Hydrogen sulfide and metal-enriched atmosphere for a Jupiter-mass exoplanet

As the closest transiting hot Jupiter to Earth, HD 189733b has been the benchmark planet for atmospheric characterization 1 – 3 . It has also been the anchor point for much of our theoretical understanding of exoplanet atmospheres from composition 4 , chemistry 5 , 6 , aerosols 7 to atmospheric dyna...

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Veröffentlicht in:Nature (London) 2024-08, Vol.632 (8026), p.752-756
Hauptverfasser: Fu, Guangwei, Welbanks, Luis, Deming, Drake, Inglis, Julie, Zhang, Michael, Lothringer, Joshua, Ih, Jegug, Moses, Julianne I., Schlawin, Everett, Knutson, Heather A., Henry, Gregory, Greene, Thomas, Sing, David K., Savel, Arjun B., Kempton, Eliza M.-R., Louie, Dana R., Line, Michael, Nixon, Matt
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container_title Nature (London)
container_volume 632
creator Fu, Guangwei
Welbanks, Luis
Deming, Drake
Inglis, Julie
Zhang, Michael
Lothringer, Joshua
Ih, Jegug
Moses, Julianne I.
Schlawin, Everett
Knutson, Heather A.
Henry, Gregory
Greene, Thomas
Sing, David K.
Savel, Arjun B.
Kempton, Eliza M.-R.
Louie, Dana R.
Line, Michael
Nixon, Matt
description As the closest transiting hot Jupiter to Earth, HD 189733b has been the benchmark planet for atmospheric characterization 1 – 3 . It has also been the anchor point for much of our theoretical understanding of exoplanet atmospheres from composition 4 , chemistry 5 , 6 , aerosols 7 to atmospheric dynamics 8 , escape 9 and modelling techniques 10 , 11 . Previous studies of HD 189733b have detected carbon and oxygen-bearing molecules H 2 O and CO (refs.  12 , 13 ) in the atmosphere. The presence of CO 2 and CH 4 has been claimed 14 , 15 but later disputed 12 , 16 , 17 . The inferred metallicity based on these measurements, a key parameter in tracing planet formation locations 18 , varies from depletion 19 , 20 to enhancement 21 , 22 , hindered by limited wavelength coverage and precision of the observations. Here we report detections of H 2 O (13.4 σ ), CO 2 (11.2 σ ), CO (5 σ ) and H 2 S (4.5 σ ) in the transmission spectrum (2.4–5.0 μm) of HD 189733b. With an equilibrium temperature of about 1,200 K, H 2 O, CO and H 2 S are the main reservoirs for oxygen, carbon and sulfur. Based on the measured abundances of these three main volatile elements, we infer an atmospheric metallicity of three to five times stellar. The upper limit on the methane abundance at 5 σ is 0.1 ppm, which indicates a low carbon-to-oxygen ratio (
doi_str_mv 10.1038/s41586-024-07760-y
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It has also been the anchor point for much of our theoretical understanding of exoplanet atmospheres from composition 4 , chemistry 5 , 6 , aerosols 7 to atmospheric dynamics 8 , escape 9 and modelling techniques 10 , 11 . Previous studies of HD 189733b have detected carbon and oxygen-bearing molecules H 2 O and CO (refs.  12 , 13 ) in the atmosphere. The presence of CO 2 and CH 4 has been claimed 14 , 15 but later disputed 12 , 16 , 17 . The inferred metallicity based on these measurements, a key parameter in tracing planet formation locations 18 , varies from depletion 19 , 20 to enhancement 21 , 22 , hindered by limited wavelength coverage and precision of the observations. Here we report detections of H 2 O (13.4 σ ), CO 2 (11.2 σ ), CO (5 σ ) and H 2 S (4.5 σ ) in the transmission spectrum (2.4–5.0 μm) of HD 189733b. With an equilibrium temperature of about 1,200 K, H 2 O, CO and H 2 S are the main reservoirs for oxygen, carbon and sulfur. Based on the measured abundances of these three main volatile elements, we infer an atmospheric metallicity of three to five times stellar. The upper limit on the methane abundance at 5 σ is 0.1 ppm, which indicates a low carbon-to-oxygen ratio (&lt;0.2), suggesting formation through the accretion of water-rich icy planetesimals. The low oxygen-to-sulfur and carbon-to-sulfur ratios also support the planetesimal accretion formation pathway 23 . 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It has also been the anchor point for much of our theoretical understanding of exoplanet atmospheres from composition 4 , chemistry 5 , 6 , aerosols 7 to atmospheric dynamics 8 , escape 9 and modelling techniques 10 , 11 . Previous studies of HD 189733b have detected carbon and oxygen-bearing molecules H 2 O and CO (refs.  12 , 13 ) in the atmosphere. The presence of CO 2 and CH 4 has been claimed 14 , 15 but later disputed 12 , 16 , 17 . The inferred metallicity based on these measurements, a key parameter in tracing planet formation locations 18 , varies from depletion 19 , 20 to enhancement 21 , 22 , hindered by limited wavelength coverage and precision of the observations. Here we report detections of H 2 O (13.4 σ ), CO 2 (11.2 σ ), CO (5 σ ) and H 2 S (4.5 σ ) in the transmission spectrum (2.4–5.0 μm) of HD 189733b. With an equilibrium temperature of about 1,200 K, H 2 O, CO and H 2 S are the main reservoirs for oxygen, carbon and sulfur. Based on the measured abundances of these three main volatile elements, we infer an atmospheric metallicity of three to five times stellar. The upper limit on the methane abundance at 5 σ is 0.1 ppm, which indicates a low carbon-to-oxygen ratio (&lt;0.2), suggesting formation through the accretion of water-rich icy planetesimals. The low oxygen-to-sulfur and carbon-to-sulfur ratios also support the planetesimal accretion formation pathway 23 . 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subjects 639/33/34/862
639/33/445/824
639/33/445/862
Abundance
Atmosphere
Atmosphere - chemistry
Atmospheric models
Carbon
Carbon dioxide
Carbon Dioxide - analysis
Carbon Monoxide - analysis
Extrasolar planets
Extraterrestrial Environment - chemistry
Gas giant planets
Humanities and Social Sciences
Hydrogen sulfide
Hydrogen Sulfide - analysis
Hydrogen Sulfide - chemistry
Hydrogen Sulfide - metabolism
Jupiter
Light
Metallicity
Metals - analysis
Metals - chemistry
Methane - analysis
Methane - chemistry
multidisciplinary
Oxygen
Planet formation
Planetary atmospheres
Planets
Science
Science (multidisciplinary)
Sulfur
Temperature
Water - analysis
Water - chemistry
title Hydrogen sulfide and metal-enriched atmosphere for a Jupiter-mass exoplanet
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