Evidence that 1I/2017 U1 (`Oumuamua) was composed of molecular hydrogen ice
arXiv:2005.12932 · doi:10.3847/2041-8213/ab963f
Abstract
`Oumuamua (I1 2017) was the first macroscopic () body observed to traverse the inner solar system on an unbound hyperbolic orbit. Its light curve displayed strong periodic variation, and it showed no hint of a coma or emission from molecular outgassing. Astrometric measurements indicate that 'Oumuamua experienced non-gravitational acceleration on its outbound trajectory, but energy balance arguments indicate this acceleration is inconsistent with a water ice sublimation-driven jet of the type exhibited by solar system comets. We show that all of `Oumaumua's observed properties can be explained if it contained a significant fraction of molecular hydrogen (H) ice. H sublimation at a rate proportional to the incident solar flux generates a surface-covering jet that reproduces the observed acceleration. Mass wasting from sublimation leads to monotonic increase in the body axis ratio, explaining `Oumuamua's shape. Back-tracing `Oumuamua's trajectory through the Solar System permits calculation of its mass and aspect ratio prior to encountering the Sun. We show that H-rich bodies plausibly form in the coldest dense cores of Giant Molecular Clouds, where number densities are of order , and temperatures approach the background. Post-formation exposure to galactic cosmic rays implies a Myr age, explaining the kinematics of `Oumuamua's inbound trajectory.
arXiv commentAccepted for publication in ApJL, 8 pages, 2 figures. All software is available at https://github.com/DSeligman/Oumuamua_Hydrogen
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