Comparisons of the core and mantle compositions of earth analogs from different terrestrial planet formation scenarios

1Jesse T.Gu,1Rebecca, A.Fischer,1Matthew C.Brennan,2Matthew S.Clement,3Seth A.Jacobson,4Nathan A.Kaib,5David P.O’Brien,6Sean N.Raymond
Icarus (in Press) Link to Article []
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA
2Earth and Planets Laboratory, Carnegie Institution for Science, Washington D.C., CO, USA
3Department of Earth and Environmental Sciences, Michigan State University, East Lansing, MI, USA
4HL Dodge Department of Physics and Astronomy, University of Oklahoma, Norman, OK, USA
5Planetary Science Institute, Tucson, AZ, USA
6Laboratoire d’Astrophysique de Bordeaux, Université de Bordeaux, CNRS, Bordeaux, France
Copyright Elsevier

The chemical compositions of Earth’s core and mantle provide insight into the processes that led to their formation. N-body simulations, on the other hand, generally do not contain chemical information, and seek to only reproduce the masses and orbits of the terrestrial planets. These simulations can be grouped into four potentially viable scenarios of Solar System formation (Classical, Annulus, Grand Tack, and Early Instability) for which we compile a total of 433 N-body simulations. We relate the outputs of these simulations to the chemistry of Earth’s core and mantle using a melt-scaling law combined with a multi-stage model of core formation. We find the compositions of Earth analogs to be largely governed by the fraction of equilibrating embryo cores (kcore_emb) and the initial embryo masses in N-body simulations, rather than the simulation type, where higher values of kcore_emb and larger initial embryo masses correspond to higher concentrations of Ni, Co, Mo, and W in Earth analog mantles and higher concentrations of Si and O in Earth analog cores. As a result, larger initial embryo masses require smaller values of kcore_emb to match Earth’s mantle composition. On the other hand, compositions of Earth analog cores are sensitive to the temperatures of equilibration and fO2 of accreting material. Simulation type may be important when considering magma ocean lifetimes, where Grand Tack simulations have the largest amounts of material accreted after the last giant impact. However, we cannot rule out any accretion scenarios or initial embryo masses due to the sensitivity of Earth’s mantle composition to different parameters and the stochastic nature of N-body simulations. We use our compiled simulations to explore the relationship between initial embryo masses and the melting history of Earth analogs, where the complex interplay between the timing between impacts, magma ocean lifetimes, and volatile delivery could affect the compositions of Earth analogs formed from different simulation types. Comparing the last embryo impacts experienced by Earth analogs to specific Moon-forming scenarios, we find the characteristics of the Moon-forming impact are dependent on the initial conditions in N-body simulations where larger initial embryo masses promote larger and slower Moon-forming impactors. Mars-sized initial embryos are most consistent with the canonical hit-and-run scenario onto a solid mantle. Our results suggest that constraining the fraction of equilibrating impactor core (kcore) and the initial embryo masses in N-body simulations could be significant for understanding both Earth’s accretion history and characteristics of the Moon-forming impact.


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