Analysis of terrestrial planet formation by the Grand Tack model: System architecture and tack location
R. Brasser, S. Matsumura, S. Ida, S. J. Mojzsis, S. C. Werner

TL;DR
This study evaluates the Grand Tack model of terrestrial planet formation through extensive N-body simulations, finding that a tack location at 2 AU better explains the observed inner solar system than 1.5 AU, especially under oligarchic initial conditions.
Contribution
It provides a comprehensive analysis of how different tack locations and initial conditions affect terrestrial planet formation, favoring a farther-out tack at 2 AU for better alignment with observations.
Findings
A tack at 1.5 AU is inconsistent with the observed planet distribution.
A tack at 2 AU better reproduces the mass and orbital architecture of terrestrial planets.
Oligarchic initial conditions more accurately match the solar system's features.
Abstract
The Grand Tack model of terrestrial planet formation has emerged in recent years as the premier scenario used to account for several observed features of the inner solar system. It relies on early migration of the giant planets to gravitationally sculpt and mix the planetesimal disc down to ~1 AU, after which the terrestrial planets accrete from material left in a narrow circum-solar annulus. Here we have investigated how the model fares under a range of initial conditions and migration course-change (`tack') locations. We have run a large number of N-body simulations with a tack location of 1.5 AU and 2 AU and tested initial conditions using equal mass planetary embryos and a semi-analytical approach to oligarchic growth. We make use of a recent model of the protosolar disc that takes account of viscous heating, include the full effect of type 1 migration, and employ a realistic…
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