Col-OSSOS: Investigating the Origins of Different Surfaces in the Primordial Kuiper Belt
Laura E. Buchanan, Megan E. Schwamb, Wesley C. Fraser, Michele T. Bannister, J. J. Kavelaars, Michaël Marsset, Rosemary E. Pike, David Nesvorný, Samantha M. Lawler, Susan D. Benecchi, Nuno Peixinho, Nicole J. Tan, Kathryn Volk, Mike Alexandersen, Jean-Marc Petit
TL;DR
Col-OSSOS colours of TNOs reveal a bimodal optical distribution linked to a bi- or multi-component primordial disk. The authors couple Col-OSSOS data with two Neptune-migration scenarios (condensed and extended disks) to locate a surface-colour transition line, testing Red/Neutral and BrightIR/FaintIR classifications via binomial likelihoods and dynamical cuts. They employ the OSSOS survey simulator and a CFEPS L7 intrinsic-population model to estimate intrinsic colour fractions, finding that inner-neutral/outer-red or inner-BrightIR/outer-FaintIR disk configurations best explain the observations, with transition positions around 27–32 au depending on the model. The work provides constraints on early solar-system structure, informs interpretations of Neptune Trojans and blue binaries, and demonstrates a framework ready for upcoming LSST data to further refine the primordial-color distribution in the Kuiper belt.
Abstract
The Colours of the Outer Solar System Origins Survey (Col-OSSOS) measured the optical/NIR colours of a brightness-complete sample of Trans-Neptunian Objects (TNOs). Like previous surveys, this one found a bimodal colour distribution in TNOs, categorised as red and very red. Additionally, this survey proposed an alternative surface classification scheme: FaintIR and BrightIR. Cold classical TNOs mostly have very red or FaintIR surfaces, while dynamically excited TNOs show a mixture of surfaces. This likely indicates that formation locations and proximity to the Sun influenced surface characteristics and color changes. Our study combines the data from Col-OSSOS with two dynamical models describing the formation of the Kuiper belt during Neptune's migration. We investigate the proposed surface-colour changing line and explore the distribution of different surfaces within the primordial disk. By comparing radial colour transitions across various scenarios, we explore the origins of surface characteristics and their implications within the context of BrightIR and FaintIR classifications. Moreover, we extend our analysis to examine the distribution of these surface classes within the present-day Kuiper Belt, providing insights into the configuration of the early solar system's planetesimal disk prior to giant planet migration. We find that the most likely primordial disk compositions are inner neutral / outer red (with transition $30.0^{+1.1}_{-1.2}$ au), or inner BrightIR / outer FaintIR (with transition $31.5^{+1.1}_{-1.2}$ au).
