The First JWST View of a 30-Myr-old Protoplanetary Disk Reveals a Late-stage Carbon-rich Phase

Feng Long, 凤 龙, Ilaria Pascucci, Adrien Houge, Andrea Banzatti, Klaus M. Pontoppidan, Joan Najita, Sebastiaan Krijt, Chengyan Xie, Joe Williams, Gregory J. Herczeg, 雷歌 沈, Sean M. Andrews, Edwin Bergin, Geoffrey A. Blake, María José Colmenares, Daniel Harsono, Carlos E. Romero-Mirza, Rixin Li, 日新 李, Cicero X. Lu, Paola Pinilla, David J. Wilner, Miguel Vioque, Ke Zhang and the JDISCS collaboration
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Abstract

We present a JWST MIRI/MRS spectrum of the inner disk of WISE J044634.16–262756.1B (hereafter J0446B), an old (∼34 Myr) M4.5 star but with hints of ongoing accretion. The spectrum is molecule-rich and dominated by hydrocarbons. We detect 14 molecular species (H2, CH3, CH4, C2H2, 13CCH2, C2H4, C2H6, C3H4, C4H2, C6H6, HCN, HC3N, CO2, and 13CO2) and two atomic lines ([Ne ii] and [Ar ii]), all observed for the first time in a disk at this age. The detection of spatially unresolved H2 and Ne gas strongly supports that J0446B hosts a long-lived primordial disk, rather than a debris disk. The marginal H2O detection and the high C2H2/CO2 column density ratio indicate that the inner disk of J0446B has a very carbon-rich chemistry, with a gas-phase C/O ratio ≳2, consistent with what has been found in most primordial disks around similarly low-mass stars. In the absence of significant outer disk dust substructures, inner disks are expected to first become water-rich due to the rapid inward drift of icy pebbles and evolve into carbon-rich as outer disk gas flows inward on longer timescales. The faint millimeter emission in such low-mass star disks implies that they may have depleted their outer icy pebble reservoir early and already passed the water-rich phase. Models with pebble drift and volatile transport suggest that maintaining a carbon-rich chemistry for tens of Myr likely requires a slowly evolving disk with α-viscosity ≲10−4. This study represents the first detailed characterization of disk gas at ∼30 Myr, strongly motivating further studies into the final stages of disk evolution.
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JWST首次观测到的30迈的原行星盘揭示了一个晚期的富碳阶段
我们展示了WISE J044634.16-262756.1B(以下简称J0446B)内盘的JWST MIRI/MRS光谱,这是一颗古老的(~ 34 Myr) M4.5恒星,但有持续吸积的迹象。光谱中分子丰富,以碳氢化合物为主。我们检测到14种分子(H2、CH3、CH4、C2H2、13CCH2、C2H4、C2H6、C3H4、C4H2、C6H6、HCN、HC3N、CO2和13CO2)和2条原子线([Ne ii]和[Ar ii]),这些都是在这个年龄的磁盘中首次观察到的。探测到空间上无法解析的H2和Ne气体有力地支持了J0446B拥有一个长寿的原始盘,而不是一个碎片盘。边际H2O检测和高C2H2/CO2柱密度比表明,J0446B的内盘具有非常富碳的化学成分,气相C/O比值为> 2,与大多数类似低质量恒星周围的原始盘的发现一致。在没有重要的外盘尘埃亚结构的情况下,由于冰冷的鹅卵石迅速向内漂移,预计内盘首先会变得富含水,并随着外盘气体在更长的时间尺度上向内流动而演变成富含碳。这种低质量恒星盘中微弱的毫米辐射表明,它们可能很早就耗尽了外层的冰卵石储集层,并且已经度过了富水阶段。具有卵石漂移和挥发性输运的模型表明,维持几十Myr的富碳化学可能需要一个α-粘度> 10−4的缓慢演化的圆盘。这项研究首次详细描述了~ 30 Myr的盘状气体,有力地推动了对盘状气体演化最后阶段的进一步研究。
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