Implications of evaporative cooling by H for 1I/`Oumuamua
arXiv:2303.13861 · doi:10.3847/2041-8213/acdf57
Abstract
The first interstellar object observed in our solar system, 1I/`Oumuamua, exhibited several peculiar properties, including extreme elongation and non-gravitational acceleration. Bergner and Seligman (hereafter BS23) proposed that evaporation of trapped H created by cosmic rays (CRs) can explain the non-gravitational acceleration. However, their modeling of the thermal structure of 1I/`Oumuamua ignored the crucial cooling effect of evaporating H. By taking into account the cooling by H evaporation, we show that the surface temperature of H-water ice is a factor of 9 lower than the case without evaporative cooling. As a result, the thermal speed of outgassing H is decreased by a factor of 3. Our one-dimensional thermal modeling that takes into account evaporative cooling for two chosen values of thermal conductivity of and WKm shows that the water ice volume available for H sublimation at K would be reduced by a factor of 9 and 5 compared to the results of BS23, not enabling enough hydrogen to propel 1I/`Oumuamua.
arXiv comment6 pages, 2 figure; Accepted for publication, Astrophysical Journal Letters
References in corpus (23)
- Interstellar Interloper 1I/2017 U1: Observations from the NOT and WIYN Telescopes
- Could Solar Radiation Pressure Explain 'Oumuamua's Peculiar Acceleration?
- Spectroscopy and thermal modelling of the first interstellar object 1I/2017 U1 'Oumuamua
- Interstellar Interlopers: Number Density and Origins of 'Oumuamua-like Objects
- Spitzer Observations of Interstellar Object 1I/`Oumuamua
- Col-OSSOS: Colors of the Interstellar Planetesimal 1I/`Oumuamua
- The tumbling rotational state of 1I/`Oumuamua
- Modeling the light curve of `Oumuamua: evidence for torque and disc-like shape
- Evidence that 1I/2017 U1 (`Oumuamua) was composed of molecular hydrogen ice
- Tidal fragmentation as the origin of 1I/2017 U1 ('Oumuamua)
- Could 1I/'Oumuamua be an icy fractal aggregate?
- 1I/'Oumuamua as an N2 ice fragment of an exo-pluto surface. II. Generation of N2 ice fragments and the origin of 'Oumuamua
- 1I/'Oumuamua as an N2 ice fragment of an exo-Pluto surface: I. size and compositional constraints
- Spin Evolution and Cometary Interpretation of the Interstellar Minor Object 1I/2017 'Oumuamua
- Acceleration of 1I/`Oumuamua from radiolytically produced H in HO ice
- On origin and destruction of relativistic dust and its implication for ultrahigh energy cosmic rays
- Destruction of molecular hydrogen ice and Implications for 1I/2017 U1 (`Oumuamua)
- The similarity of the interstellar comet 2I/Borisov to solar system comets from high resolution optical spectroscopy
- Explaining the elongated shape of 'Oumuamua by the Eikonal abrasion model
- Solid H2 in the interstellar medium
- What and Whence 1I/`Oumuamua: A Contact Binary from the Debris of a Young Planetary System?
- Spinup and Disruption of Interstellar Asteroids by Mechanical Torques, and Implications for 1I/2017 U1 (`Oumuamua)
- Collisional Elongation: Possible Origin of Extremely Elongated Shape of 1I/`Oumuamua