Evidence that 1I/2017 U1 (`Oumuamua) was composed of molecular hydrogen ice
Darryl Seligman, Gregory Laughlin

TL;DR
This paper proposes that 'Oumuamua was composed mainly of molecular hydrogen ice, explaining its observed acceleration, shape, and trajectory through a novel sublimation model involving H2, and suggests such bodies form in cold molecular cloud cores.
Contribution
It introduces the hypothesis that 'Oumuamua's properties are consistent with H2 ice composition, providing a new explanation for its non-gravitational acceleration and shape evolution.
Findings
H2 sublimation can produce the observed acceleration
'Oumuamua's shape change is explained by mass wasting from sublimation
H2-rich bodies likely form in cold molecular cloud cores
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…
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