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下沉的硅酸盐 I:利用JWST表征包含T0褐矮星CWISE J210640.16+250729.0的基准系统

Sinking Silicates I: Characterizing the benchmark system containing the T0 brown dwarf CWISE J210640.16+250729.0 using JWST

Austin Rothermich, Jacqueline K. Faherty, Ben Burningham, Catherine Manea, Emily Calamari, Genaro Suárez, Daniella C. Bardalez Gagliuffi, John M. Brewer, Kelle L. Cruz, Josefine Gaarn, Jonathan Gagné, Eileen C. Gonzales, Marina E. Gemma, Viktória Kecskeméthy, Mark S. Marley, Caprice L. Phillips, Channon Visscher, Johanna M. Vos, Niall Whiteford

arXiv 2609.13433首次发表:更新:

发表机构

American Museum of Natural History; Graduate Center, City University of New York; Hunter College, City University of New York; Backyard Worlds: Planet 9; University of Hertfordshire; University of Utah; Amherst College; San Francisco State University(美国自然历史博物馆; 纽约市立大学研究生中心; 纽约市立大学亨特学院; 后院世界:第九颗行星; 赫特福德大学; 犹他大学; 阿默斯特学院; 旧金山州立大学)

机构由 AI 辅助整理,请以论文原文为准。

AI 中文总结

本研究利用JWST完整表征L/T过渡褐矮星CW2106,推导其基本参数,发现近红外需多云模型而中红外需无云模型,预测云层以顽火辉石为主并移除约23%的体氧。

AI 中文摘要

在本研究中,我们利用詹姆斯·韦布空间望远镜(JWST)展示了L/T过渡天体CWISE J210640.16+250729.0(CW2106)的完整(97.3%完备)0.8–12.5微米光谱能量分布(SED)。我们提供了主星元素丰度和年龄的全面表征。我们经验性地推导了CW2106的辐射光度(L_bol≈-4.825太阳光度),并获得了其质量(M≈50–62木星质量)、半径(R≈0.83–0.87木星半径)、有效温度(T_eff≈1213 K)和表面重力(log g≈5.28 dex)的估计值。我们发现近红外(near-IR)光谱(0.8–2.5微米)最适合用多云大气模型再现,而中红外(mid-IR)光谱(5–12.5微米)最适合用无云模型再现。这表明云层仅限于大气最深层可观测部分,并通过缺乏9微米硅酸盐特征得到证实。利用主星的Mg/Si比以及热化学模型,我们预测CW2106中的云主要由顽火辉石(MgSiO3)组成,从大气中移除了约23%的体氧。未来的反演研究将有助于探究这些云物种的存在及其全部影响。

英文摘要

In this study, we present the full (97.3\% complete) 0.8--12.5 $μ$m spectral energy distribution (SED) of an L/T transition object, CWISE J210640.16+250729.0 (CW2106), using the James Webb Space Telescope (JWST). We provide a full characterization of the host star's elemental abundances and age. We empirically derive the bolometric luminosity ($L_{\rm bol}\approx-4.825$ $\textup{L}_\odot$) of CW2106, and obtain estimates of its mass (M$\approx50-62$ M$_{\rm Jup}$), radius (R$\approx0.83-0.87$ R$_{\rm Jup}$), effective temperature ($T_{\rm eff}$$\approx1213$ K), and surface gravity ($\log~g$$\approx5.28$ dex). We find the near-infrared (near-IR) spectrum ($0.8-2.5 ~μ$m) is best reproduced with cloudy atmospheric models while the mid-infrared (mid-IR) spectrum ($5-12.5 ~μ$m) is best reproduced with cloudless models. This suggests a cloud layer restricted to only the deepest observable parts of the atmosphere and is qualified by the lack of a 9 $μ$m silicate feature. Making use of the Mg/Si ratio of the primary, alongside thermochemical models, we predict the clouds in CW2106 to be composed primarily of enstatite (MgSiO$_3$), removing $\sim23\%$ of the bulk oxygen out of the atmosphere. Future retrieval studies will be able to help investigate the existence and full impact of these cloud species.

Comments30 pages, 12 Figures, 4 Tables. Accepted for publication in ApJ

论文原文

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