Abstract
Observations show that 100 km class Kuiper Belt objects (KBOs) can be divided into (at least) two color groups, red (R; g-i < 1.2) and very red (VR; g-i > 1.2), reflecting a difference in their surface composition. This is thought to imply that KBOs formed over a relatively wide range of radial distance, r. The cold classicals at 42 au < r < 47 au are predominantly VR, and known Neptune Trojans at r ≃ 30 au are mostly R. Intriguingly, however, the dynamically hot KBOs show a mix of R and VR colors and no correlation of color with r. Here we perform migration/instability simulations where the Kuiper Belt is populated from an extended planetesimal disk. We find that the color observations can be best understood if R objects formed at r < r∗ and VR objects at r > r∗, with 30 au < r∗ < 40 au. The proposed transition at 30 au < r∗ < 40 au would explain why the VR objects in the dynamically hot population have smaller orbital inclinations than the R objects, because the orbital excitation from Neptune weakens for orbits starting beyond 30 au. Possible causes of the R-VR color bimodality are discussed.
Original language | English |
---|---|
Article number | 46 |
Journal | Astronomical Journal |
Volume | 160 |
Issue number | 1 |
DOIs | |
Publication status | Published - 29 Jun 2020 |
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science
Fingerprint
Dive into the research topics of 'OSSOS XX: The Meaning of Kuiper Belt Colors'. Together they form a unique fingerprint.Student theses
-
Exploring the relics of planet formation: the Kuiper Belt colour/composition connection
Buchanan, L. (Author), Schwamb, M. (Supervisor) & Fitzsimmons, A. (Supervisor), Dec 2023Student thesis: Doctoral Thesis › Doctor of Philosophy
File