銀河に最も多い惑星の新たな像を提示する研究(New study revises our picture of the most common planets in the galaxy)

2025-11-05 シカゴ大学

シカゴ大学のEliza Kempton教授らは、最も一般的な系外惑星「ミニ・ネプチューン」の多くが溶融惑星ではなく固体表面を持つ可能性を示した。これまで高温高圧下で全球マグマ海に覆われていると考えられていたが、JWST観測とモデリングにより、厚い大気の圧力で岩石が再固化することが判明。代表例GJ 1214 bでは大気が重元素に富み、地球内部のような超高圧条件で固体化が起こると示された。惑星形成理論の再考を促し、系外惑星の多様性理解に新視点を与える。成果はAstrophysical Journal Letters誌に掲載。

銀河に最も多い惑星の新たな像を提示する研究(New study revises our picture of the most common planets in the galaxy)
A new study finds that many “mini-Neptunes”—perhaps the most common planets in the galaxy—are under so much pressure from their heavy atmospheres that the surface is likely compressed solid. Illustration courtesy NASA/JPL-Caltech/R. Hurt (IPAC)

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海王星より下の太陽系外惑星の全てがマグマオーシャンを持つわけではない Not All Sub-Neptune Exoplanets Have Magma Oceans

Bodie Breza, Matthew C. Nixon, and Eliza M.-R. Kempton
The Astrophysical Journal Letters  Published: 2025 November 5
DOI:10.3847/2041-8213/ae0c07

Abstract

The evolution and structure of sub-Neptunes may be strongly influenced by interactions between the outer gaseous envelope of the planet and a surface magma ocean. However, given the wide variety of permissible interior structures of these planets, it is unclear whether conditions at the envelope–mantle boundary will always permit a molten silicate layer or whether some sub-Neptunes might instead host a solid silicate surface. In this work, we use internal structure modeling to perform an extensive exploration of surface conditions within the sub-Neptune population across a range of bulk and atmospheric parameters. We find that a significant portion of the population may lack present-day magma oceans. In particular, planets with a high atmospheric mean molecular weight and large envelope mass fraction are likely to instead have a solid silicate surface, since the pressure at the envelope–mantle boundary is high enough that the silicates will be in solid postperovskite phase. This result is particularly relevant given recent inferences of high-mean molecular weight atmospheres from JWST observations of several sub-Neptunes. We apply this approach to a number of sub-Neptunes with existing or upcoming JWST observations and find that in almost all cases, a range of solutions exist that do not possess a present-day magma ocean. Our analysis provides critical context for interpreting sub-Neptunes and their atmospheres.

1701物理及び化学
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