近傍スーパーアースの表面組成を解析し過酷環境を解明(A barren, rocky exoplanet with no protection from cosmic radiation)

2026-05-04 マックス・プランク研究所

Max Planck Societyの研究者らは、近傍のスーパーアース型系外惑星の表面組成を詳細に解析した。観測データと大気・地表モデルを組み合わせることで、この惑星が岩石主体か揮発性物質を含むかを推定し、表面環境の特徴を明らかにした。従来はサイズや質量からの間接推定に限られていたが、本研究はより直接的に化学組成へ迫る手法を提示している。これにより系外惑星の形成過程や進化、居住可能性の評価に新たな知見を提供する。今後の高精度観測と組み合わせることで、多様な惑星環境の理解がさらに進展すると期待される。

近傍スーパーアースの表面組成を解析し過酷環境を解明(A barren, rocky exoplanet with no protection from cosmic radiation)
Infrared spectrum of LHS 3844 b’s hot dayside derived from the brightness contrast to its host star in ppm (parts per million = 0.0001%) at different wavelengths. The observational data obtained from the James Webb and Spitzer Space Telescopes are consistent with mantle or lava rock, whereas they rule out an Earth-like crust.

<関連情報>

JWSTの中赤外線分光観測による、岩石質の系外惑星LHS 3844 bの暗く特徴のない表面 The dark and featureless surface of rocky exoplanet LHS 3844 b from JWST mid-infrared spectroscopy

Sebastian Zieba,Laura Kreidberg,Brandon P. Coy,Aaron Bello-Arufe,Kimberly Paragas,Xintong Lyu,Renyu Hu,Aishwarya Iyer,Edwin S. Kite,Daniel D. B. Koll,Kay Wohlfarth,Emerson Whittaker,Heather Knutson,Robin Wordsworth,Caroline Morley & Laura Schaefer
Nature Astronomy  Published:04 May 2026
DOI:https://doi.org/10.1038/s41550-026-02860-3

Abstract

The James Webb Space Telescope (JWST) has opened a new era in the study of rocky exoplanets, enabling direct characterization of their surfaces with mid-infrared spectroscopy. Different types of rock have distinct spectral features that are diagnostic of the chemical composition and other physical properties like surface texture. Measurements of these features can provide valuable clues about a planet’s geologic history and interior processes. Here we report a JWST 5–12-μm thermal emission spectrum for the rocky exoplanet LHS 3844 b. It is best matched by a dark, low-silica surface, such as basalt or other olivine-rich materials. The spectrum rules out surfaces covered by fresh, small-sized grains (powders); however, space weathering can darken the powders and make them more consistent with the data. The data also disfavour trace concentrations of CO2 or SO2 gas (with 5σ and 3σ upper limits of 100 mbar and 10 μbar, respectively). Taken together, these results are well fit by an old, space-weathered surface with no evidence of accumulated volcanic gases.

0303宇宙環境利用
ad
ad
Follow
ad
タイトルとURLをコピーしました