquet
Affiliation:
Muséum national d’Histoire naturelle, UMR 7590, CP52, 57 rue Cuvier, 75005, Paris, France, email: pignatale@ipgp.fr
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Abstract

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Chondrites are made of a mixture of solids formed at high and low temperatures. This heterogeneity was thought to be produced by large scale transport processes in the Sun’s isolated accretion disk. However, mounting evidences suggest that refractory inclusions in chondrites were produced together with the disk formation.

We present numerical simulations of the formation and transport of rocky materials during the collapse of the Solar Nebula’s parent cloud and the consequent disk assembling.

We find that the interplay between the cloud collapse, the dynamics of gas and dust and thermal processing of different species in the disk, results in a local mixing of solids with different thermal histories. Our simulations return an heterogeneous distribution of refractory material with higher concentration in the outer disk. This refractory material has a short formation timescales, during the first tens of kyr of the Sun (class 0-I). Our results open new frontiers into the origin of the compositional diversity of chondrites.

Type
Contributed Papers
Copyright
© International Astronomical Union 2020 

References

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