Wet-and-wild water worlds may form under pressure

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Image by Adis Resic from Pixabay
Image by Adis Resic from Pixabay

Some planets may produce water during their formation via reactions between their rocks and hydrogen under pressure, according to international research. The team experimented with pulsed lasers and high pressure to heat rock samples in the lab. They found that hydrogen reacted with melted silicates from the rocks, releasing oxygen that bonded with leftover hydrogen to form water. They suggest that this reaction could happen in the core of exoplanets over billions of years. This method of water creation on planets differs from what has typically been observed on exoplanets between the size of Earth and Neptune that are located far away from their host star, where water comes from space, and could explain why NASA's Kepler mission was able to find exoplanets with liquid water that orbit closer to their host star.

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From: Springer Nature

Planetary science: Water worlds might form under pressure (N&V)

Some exoplanets may produce water during their formation via reactions between rocks and hydrogen, according to new research in Nature. The findings offer insight into why some exoplanets have water on their surface.

The presence of water is a key ingredient in determining a planet’s habitability, and water has been thought to form through condensation from space as ice or snow at low temperatures. This process has typically been observed in exoplanets between the size of Earth and Neptune that are located far away from their host star. However, NASA’s Kepler mission has found exoplanets between the sizes of Earth and Neptune with liquid water that orbit close to their sun, calling this process into question.

Harrison Horn and colleagues simulated reactions that could occur during planetary formation by heating rock samples with pulsed lasers in a high-pressure laboratory environment. They observed that hydrogen reacted with melted silicates from the rocks to release oxygen, which then bonded with leftover hydrogen to form water molecules. The authors suggest that this reaction could most likely occur in the high-pressure and high-temperature core–envelope boundary of exoplanets, where the denser, rocky core meets an outer envelope of gaseous elements. They suggest that this water-generating reaction could occur over billions of years on some exoplanets more massive than Earth. However, the speed of these reactions is determined by how much hydrogen is available and how hot the core–envelope boundary is.

The authors note that these findings challenge the pre-existing knowledge on how water forms on exoplanets of certain sizes and at certain distances from their host star.

Journal/
conference:
Nature
Research:Paper
Organisation/s: Arizona State University, USA
Funder: S.-H.S. and H.W.H. were supported by the National Science Foundation (NSF) grants AST-2108129, AST-2406790 and EAR-1921298. Portions of this work were performed at GeoSoilEnviroCARS (The University of Chicago, Sector 13), Advanced Photon Source, Argonne National Laboratory. GeoSoilEnviroCARS is supported by the NSF, Earth Sciences (EAR-1634415). This research used resources of the Advanced Photon Source, a US DOE Office of Science User Facility operated for the DOE Office of Science by the Argonne National Laboratory under contract no. DE-AC02-06CH11357. We acknowledge the use of facilities in the Eyring Materials Center at ASU. Part of this work was performed under the auspices of the US DOE by Lawrence Livermore National Laboratory under contract DE-AC52-07NA27344. The opinions are those of the authors and do not necessarily represent the opinions of LLNL, LLNS, DOE, NNSA or the US government. The US government, and the publisher, by accepting the article for publication, acknowledge that the US government retains a non-exclusive, paid-up, irrevocable, worldwide licence to publish or reproduce the published form of this manuscript, or allow others to do so, for US government purposes (release authorization no. LLNL-JRNL-872168). A.V. acknowledges support by ISF grants 770/21 and 773/21.
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