Astrochemistry

An Impact-free Mechanism To Deliver Water To Terrestrial Planets And Exoplanets

By Keith Cowing
Status Report
astro-ph.EP
December 3, 2024
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An Impact-free Mechanism To Deliver Water To Terrestrial Planets And Exoplanets
Alma observation predictions to target water in HD 69830 showing the integrated flux in Jy.km.s−1 for the o-H2O 1029 − 936 transition at 321.22 GHz as a function of the temperature and the quantity of water. The black dashed line indicates the critical mass level when water starts self-shielding. The level at 0.012 Jy.km.s−1 is for a signalto-noise ratio of 5 represented by the solid white line labelled 5σ. This line is rather sensitive to low amounts of water and may allow for the detection of the first water gas disk in the near future. — astro-ph.EP

To date, the most widespread scenario is that the Earth originated without water and was brought to the planet mainly due to impacts by wet asteroids coming from further out in space. However, many uncertainties remain regarding the exact processes that supply water to inner terrestrial planets.

This article explores a new mechanism that would allow water to be efficiently transported to planets without impacts. We propose that primordial asteroids were icy and that when the ice sublimated, it formed a gaseous disk that could then reach planets and deliver water.

We have developed a new model that follows the sublimation of asteroids and evolves the subsequent gas disk using a viscous diffusion code. We can then quantify the amount of water that can be accreted onto each planet in a self-consistent manner.

We find that this new disk-delivery mechanism can explain the water content on Earth as well as on other planets. Our model shows most of the water being delivered between 20 and 30 Myr after the birth of the Sun. Our scenario implies the presence of a gaseous water disk with substantial mass for 100s Myr, which could be one of the key tracers of this mechanism.

We show that such a watery disk could be detected in young exo-asteroid belts with ALMA. We propose that viscous water transport is inevitable and more generic than the impact scenario. We also suggest it is a universal process that may also occur in extrasolar systems.

The conditions required for this scenario to unfold are indeed expected to be present in most planetary systems: an opaque proto-planetary disk that is initially cold enough for ice to form in the exo-asteroid belt region, followed by a natural outward-moving snow line that allows this initial ice to sublimate after the dissipation of the primordial disk, creating a viscous secondary gas disk and leading to the accretion of water onto the exoplanets.

Quentin Kral, Paul Huet, Camille Bergez-Casalou, Philippe Thébault, Sébastien Charnoz, Sonia Fornasier

Comments: 26 pages, 11 figures, accepted for publication in A&A. Abstract shortened
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2412.01409 [astro-ph.EP] (or arXiv:2412.01409v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2412.01409
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Related DOI:
https://doi.org/10.1051/0004-6361/202451263
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Submission history
From: Quentin Kral
[v1] Mon, 2 Dec 2024 11:54:30 UTC (275 KB)
https://arxiv.org/abs/2412.01409
Astrobiology, astrochemistry,

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻