MINDS. Hydrocarbons detected by JWST/MIRI in the inner disk of Sz28 consistent with a high C/O gas-phase chemistry

J. Kanwar, I. Kamp, H. Jang, L. Waters, E. V. Dishoeck, V. Christiaens, A. M. Arabhavi, Thomas K. Henning, M. Gudel, P. Woitke, Olivier Absil, D. Barrado, A. C. O. Garatti, A. Glauser, F. Lahuis, S. Scheithauer, B. Vandenbussche, D. Gasman, S. Grant, N. Kurtovic, G. Perotti, B. Tabone, M. Temmink
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Abstract

With the advent of JWST, we are acquiring unprecedented insights into the physical and chemical structure of the inner regions of planet-forming disks where terrestrial planet formation occurs. Very low-mass stars (VLMSs) are known to have a high occurrence of the terrestrial planets orbiting them. Exploring the chemical composition of the gas in these inner disk regions can help us better understand the connection between planet-forming disks and planets. sun We used the dust-fitting tool DuCK to determine the dust continuum and to place constraints on the dust composition and grain sizes. We used 0D slab models to identify and fit the molecular spectral features, which yielded estimates on the temperature, column density, and emitting area. To test our understanding of the chemistry in the disks around VLMSs, we employed the thermo-chemical disk model P RO D I M O and investigated the reservoirs of the detected hydrocarbons. We explored how the C/O ratio affects the inner disk chemistry. JWST reveals a plethora of hydrocarbons, including CH3 CH4 C2H2 CCH2 C2H6 C3H4 C4H2 and C6H6 which suggests a disk with a gaseous C/O\,>\,1. Additionally, we detect CO2 CO2 HCN and HC3N H2O and OH are absent from the spectrum. We do not detect polycyclic aromatic hydrocarbons. Photospheric stellar absorption lines of H2O and CO are identified. Notably, our radiation thermo-chemical disk models are able to produce these detected hydrocarbons in the surface layers of the disk when C/O\,>\,1. The presence of C C+ H, and H2 is crucial for the formation of hydrocarbons in the surface layers, and a C/O ratio larger than 1 ensures the surplus of C needed to drive this chemistry. Based on this, we predict a list of additional hydrocarbons that should also be detectable. Both amorphous and crystalline silicates (enstatite and forsterite) are present in the disk and we find grain sizes of 2 and 5\,mu m. The disk around Sz28 is rich in hydrocarbons, and its inner regions have a high gaseous C/O ratio. In contrast, it is the first VLMS disk in the MINDS sample to show both distinctive dust features and a rich hydrocarbon chemistry. The presence of large grains indicates dust growth and evolution. Thermo-chemical disk models that employ an extended hydrocarbon chemical network together with C/O\,>1 are able to explain the hydrocarbon species detected in the spectrum.
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MINDS.JWST/MIRI 在 Sz28 内盘探测到的碳氢化合物与高 C/O 气相化学相一致
随着 JWST 的问世,我们对行星形成盘内部区域的物理和化学结构有了前所未有的深入了解。众所周知,超低质量恒星(VLMSs)中有大量的类地行星围绕它们运行。探索这些内盘区域气体的化学成分有助于我们更好地理解行星形成盘与行星之间的联系。 我们使用尘埃拟合工具 DuCK 来确定尘埃连续面,并对尘埃成分和粒度进行约束。我们使用 0D 板坯模型来识别和拟合分子光谱特征,从而对温度、柱密度和发射区域做出估计。为了检验我们对 VLMSs 周围磁盘化学性质的理解,我们使用了热化学磁盘模型 P RO D I M O,并对探测到的碳氢化合物的储层进行了研究。我们探讨了C/O比如何影响内盘化学。JWST发现了大量碳氢化合物,包括CH3 CH4 C2H2 CCH2 C2H6 C3H4 C4H2和C6H6。此外,我们还探测到 CO2 CO2 HCN 和 HC3N H2O,光谱中没有 OH。我们没有探测到多环芳烃。光层恒星吸收线 H2O 和 CO 被识别出来。值得注意的是,当C/O\,>\,1时,我们的辐射热化学盘模型能够在盘的表层产生这些探测到的碳氢化合物。C C+ H和H2的存在对于表层碳氢化合物的形成至关重要,而大于1的C/O比确保了驱动这种化学反应所需的过剩C。在此基础上,我们预测了一系列也应该可以检测到的其他碳氢化合物。Sz28周围的圆盘富含碳氢化合物,其内部区域具有较高的气态C/O比。相比之下,它是MINDS样本中第一个同时显示出独特的尘埃特征和丰富的碳氢化合物化学成分的VLMS盘。大颗粒的存在表明了尘埃的生长和演化。采用扩展碳氢化合物化学网络和 C/O(>1)的热化学盘模型能够解释光谱中探测到的碳氢化合物种类。
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