论文标题
坚固的磁化和金属势氛围的签名
Signatures of Strong Magnetization and Metal-Poor Atmosphere for a Neptune-Size Exoplanet
论文作者
论文摘要
外球星的磁层尚未明确检测到。在运输过程中,恒星行星相互作用和中性原子氢的吸收以检测热木星中的磁场的研究尚无定论,并且对过境吸收非唯一的解释。相比之下,离子化的物种逃脱了磁化外球星球,尤其是从极性盖中,应填充磁层,从而可以检测到从等离子体到扩展的磁尾的不同区域,以及产生它们的磁场的表征。在这里,我们报告了HAT-P-11B的紫外线观测,低质量(0.08 MJ)外球星表现出中性氢的强,相扩展的过境吸收(最大和尾部过境深度为32 \ pm 4%,27 \ pm 4%)和单一晶状体碳(15 \ pm 4%%,12.5 \ pm 4%)。我们表明,大气的含量应少于太阳金属性(在200个bar)的六倍,并且系外行星还必须具有扩展的磁尾(1.8-3.1 au)。 HAT-P-11B赤道磁场强度应约为1-5高斯。我们使用电离物种同时得出金属性和磁场强度的全质方法现在可以限制外部球星的内部和发电机模型,这对形成和进化场景产生了影响。
The magnetosphere of an exoplanet has yet to be unambiguously detected. Investigations of star-planet interaction and neutral atomic hydrogen absorption during transit to detect magnetic fields in hot Jupiters have been inconclusive, and interpretations of the transit absorption non-unique. In contrast, ionized species escaping a magnetized exoplanet, particularly from the polar caps, should populate the magnetosphere, allowing detection of different regions from the plasmasphere to the extended magnetotail, and characterization of the magnetic field producing them. Here, we report ultraviolet observations of HAT-P-11b, a low-mass (0.08 MJ) exoplanet showing strong, phase-extended transit absorption of neutral hydrogen (maximum and tail transit depths of 32 \pm 4%, 27 \pm 4%) and singly ionized carbon (15 \pm 4%, 12.5 \pm 4%). We show that the atmosphere should have less than six times the solar metallicity (at 200 bars), and the exoplanet must also have an extended magnetotail (1.8-3.1 AU). The HAT-P-11b equatorial magnetic field strength should be about 1-5 Gauss. Our panchromatic approach using ionized species to simultaneously derive metallicity and magnetic field strength can now constrain interior and dynamo models of exoplanets, with implications for formation and evolution scenarios.