Oxidation of the Interiors of Carbide Exoplanets

Astrophysical measurements have shown that some stars have sufficiently high carbon-to-oxygen ratios such that the planets they host would be mainly composed of carbides instead of silicates. We studied the behavior of silicon carbide in the presence of water under the high pressure–temperature cond...

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Main Authors: H. W. Horn, E. Garhart, K. Leinenweber, V. Prakapenka, E. Greenberg, S.-H. Shim
Format: Article
Language:English
Published: IOP Publishing 2020-01-01
Series:The Planetary Science Journal
Subjects:
Online Access:https://doi.org/10.3847/PSJ/abaa3e
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author H. W. Horn
E. Garhart
K. Leinenweber
V. Prakapenka
E. Greenberg
S.-H. Shim
author_facet H. W. Horn
E. Garhart
K. Leinenweber
V. Prakapenka
E. Greenberg
S.-H. Shim
author_sort H. W. Horn
collection DOAJ
description Astrophysical measurements have shown that some stars have sufficiently high carbon-to-oxygen ratios such that the planets they host would be mainly composed of carbides instead of silicates. We studied the behavior of silicon carbide in the presence of water under the high pressure–temperature conditions relevant to planetary interiors in the laser-heated diamond-anvil cell. When reacting with water, silicon carbide converts to silica (stishovite) and diamond at pressures up to 50 GPa and temperatures up to 2500 K: $\mathrm{SiC}+2{{\rm{H}}}_{2}{\rm{O}}\to {\mathrm{SiO}}_{2}+{\rm{C}}+2{{\rm{H}}}_{2}$ . Therefore, if water can be incorporated into carbide planets during their formation or through later delivery, they could be oxidized and have mineralogy dominated by silicates and diamond in their interiors. The reaction could produce CH _4 at shallower depths and H _2 at greater depths that could be degassed from the interior, causing the atmospheres of the converted carbon planets to be rich in reducing gases. Excess water after the reaction can be stored in dense silica polymorphs in the interiors of the converted carbon planets. Such conversion of mineralogy to diamond and silicates would decrease the density of carbon-rich planet, making the converted planets distinct from silicate planets in mass–radius relations for the 2–8 Earth mass range.
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spelling doaj-art-58f0bdc1e51f4785aabeb2bbf648b4882025-08-20T03:09:24ZengIOP PublishingThe Planetary Science Journal2632-33382020-01-01123910.3847/PSJ/abaa3eOxidation of the Interiors of Carbide ExoplanetsH. W. Horn0https://orcid.org/0000-0003-3809-0446E. Garhart1K. Leinenweber2V. Prakapenka3E. Greenberg4S.-H. Shim5https://orcid.org/0000-0001-5203-6038School of Earth and Space Exploration, Arizona State University , Tempe, AZ 85287, USA ; horn24@llnl.gov , shdshim@gmail.comSchool of Earth and Space Exploration, Arizona State University , Tempe, AZ 85287, USA ; horn24@llnl.gov , shdshim@gmail.comEyring Materials Center, Arizona State University , Tempe, AZ 85287, USAGeoSoilEnviroCARS, University of Chicago , Chicago, IL 60637, USAGeoSoilEnviroCARS, University of Chicago , Chicago, IL 60637, USASchool of Earth and Space Exploration, Arizona State University , Tempe, AZ 85287, USA ; horn24@llnl.gov , shdshim@gmail.comAstrophysical measurements have shown that some stars have sufficiently high carbon-to-oxygen ratios such that the planets they host would be mainly composed of carbides instead of silicates. We studied the behavior of silicon carbide in the presence of water under the high pressure–temperature conditions relevant to planetary interiors in the laser-heated diamond-anvil cell. When reacting with water, silicon carbide converts to silica (stishovite) and diamond at pressures up to 50 GPa and temperatures up to 2500 K: $\mathrm{SiC}+2{{\rm{H}}}_{2}{\rm{O}}\to {\mathrm{SiO}}_{2}+{\rm{C}}+2{{\rm{H}}}_{2}$ . Therefore, if water can be incorporated into carbide planets during their formation or through later delivery, they could be oxidized and have mineralogy dominated by silicates and diamond in their interiors. The reaction could produce CH _4 at shallower depths and H _2 at greater depths that could be degassed from the interior, causing the atmospheres of the converted carbon planets to be rich in reducing gases. Excess water after the reaction can be stored in dense silica polymorphs in the interiors of the converted carbon planets. Such conversion of mineralogy to diamond and silicates would decrease the density of carbon-rich planet, making the converted planets distinct from silicate planets in mass–radius relations for the 2–8 Earth mass range.https://doi.org/10.3847/PSJ/abaa3eExoplanet structureExoplanet atmospheresCarbon planetsExoplanet evolution
spellingShingle H. W. Horn
E. Garhart
K. Leinenweber
V. Prakapenka
E. Greenberg
S.-H. Shim
Oxidation of the Interiors of Carbide Exoplanets
The Planetary Science Journal
Exoplanet structure
Exoplanet atmospheres
Carbon planets
Exoplanet evolution
title Oxidation of the Interiors of Carbide Exoplanets
title_full Oxidation of the Interiors of Carbide Exoplanets
title_fullStr Oxidation of the Interiors of Carbide Exoplanets
title_full_unstemmed Oxidation of the Interiors of Carbide Exoplanets
title_short Oxidation of the Interiors of Carbide Exoplanets
title_sort oxidation of the interiors of carbide exoplanets
topic Exoplanet structure
Exoplanet atmospheres
Carbon planets
Exoplanet evolution
url https://doi.org/10.3847/PSJ/abaa3e
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AT kleinenweber oxidationoftheinteriorsofcarbideexoplanets
AT vprakapenka oxidationoftheinteriorsofcarbideexoplanets
AT egreenberg oxidationoftheinteriorsofcarbideexoplanets
AT shshim oxidationoftheinteriorsofcarbideexoplanets