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Debris disks as signposts of terrestrial planet formation
Open accessAbstract
There exists strong circumstantial evidence from their eccentric orbits that most of the known extra-solar planetary systems are the survivors of violent dynamical instabilities. Here we explore the effect of giant planet instabilities on the formation and survival of terrestrial planets. We numerically simulate the evolution of planetary systems around Sun-like stars that include three components: (i) an inner disk of planetesimals and planetary embryos; (ii) three giant planets at Jupiter-Saturn distances; and (iii) an outer disk of planetesimals comparable to estimates of the primitive Kuiper belt. We calculate the dust production and spectral energy distribution of each system by assuming that each planetesimal particle represents an ensemble of smaller bodies in collisional equilibrium. Our main result is a strong correlation between the evolution of the inner and outer parts of planetary systems, i.e. between the presence of terrestrial planets and debris disks. Strong giant planet instabilities – that produce very eccentric surviving planets – destroy all rocky material in the system, including fully-formed terrestrial planets if the instabilities occur late, and also destroy the icy planetesimal population. Stable or weakly unstable systems allow terrestrial planets to accrete in their inner regions and significant dust to be produced in their outer regions, detectable at mid-infrared wavelengths as debris disks. Stars older than ~100 Myr with bright cold dust emission (in particular at λ ~ 70 μm) signpost dynamically calm environments that were conducive to efficient terrestrial accretion. Such emission is present around ~16% of billion-year old Solar-type stars. Our simulations yield numerous secondary results: 1) the typical eccentricities of as-yet undetected terrestrial planets are ~0.1 but there exists a novel class of terrestrial planet system whose single planet undergoes large amplitude oscillations in orbital eccentricity and inclination; 2) by scaling our systems to match the observed semimajor axis distribution of giant exoplanets, we predict that terrestrial exoplanets in the same systems should be a few times more abundant at ~0.5 AU than giant or terrestrial exoplanets at 1 AU; 3) the Solar System appears to be unusual in terms of its combination of a rich terrestrial planet system and a low dust content. This may be explained by the weak, outward-directed instability that is thought to have caused the late heavy bombardment.
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“while planet-planet scattering among gas giant planets is likely to produce a pulse of ejected planetesimals (Raymond et al. 2011;Marzari 2014)”
From Implications for Planetary System Formation from Interstellar Object 1I/2017 U1 (‘Oumuamua) (2017) · cites this paper as Raymond et al. 2011
In the citing paper
“and while systems with gas giants on stable orbits can eject planetesimals on longer timescales (Raymond et al. 2011;Barclay et al. 2017)”
From Implications for Planetary System Formation from Interstellar Object 1I/2017 U1 (‘Oumuamua) (2017) · cites this paper as Raymond et al. 2011
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Self-citation
Metadata
- Authors
- Raymond, S. N., Armitage, P. J., Moro-Martín, A., Booth, M., Wyatt, M. C., Armstrong, J. C., Mandell, A. M., Selsis, F., & West, A. A.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- Joint Institute for Laboratory Astrophysics (US)
- University of Victoria (CA)
- University of Cambridge (GB)
- Weber State University (US)
- Goddard Space Flight Center (US)
- Boston University (US)
- Venue
- Astronomy & Astrophysics
- Publisher
- EDP Sciences
- Published
- 2011-05-12
- Volume
- 530
- Pages
- A62
- ISSN
- 0004-6361 (ISSN-L)
- 1432-0746
- OpenAlex
- W1964193027
- Cited by
- 194
- References
- 184
- Citations by year
- 2026: 2 · 2025: 5 · 2024: 6 · 2023: 4 · 2022: 4 · 2021: 7 · 2020: 13 · 2019: 12 · 2018: 41 · 2017: 11 · 2016: 12 · 2015: 15 · 2014: 13 · 2013: 20 · 2012: 15
- FWCI
- 9.52
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Astronomy and Astrophysics (publishedVersion)
- arXiv (Cornell University) (submittedVersion)
- HAL (submittedVersion)
- Oskar-Bordeaux (Universite de Bordeaux) (submittedVersion)
- Funders
- National Science Foundation (0807471)
- National Aeronautics and Space Administration (NNX07AH08G, NNX09AB90G)
- Purdue University
- Weber State University
- University of Washington
- Centre National de la Recherche Scientifique
- NASA Astrobiology Institute
- Science and Technology Facilities Council (ST/H00243X/1, ST/G00269X/1)
- Division of Astronomical Sciences
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astrophysics and Star Formation Studies
- Keywords
- debris disks, terrestrial planet formation, giant planet instability, dynamical instability, dust formation, mid-infrared dust emission, eccentric planets, terrestrial exoplanets, giant exoplanets, Kuiper belt analog, Late Heavy Bombardment, solar-type stars
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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