From stars to diverse mantles, melts, crusts and atmospheres of rocky exoplanets

Fuente: arXiv
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Autori principali: Guimond, Claire Marie, Wang, Haiyang, Seidler, Fabian, Sossi, Paolo, Mahajan, Aprajit, Shorttle, Oliver
Natura: Preprint
Pubblicazione: 2024
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author Guimond, Claire Marie
Wang, Haiyang
Seidler, Fabian
Sossi, Paolo
Mahajan, Aprajit
Shorttle, Oliver
author_facet Guimond, Claire Marie
Wang, Haiyang
Seidler, Fabian
Sossi, Paolo
Mahajan, Aprajit
Shorttle, Oliver
contents This review is focused on describing the logic by which we make predictions of exoplanetary compositions and mineralogies, and how these processes could lead to compositional diversity among rocky exoplanets. We use these predictions to determine the sensitivity of present-day and future observations to detecting compositional differences between rocky exoplanets and the four terrestrial planets. First, we review data on stellar abundances and infer how changes in composition may manifest themselves in the expected bulk compositions of rocky exoplanets (section 2). Converting this information in mass-radius relationships requires calculation of the stable mineral assemblages at a given temperature-pressure-composition (T-P-X), an exercise we describe in section 3. Should the planet be hot enough to engender partial melting of the mantle, then these liquids are likely to rise to the surface and erupt to form planetary crusts; the possible compositional and mineralogical variability of which we examine in section 4. Finally, the expected spectroscopic responses of such crusts are examined in section 5.
format Preprint
id arxiv_https___arxiv_org_abs_2404_15427
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle From stars to diverse mantles, melts, crusts and atmospheres of rocky exoplanets
Guimond, Claire Marie
Wang, Haiyang
Seidler, Fabian
Sossi, Paolo
Mahajan, Aprajit
Shorttle, Oliver
Earth and Planetary Astrophysics
Solar and Stellar Astrophysics
Geophysics
This review is focused on describing the logic by which we make predictions of exoplanetary compositions and mineralogies, and how these processes could lead to compositional diversity among rocky exoplanets. We use these predictions to determine the sensitivity of present-day and future observations to detecting compositional differences between rocky exoplanets and the four terrestrial planets. First, we review data on stellar abundances and infer how changes in composition may manifest themselves in the expected bulk compositions of rocky exoplanets (section 2). Converting this information in mass-radius relationships requires calculation of the stable mineral assemblages at a given temperature-pressure-composition (T-P-X), an exercise we describe in section 3. Should the planet be hot enough to engender partial melting of the mantle, then these liquids are likely to rise to the surface and erupt to form planetary crusts; the possible compositional and mineralogical variability of which we examine in section 4. Finally, the expected spectroscopic responses of such crusts are examined in section 5.
title From stars to diverse mantles, melts, crusts and atmospheres of rocky exoplanets
topic Earth and Planetary Astrophysics
Solar and Stellar Astrophysics
Geophysics
url https://arxiv.org/abs/2404.15427