An important testable prediction of dynamical instability models for the early evolution of the solar system is that Jupiter Trojans share a source population with the Kuiper Belt. Concrete evidence of this prediction remains elusive, as Kuiper Belt objects (KBOs) and Jupiter Trojans appear to have different surface compositions. We address the long-standing question of Trojan origin by finding a dynamical subpopulation in the Kuiper Belt with Trojan-like colors. Combining existing photometric data with our own surveys on Keck I and Palomar P200, we find that the low-perihelion (q < 30 au, a > 30 au) component of the Kuiper Belt has colors that bifurcate similarly to the Jupiter Trojans, unlike Centaurs (a < 30 au), which have redder, Kuiper Belt-like colors. To connect the Jupiter Trojans to the Kuiper Belt, we test whether the distinct Trojan-like colors of low-perihelion KBOs result from surface processing or are sourced from a specific population in the Kuiper Belt. By simulating the evolution of the Canada–France Ecliptic Plane Survey synthetic population of KBOs for four billion years, we find that differences in heating timescales cannot result in a significant depletion of very red low-perihelion KBOs as compared to the Centaurs. We find that the neutrally colored scattered disk objects (e > 0.6 KBOs) contribute more to the low-perihelion KBO population than to Centaurs, resulting in their different colors.
The Trojan-like Colors of Low-perihelion Kuiper Belt Objects
Abstract
Copyright and License
© 2024. The Author(s). Published by the American Astronomical Society.
Original content from this work may be used under the terms of the Creative Commons Attribution 4.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.
Acknowledgement
The authors would like to thank Konstantin Batygin, Ryleigh Davis, and Ian Wong for their helpful discussions. We thank the anonymous referees for insightful comments and suggestions that led to an improved manuscript. This work was supported by NASA Headquarters under the NASA Earth and Space Science Fellowship Program (grant 80NSSC21K0385).
Funding
This work was supported by NASA Headquarters under the NASA Earth and Space Science Fellowship Program (grant 80NSSC21K0385).
Facilities
Keck:I (LRIS), Hale (WASP) - .
Software References
Astropy (Astropy Collaboration et al. 2013, 2018, 2022), Photutils (Bradley et al. 2023).
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Additional details
- National Aeronautics and Space Administration
- NASA Earth and Space Science Fellowship 80NSSC21K0385
- Accepted
-
2024-07-29Accepted
- Available
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2024-09-03Published
- Caltech groups
- Division of Geological and Planetary Sciences
- Publication Status
- Published