Abstract

Aims. The goal of this research is to study how the fragmentation of planetary embryos can affect the physical and dynamical properties of terrestrial planets around solar-type stars. Our study focuses on the formation and evolution of planets and water delivery in the habitable zone (HZ). We distinguish class A and class B HZ planets, which have an accretion seed initially located inside and beyond the snow line, respectively. Methods. We developed an N-body integrator that incorporates fragmentation and hit-and-run collisions, which is called D3 N-body code. From this, we performed 46 numerical simulations of planetary accretion in systems that host two gaseous giants similar to Jupiter and Saturn. We compared two sets of 23 N-body simulations, one of which includes a realistic collisional treatment and the other one models all impacts as perfect mergers. Results. The final masses of the HZ planets formed in runs with fragmentation are about 15–20% lower than those obtained without fragmentation. As for the class A HZ planets, those formed in simulations without fragmentation experience very significant increases in mass with respect to their initial values, while the growth of those produced in runs with fragmentation is less relevant. We remark that the fragments play a secondary role in the masses of the class A HZ planets, providing less than 30% of their final values. In runs without fragmentation, the final fraction of water of the class A HZ planets keeps the initial value since they do not accrete water-rich embryos. In runs with fragmentation, the final fraction of water of such planets strongly depends on the model used to distribute the water after each collision. The class B HZ planets do not show significant differences concerning their final water contents in runs with and without fragmentation. From this, we find that the collisional fragmentation is not a barrier to the survival of water worlds in the HZ.

Highlights

  • Understanding terrestrial planet formation is an ongoing challenge in planetary sciences

  • Based on the work developed by LS12. In that work he studied the final stage of terrestrial planet formation with N-body simulations, concluding that hit-and-run collisions are a common outcome of two colliding big bodies

  • According to that observed in the bottom and right panel of Fig. 8 through violet boxes, the initial masses of the class B habitable zone (HZ) planets produced in runs without fragmentation represent more than 50% of their final masses

Read more

Summary

Introduction

Understanding terrestrial planet formation is an ongoing challenge in planetary sciences. Implemented a refined collisional algorithm into MERCURY based on the work developed by LS12 In that work he studied the final stage of terrestrial planet formation with N-body simulations, concluding that hit-and-run collisions are a common outcome of two colliding big bodies. Thanks to the improvements in the collisional model proposed by LS12, we decided to move away from the perfect merging model and developed the D3 N-body code with a more realistic treatment of collisions between planetary embryos This improvement allows us to carry out a detailed study about the final composition of the planets formed. We present the different regimes implemented in the numerical integrator

Overview
Collisional model: different type of collisions
Collisional algorithm
Protoplanetary disk: model
Findings
Discussion and conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call