论文标题

在最冷的棕色矮人中观察不平衡的CO化学

Observations of Disequilibrium CO Chemistry in the Coldest Brown Dwarfs

论文作者

Miles, Brittany E., Skemer, Andrew J. I., Morley, Caroline V., Marley, Mark S., Fortney, Jonathan J., Allers, Katelyn N., Faherty, Jacqueline K., Geballe, Thomas R., Visscher, Channon, Schneider, Adam C., Lupu, Roxana, Freedman, Richard S., Bjoraker, Gordon L.

论文摘要

冷褐色矮人是广泛分离的气体巨型系外行星的出色类似物,并洞悉了我们在未来直接成像调查发现的物体中可能遇到的潜在大气化学和物理学。我们提出了低分辨率R $ \ sim $ 300 $ M $ - 带光谱序列的七个棕色矮人,有效温度在750 K至250 K之间,以及木星。这些光谱揭示了大气淬火产生的一氧化碳(CO)的不平衡丰度。我们使用涡流扩散系数(k $ _ {zz} $)来估计每个对象中垂直混合的强度。 k $ _ {zz} $凉爽气体对象的值接近其理论最大对象和温暖的对象的混合较弱,这可能是由于主要在辐射层中效率较低的对流混合而引起的。共同衍生的k $ _ {zz} $值表示在所有棕色矮人中都应该很容易观察到不平衡的磷酸(pH $ _ {3} $),但还没有显示出任何证据表明任何证据表明pH $ _ {3} $吸收。我们发现,在这些有效的温度下,氨对大气淬火相对不敏感。通过在大气模型中包括CO和Water Clouds,我们能够提高WISE 0855的$ M $ band Spectrum的拟合度。

Cold brown dwarfs are excellent analogs of widely separated, gas giant exoplanets, and provide insight into the potential atmospheric chemistry and physics we may encounter in objects discovered by future direct imaging surveys. We present a low resolution R $\sim$ 300 $M$-band spectroscopic sequence of seven brown dwarfs with effective temperatures between 750 K and 250 K along with Jupiter. These spectra reveal disequilibrium abundances of carbon monoxide (CO) produced by atmospheric quenching. We use the eddy diffusion coefficient (K$_{zz}$) to estimate the strength of vertical mixing in each object. The K$_{zz}$ values of cooler gaseous objects are close to their theoretical maximum and warmer objects show weaker mixing, likely due to less efficient convective mixing in primarily radiative layers. The CO-derived K$_{zz}$ values imply that disequilibrium phosphine (PH$_{3}$) should be easily observable in all of the brown dwarfs, but none as yet show any evidence for PH$_{3}$ absorption. We find that ammonia is relatively insensitive to atmospheric quenching at these effective temperatures. We are able to improve the fit to WISE 0855's $M$-band spectrum by including both CO and water clouds in the atmospheric model.

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