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arXiv 2402.09342astro-ph.EP
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通过内部光致蒸发改变盘成分 I:太阳质量恒星

Changing disc compositions via internal photoevaporation I: Solar-mass stars

Julia Lena Lienert, Bertram Bitsch, Thomas Henning

AI总结:

本文利用半解析一维盘模型chemcomp研究内部光致蒸发对类太阳恒星原行星盘化学演化的影响,发现光致蒸发打开间隙会阻挡向内漂移的卵石并带走外盘气体,导致内盘C/O比偏低而水含量升高,从而可与巨行星开隙情形在观测上加以区分。

摘要:

原行星盘的化学演化尚未被完全理解,若干因素影响着盘物质的最终分布。其中一个因素是向内漂移并蒸发的卵石,它们以蒸气形式富集内盘。特别是,内盘首先被水蒸气富集,导致较低的C/O比,随后来自外盘的富碳气体向内输运,再次抬升C/O比。然而,目前尚不清楚内部光致蒸发——它会带走气体并打开间隙以阻挡向内漂移的卵石——如何影响盘的化学成分。我们旨在研究类太阳恒星周围盘中的这些效应,尤其关注C/O比和水含量。模拟使用半解析一维盘模型进行。我们的代码chemcomp包括粘性演化和加热、卵石生长与漂移、卵石蒸发与凝结,以及一个简单的化学分配模型。我们表明,内部光致蒸发在原行星盘的(化学)演化中起主要作用:当它打开间隙时,向内漂移的卵石被阻止,无法再对挥发物含量作出贡献。此外,来自外盘的气体被光致蒸发风带走。因此,内盘的C/O比较低。相比之下,巨行星打开的间隙允许气体通过,导致C/O比升高,类似于没有内部光致蒸发的粘性盘。这将使我们能够在观测上区分这两种情形——当测量C/O比时,意味着我们可以从盘的观测中推断间隙结构的成因。在光致蒸发盘的情形下,我们还发现内盘水含量升高,因为水蒸气和冰经历蒸发/再凝结的循环,阻止其向内吸积到恒星上。

英文摘要:

The chemical evolution of protoplanetary discs is not fully understood, several factors influence the final distribution of disc material. One such factor are inward drifting and evaporating pebbles that enrich the inner disc with vapour. In particular, it is first enriched with water vapour, resulting in a low C/O ratio, before carbon-rich gas from the outer disc is transported inwards elevating the C/O ratio again. However, it is unclear how internal photoevaporation, which carries away gas and opens gaps that block inward drifting pebbles, affects the chemical composition of the disc. We aim to study these effects in discs around solar-like stars, where we especially focus on the C/O ratio and the water content. The simulations are carried out using a semi-analytical 1D disc model. Our code chemcomp includes viscous evolution and heating, pebble growth and drift, pebble evaporation and condensation, and a simple chemical partitioning model. We show that internal photoevaporation plays a major role in the (chemical) evolution of protoplanetary discs: As it opens a gap, inward drifting pebbles are stopped and cannot contribute to the volatile content any more. In addition, gas from the outer disc is carried away by photoevaporative winds. Consequently, the C/O ratio in the inner disc is low. In contrast, gaps opened by giant planets allow the gas to pass, resulting in an elevated C/O ratio, similar to viscous discs without internal photoevaporation. This will enable us to distinguish observationally between these two scenarios when measuring the C/O ratio, implying that we can infer the cause of gap structures in disc observations. In the case of a photoevaporative disc, we additionally find an elevated water content in the inner disc as the water vapour and ice undergo a cycle of evaporation/re-condensation, preventing its inward accretion onto the star.

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