Skip to content
DraconiticResearch
Search Sources API
190,332 studies31 sourcesUpdated 42 min ago
PreprintCC BY 4.0arXiv

Surface regolith model of near-Earth asteroid (3200) Phaethon

Abstract

The near-Earth asteroid (3200) Phaethon displays activity as it comes close to the Sun and is presumed to be the progenitor of the Geminids meteor shower. Both CM- and CY-meteorites have been suggested as possible meteorite analogues for Phaethon. Previous spectral and polarization measurements of Phaethon indicate possible surface heterogeneity in the regolith properties. By combining mineral components and their size fractions, we present a regolith model for Phaethon that reproduces the spectral, polarization, and geometric albedo measurements presented in various studies, with the aim of quantitatively characterizing the surface material and structure, as well as the regolith heterogeneity. The best fit model able to produce the measurements is constructed from large olivine particles with troilite inclusions and small scale surface roughness, mixed with smaller, porous troilite aggregates comprised of monomers resembling interplanetary dust. Our model suggests that the different spectral and polarization responses of the regolith are caused by changes in the size and amount of the small dark troilite particles. Based on the amount of troilite in the regolith model, we propose that CM-meteorites are the preferable meteorite analogue for Phaethon.

Related

  1. Dynamical Behavior and Surface Features of Large Super-Fast Rotator Near-Earth Asteroid (436724) 2011 UW158
    Caio Gomes, Andre Amarante, Filipe Monteiro +7
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsarXiv
  2. Photometric Study of the Fastest-rotating Near-Earth Asteroid 2024 XA1
    Xiliang Zhang, Xiangyu Fan, Man-To Hui +4
    The Astronomical JournalPeer-reviewedCC BY 4.0Full textPlanetary science & exoplanetsCrossref
  3. The dark surface of (163693) Atira and implications for inner-Earth asteroid origins
    Bryce T. Bolin, Carl Ingebretsen, Robert Jedicke +8
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsarXiv
  4. Constraining Particle Stiffness in Asteroid Regolith from Early-Time High-Speed Penetrator Dynamics under Local Granular Variability
    Zichen Wang, Yang Yu, Chenyang Huang +4
    arXivPreprintCC BY-NC-ND 4.0Full textInstrumentation & methodsPlanetary science & exoplanetsarXiv
  5. Polarimetric Behaviour of (3200) Phaethon: New Observations with Implications for Surface Heterogeneity
    Zuri Gray, Mikko Vuori, Eric MacLennan +4
    arXivPreprintCC BY 4.0Full textPlanetary science & exoplanetsarXiv
BibTeX
@misc{vuori2026surface,
  title = {{Surface regolith model of near-Earth asteroid (3200) Phaethon}},
  author = {Mikko Vuori and Antti Penttilä and Karri Muinonen and Hanna Pentikäinen and Ari Leppälä and Zuri Gray and Eric MacLennan and Mikael Granvik and Anne Virkki},
  howpublished = {arXiv},
  year = {2026},
  month = oct,
  doi = {10.48550/arxiv.2610.29383},
  eprint = {2610.29383},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2610.29383},
  note = {CC BY 4.0},
}
RIS
TY  - UNPB
TI  - Surface regolith model of near-Earth asteroid (3200) Phaethon
AU  - Mikko Vuori
AU  - Antti Penttilä
AU  - Karri Muinonen
AU  - Hanna Pentikäinen
AU  - Ari Leppälä
AU  - Zuri Gray
AU  - Eric MacLennan
AU  - Mikael Granvik
AU  - Anne Virkki
PY  - 2026
DA  - 2026/10/21
PB  - arXiv
DO  - 10.48550/arxiv.2610.29383
UR  - https://arxiv.org/abs/2610.29383
AB  - The near-Earth asteroid (3200) Phaethon displays activity as it comes close to the Sun and is presumed to be the progenitor of the Geminids meteor shower. Both CM- and CY-meteorites have been suggested as possible meteorite analogues for Phaethon. Previous spectral and polarization measurements of Phaethon indicate possible surface heterogeneity in the regolith properties. By combining mineral components and their size fractions, we present a regolith model for Phaethon that reproduces the spectral, polarization, and geometric albedo measurements presented in various studies, with the aim of quantitatively characterizing the surface material and structure, as well as the regolith heterogeneity. The best fit model able to produce the measurements is constructed from large olivine particles with troilite inclusions and small scale surface roughness, mixed with smaller, porous troilite aggregates comprised of monomers resembling interplanetary dust. Our model suggests that the different spectral and polarization responses of the regolith are caused by changes in the size and amount of the small dark troilite particles. Based on the amount of troilite in the regolith model, we propose that CM-meteorites are the preferable meteorite analogue for Phaethon.
ER  -