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GW Ori: circumtriple rings and planets (2109.09776v1)

Published 20 Sep 2021 in astro-ph.EP and astro-ph.SR

Abstract: GW Ori is a hierarchical triple star system with a misaligned circumtriple protoplanetary disc. Recent ALMA observations have identified three dust rings with a prominent gap at $100\, \rm au$ and misalignments between each of the rings. A break in the gas disc may be driven either by the torque from the triple star system or a planet that is massive enough to carve a gap in the disc. Once the disc is broken, the rings nodally precess on different timescales and become misaligned. We investigate the origins of the dust rings by means of $N$-body integrations and 3-dimensional hydrodynamic simulations. We find that for observationally-motivated parameters of protoplanetary discs, the disc does not break due to the torque from the star system. We suggest that the presence of a massive planet (or planets) in the disc separates the inner and outer disc. We conclude that the disc breaking in GW Ori is likely caused by undetected planets -- the first planet(s) in a circumtriple orbit.

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Summary

  • The paper reveals that planetary influence likely explains the misaligned circumtriple dust rings observed in GW Ori.
  • The study employs ALMA data and advanced N-body and hydrodynamic simulations to test disc breaking mechanisms.
  • Results highlight that gravitational torque from the triple stars is insufficient, pointing to one or more massive planets as the cause.

Analysis of "GW Ori: Circumtriple Rings and Planets"

In the paper "GW Ori: circumtriple rings and planets," Smallwood et al. examine the hierarchical triple star system GW Ori, which is encircled by a misaligned circumtriple protoplanetary disc. The paper utilizes recent ALMA observations that have delineated three distinct dust rings with a notable gap located at approximately 100 AU from the stars. There is also a detected misalignment amongst the rings themselves.

Key Findings

The research explores potential origins of these rings through both N-body integrations and three-dimensional hydrodynamic simulations. Two primary hypotheses were considered for the formation of the observed disc structures:

  1. Stellar Torque Hypothesis: The first hypothesis suggests that disc breaking is driven by the gravitational torque exerted by the misaligned triple star system. This process, if significant enough, could cause the circumtriple disc to break and eventually form distinct planes that can precess at different rates.
  2. Planetary Influence Hypothesis: The second hypothesis posits that an undetected planet, or possibly multiple planets, within the disc could be responsible for the pronounced gap and misalignments. Such a planet would need to have sufficient mass to carve a gap in the disc, leading to a broken configuration.

The paper finds that given the parameters typically expected for protoplanetary discs, the torque from the stellar system alone does not lead to disc breaking. Consequently, the analysis gravitates towards the planetary hypothesis. The authors conclude that the observed disc breaking in GW Ori is more likely due to the influence of one or more planets within the system.

Observational Evidence and Simulations

In supporting their conclusion, Smallwood et al. use comprehensive simulations to demonstrate the dynamical evolution of the GW Ori system. The paper details that the torque from the triple star system was insufficient to align with the observed disc configuration. However, the inclusion of a massive planet in the simulation yielded results consistent with observed data, thereby lending credence to the planetary hypothesis.

Implications and Future Work

The discovery of planets capable of destabilizing and misaligning protoplanetary discs in hierarchical stellar systems has significant implications for our understanding of planet formation in complex gravitational fields. This paper proposes the presence of the first circumtriple planet(s) in GW Ori, making it an interesting target for further observational campaigns aimed at directly detecting such planetary bodies.

Future work should focus on the detection of these planets through direct imaging or other indirect methods such as radial velocities or transit observations. Additionally, expanding the scope of simulations to explore a variety of planet masses, disc viscosities, and initial conditions will fortify the understanding of disc-planet interactions in circumtriple settings.

Overall, the paper importantly contributes to the niche field of circumtriple systems by coupling observational data with detailed theoretical models, advancing our comprehension of disc dynamics and planet formation in multi-star environments.

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