Tidal Evolution of Kepler lower-mass Planets

TL;DR

This study investigates how tidal interactions influence the orbital evolution of Kepler's low-mass planets, revealing statistical patterns and potential formation scenarios consistent with observations.

Contribution

It provides a simulation-based analysis of tidal effects on low-mass planets' orbits, exploring parameter influences and proposing formation mechanisms.

Findings

Semi-major axis increases with initial semi-major axis and eccentricity.

Simulation results align with observations for certain initial conditions.

Other parameters have minor effects on final orbital distribution.

Abstract

The planets with a radius $<$ 4 $R$$_\oplus$ observed by the Kepler mission exhibit a unique feature, and propose a challenge for current planetary formation models. The tidal effect between a planet and its host star plays an essential role in reconfiguring the final orbits of the short-period planets. In this work, based on various initial Rayleigh distributions of the orbital elements, the final semi-major axis distributions of the planets with a radius $<$ 4 $R_\oplus$ after suffering tidal evolutions are investigated. Our simulations have qualitatively revealed some statistical properties: the semi-major axis and its peak value all increase with the increase of the initial semi-major axis and eccentricity. For the case that the initial mean semi-major axis is less than 0.1 au and the mean eccentricity is larger than 0.25, the results of numerical simulation are approximately consistent with the observation. In addition, the effects of other parameters, such as the tidal dissipation coefficient, stellar mass and planetary mass, etc., on the final semi-major axis distribution after tidal evolution are all relatively small. Based on the simulation results, we have tried to find some clues for the formation mechanism of low-mass planets. We speculate that these low-mass planets probably form in the far place of protoplanetary disk with a moderate eccentricity via the type I migration, and it is also possible to form in situ.