School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA.
Bay Area Environmental Research Institute, NASA's Ames Research Center, Moffett Field, CA, USA.
Nature. 2024 Jun;630(8018):836-840. doi: 10.1038/s41586-024-07514-w. Epub 2024 May 20.
Interactions between exoplanetary atmospheres and internal properties have long been proposed to be drivers of the inflation mechanisms of gaseous planets and apparent atmospheric chemical disequilibrium conditions. However, transmission spectra of exoplanets have been limited in their ability to observationally confirm these theories owing to the limited wavelength coverage of the Hubble Space Telescope (HST) and inferences of single molecules, mostly HO (ref. ). In this work, we present the panchromatic transmission spectrum of the approximately 750 K, low-density, Neptune-sized exoplanet WASP-107b using a combination of HST Wide Field Camera 3 (WFC3) and JWST Near-Infrared Camera (NIRCam) and Mid-Infrared Instrument (MIRI). From this spectrum, we detect spectroscopic features resulting from HO (21σ), CH (5σ), CO (7σ), CO (29σ), SO (9σ) and NH (6σ). The presence of these molecules enables constraints on the atmospheric metal enrichment (M/H is 10-18× solar), vertical mixing strength (logK = 8.4-9.0 cm s) and internal temperature (>345 K). The high internal temperature is suggestive of tidally driven inflation acting on a Neptune-like internal structure, which can naturally explain the large radius and low density of the planet. These findings suggest that eccentricity-driven tidal heating is a critical process governing atmospheric chemistry and interior-structure inferences for most of the cool (<1,000 K) super-Earth-to-Saturn-mass exoplanet population.
系外行星大气与其内部性质之间的相互作用一直被认为是驱动气态行星膨胀机制和明显大气化学失衡状态的因素。然而,由于哈勃太空望远镜(HST)的波长覆盖范围有限,以及对单个分子(主要是 HO)的推断,系外行星的传输光谱在观测上确认这些理论的能力有限。在这项工作中,我们使用哈勃太空望远镜宽场相机 3(WFC3)和 JWST 近红外相机(NIRCam)和中红外仪器(MIRI)组合,展示了约 750 K、低密度、海王星大小的系外行星 WASP-107b 的全色传输光谱。从这个光谱中,我们探测到了 HO(21σ)、CH(5σ)、CO(7σ)、CO(29σ)、SO(9σ)和 NH(6σ)的光谱特征。这些分子的存在使得可以限制大气金属丰度(M/H 为 10-18×太阳)、垂直混合强度(logK=8.4-9.0 cm s)和内部温度(>345 K)。内部温度高表明潮汐驱动的膨胀作用于类似海王星的内部结构,这可以自然地解释行星的大半径和低密度。这些发现表明,偏心驱动的潮汐加热是大多数冷却(<1,000 K)超地球到土星质量系外行星的大气化学和内部结构推断的关键过程。