2011/10/20 by M. R. Hogerheijde, Michiel R. Hogerheijde, Edwin A. Bergin +22 · 8 citations
Chemistry · Physics and Astronomy · #Astro and Planetary Science #Astrobiology #Astrophysics #Astrophysics and Star Formation Studies #Biology #Chemistry #Environmental science #Geology #Petroleum engineering #Physics #Planet #Stellar, planetary, and galactic studies #Water ice #Water reservoir #Water vapor #astro-ph.EP #astro-ph.SR
paper · pdf · doi:10.1126/science.1208931
published as Science 6054 (2011), 338 · 18 pages, 2 figures. Corrected typo in reported mass (in g) of detected water vapor reservoir. All conclusions are unchanged
openalex publication_date 2011/10/20 · arxiv created 2011/10/24 · arxiv updated 2015/05/29 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/05
Icy bodies may have delivered the oceans to the early Earth, yet little is known about water in the ice-dominated regions of extrasolar planet-forming disks. The Heterodyne Instrument for the Far-Infrared on board the Herschel Space Observatory has detected emission lines from both spin isomers of cold water vapor from the disk around the young star TW Hydrae. This water vapor likely originates from ice-coated solids near the disk surface, hinting at a water ice reservoir equivalent to several thousand Earth oceans in mass. The water's ortho-to-para ratio falls well below that of solar system comets, suggesting that comets contain heterogeneous ice mixtures collected across the entire solar nebula during the early stages of planetary birth.