Spatially resolving the volatile sulfur abundance in the HD 100546 protoplanetary disc

Keyte, Luke; Kama, Mihkel; Chuang, Ko-Ju; Cleeves, L Ilsedore; Drozdovskaya, Maria N.; Furuya, Kenji; Rawlings, Jonathan; Shorttle, Oliver (2024). Spatially resolving the volatile sulfur abundance in the HD 100546 protoplanetary disc. Monthly Notices of the Royal Astronomical Society, 528(1), pp. 388-407. Oxford University Press 10.1093/mnras/stae019

[img]
Preview
Text
stae019.pdf - Published Version
Available under License Creative Commons: Attribution (CC-BY).

Download (3MB) | Preview

Volatile elements play a crucial role in the formation of planetary systems. Their abundance and distribution in protoplanetary discs provide vital insights into the connection between formation processes and the atmospheric composition of individual planets. Sulfur, being one of the most abundant elements in planet-forming environments, is of great significance, and now observable in exoplanets with JWST. However, planetary formation models currently lack vital knowledge regarding sulfur chemistry in protoplanetary discs. Developing a deeper understanding of the major volatile sulfur carriers in discs is essential to building models that can meaningfully predict planetary atmospheric composition, and reconstruct planetary formation pathways. In this work, we combine archival observations with new data from the Atacama Large sub-Millimeter Array (ALMA) and the Atacama Pathfinder EXperiment (APEX), covering a range of sulfur-bearing species/isotopologs. We interpret this data using the DALI thermo-chemical code, for which our model is highly refined and disc-specific. We find that volatile sulfur is heavily depleted from the cosmic value by a factor of ∼1000, with a disc-averaged abundance of S/H ∼ 10−8. We show that the gas-phase sulfur abundance varies radially by ≳3 orders of magnitude, with the highest abundances inside the inner dust ring and coincident with the outer dust ring at r ∼ 150–230 au. Extracting chemical abundances from our models, we find OCS, H2CS, and CS to be the dominant molecular carriers in the gas phase. We also infer the presence of a substantial OCS ice reservoir. We relate our results to the potential atmospheric composition of planets in HD 100546, and the wider exoplanet population.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Physics Institute > Space Research and Planetary Sciences
08 Faculty of Science > Physics Institute
10 Strategic Research Centers > Center for Space and Habitability (CSH)
08 Faculty of Science > Physics Institute > NCCR PlanetS

UniBE Contributor:

Drozdovskaya, Maria Nikolayevna

Subjects:

500 Science > 520 Astronomy
500 Science
500 Science > 530 Physics

ISSN:

0035-8711

Publisher:

Oxford University Press

Language:

English

Submitter:

Danielle Zemp

Date Deposited:

04 Apr 2024 12:18

Last Modified:

04 Apr 2024 12:18

Publisher DOI:

10.1093/mnras/stae019

BORIS DOI:

10.48350/195537

URI:

https://boris.unibe.ch/id/eprint/195537

Actions (login required)

Edit item Edit item
Provide Feedback