Configuration of Single Giant Planet Systems Generating `Oumuamua-Like Interstellar Asteroids
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arXiv
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| Format: | Preprint |
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2025
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| _version_ | 1866913685918711808 |
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| author | Zheng, Xi-Ling Zhou, Ji-Lin |
| author_facet | Zheng, Xi-Ling Zhou, Ji-Lin |
| contents | The first discovered interstellar small object, `Oumuamua (1I/2017 U1), presents unique physical properties of extremely elongated geometric shape and dual characteristics of an asteroid and a comet. These properties suggest a possible origin through tidal fragmentation, which posits that `Oumuamua was produced through intensive tidal fragmentation during a close encounter with a star or a white dwarf, resulting in its shape and ejection from its natal system. According to this mechanism, a high initial orbit eccentricity and a small pericentre of the parent body are necessary to produce `Oumuamua-like objects. To verify whether this mechanism can occur in single giant planet systems, we conduct long-term numerical simulations of systems with a low-mass ($0.5M_\odot$) host star and a giant planet in this study. We determine that an eccentric orbit ($e_\mathrm{p}\sim0.2$) and a Jupiter-mass ($M_\mathrm{p}\sim M_\mathrm{J}$) of the planet appears to be optimal to generate sufficient perturbations for the production of `Oumuamua-like objects. When the planetary semi-major axis $a_\mathrm{p}$ increases, the proportion of planetesimals ejected beyond the system $P(\mathrm{ej})$ increases accordingly, while the possibilities of ejected planetesimals undergoing stellar tidal fragmentation $P(\mathrm{tidal}|\mathrm{ej})$ remains relatively constant at $\sim0.6\%$. Focusing on stellar tidal fragmentation alone, the ratio of extremely elongated interstellar objects to all interstellar objects is $P_\mathrm{e}\sim3\%$. |
| format | Preprint |
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arxiv_https___arxiv_org_abs_2502_03336 |
| institution | arXiv |
| publishDate | 2025 |
| record_format | arxiv |
| spellingShingle | Configuration of Single Giant Planet Systems Generating `Oumuamua-Like Interstellar Asteroids Zheng, Xi-Ling Zhou, Ji-Lin Earth and Planetary Astrophysics The first discovered interstellar small object, `Oumuamua (1I/2017 U1), presents unique physical properties of extremely elongated geometric shape and dual characteristics of an asteroid and a comet. These properties suggest a possible origin through tidal fragmentation, which posits that `Oumuamua was produced through intensive tidal fragmentation during a close encounter with a star or a white dwarf, resulting in its shape and ejection from its natal system. According to this mechanism, a high initial orbit eccentricity and a small pericentre of the parent body are necessary to produce `Oumuamua-like objects. To verify whether this mechanism can occur in single giant planet systems, we conduct long-term numerical simulations of systems with a low-mass ($0.5M_\odot$) host star and a giant planet in this study. We determine that an eccentric orbit ($e_\mathrm{p}\sim0.2$) and a Jupiter-mass ($M_\mathrm{p}\sim M_\mathrm{J}$) of the planet appears to be optimal to generate sufficient perturbations for the production of `Oumuamua-like objects. When the planetary semi-major axis $a_\mathrm{p}$ increases, the proportion of planetesimals ejected beyond the system $P(\mathrm{ej})$ increases accordingly, while the possibilities of ejected planetesimals undergoing stellar tidal fragmentation $P(\mathrm{tidal}|\mathrm{ej})$ remains relatively constant at $\sim0.6\%$. Focusing on stellar tidal fragmentation alone, the ratio of extremely elongated interstellar objects to all interstellar objects is $P_\mathrm{e}\sim3\%$. |
| title | Configuration of Single Giant Planet Systems Generating `Oumuamua-Like Interstellar Asteroids |
| topic | Earth and Planetary Astrophysics |
| url | https://arxiv.org/abs/2502.03336 |