TY - JOUR
T1 - Hydrogen escaping from a pair of exoplanets smaller than Neptune
AU - Loyd, R. O.Parke
AU - Schreyer, Ethan
AU - Owen, James E.
AU - Rogers, James G.
AU - Broome, Madelyn I.
AU - Shkolnik, Evgenya L.
AU - Murray-Clay, Ruth
AU - Wilson, David J.
AU - Peacock, Sarah
AU - Teske, Johanna
AU - Schlichting, Hilke E.
AU - Duvvuri, Girish M.
AU - Youngblood, Allison
AU - Schneider, P. Christian
AU - France, Kevin
AU - Giacalone, Steven
AU - Batalha, Natasha E.
AU - Schneider, Adam C.
AU - Longo, Isabella
AU - Barman, Travis
AU - Ardila, David R.
N1 - Publisher Copyright:
© The Author(s), under exclusive licence to Springer Nature Limited 2025.
PY - 2025/2/20
Y1 - 2025/2/20
N2 - Exoplanet surveys have shown a class of abundant exoplanets smaller than Neptune on close, <100-day orbits1, 2, 3–4. These planets form two populations separated by a natural division at about 1.8 R⊕ termed the radius valley. It is uncertain whether these populations arose from separate dry versus water-rich formation channels, evolved apart because of long-term atmospheric loss or a combination of both5, 6, 7, 8, 9, 10, 11, 12, 13–14. Here we report observations of ongoing hydrogen loss from two sibling planets, TOI-776 b (1.85 ± 0.13 R⊕) and TOI-776 c (2.02 ± 0.14 R⊕), the sizes of which near the radius valley and mature (1–4 Gyr) age make them valuable for investigating the origins of the divided population of which they are a part. During the transits of these planets, absorption appeared against the Lyman-α emission of the host star, compatible with hydrogen escape at rates equivalent to 0.03–0.6% and 0.1–0.9% of the total mass per billion years of each planet, respectively. Observations of the outer planet, TOI-776 c, are incompatible with an outflow of dissociated steam, suggesting both it and its inner sibling formed in a dry environment. These observations support the strong role of hydrogen loss in the evolution of close-orbiting sub-Neptunes5, 6, 7–8,15,16.
AB - Exoplanet surveys have shown a class of abundant exoplanets smaller than Neptune on close, <100-day orbits1, 2, 3–4. These planets form two populations separated by a natural division at about 1.8 R⊕ termed the radius valley. It is uncertain whether these populations arose from separate dry versus water-rich formation channels, evolved apart because of long-term atmospheric loss or a combination of both5, 6, 7, 8, 9, 10, 11, 12, 13–14. Here we report observations of ongoing hydrogen loss from two sibling planets, TOI-776 b (1.85 ± 0.13 R⊕) and TOI-776 c (2.02 ± 0.14 R⊕), the sizes of which near the radius valley and mature (1–4 Gyr) age make them valuable for investigating the origins of the divided population of which they are a part. During the transits of these planets, absorption appeared against the Lyman-α emission of the host star, compatible with hydrogen escape at rates equivalent to 0.03–0.6% and 0.1–0.9% of the total mass per billion years of each planet, respectively. Observations of the outer planet, TOI-776 c, are incompatible with an outflow of dissociated steam, suggesting both it and its inner sibling formed in a dry environment. These observations support the strong role of hydrogen loss in the evolution of close-orbiting sub-Neptunes5, 6, 7–8,15,16.
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U2 - 10.1038/s41586-024-08490-x
DO - 10.1038/s41586-024-08490-x
M3 - Article
C2 - 39939756
AN - SCOPUS:85217793006
SN - 0028-0836
VL - 638
SP - 636
EP - 639
JO - Nature
JF - Nature
IS - 8051
ER -