Smuggling unnoticed: Towards a 2D view of water and dust delivery to the inner regions of protoplanetary discs

Fuente: arXiv
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Houge, Adrien, Krijt, Sebastiaan, Banzatti, Andrea, Blake, Geoffrey A., Pinilla, Paola, Pontoppidan, Klaus M., Trapman, Leon, Williams, Joe, Zhang, Ke
Format: Preprint
Publié: 2025
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1866913643601330176
author Houge, Adrien
Krijt, Sebastiaan
Banzatti, Andrea
Blake, Geoffrey A.
Pinilla, Paola
Pontoppidan, Klaus M.
Trapman, Leon
Williams, Joe
Zhang, Ke
author_facet Houge, Adrien
Krijt, Sebastiaan
Banzatti, Andrea
Blake, Geoffrey A.
Pinilla, Paola
Pontoppidan, Klaus M.
Trapman, Leon
Williams, Joe
Zhang, Ke
contents Infrared spectroscopy, e.g., with JWST, provides a glimpse into the chemical inventory of the innermost region of protoplanetary discs, where terrestrial planets eventually form. The chemical make-up of regions inside snowlines is connected to the material drifting from the outer regions, which can be modeled with dust evolution models. However, infrared observations are limited by the high dust extinction in the inner disc, and only probes the abundances of gaseous species in the disc surface layers. As a result, the bulk mass of delivered volatiles is not directly relatable to what is measured through infrared spectra. In this paper, we investigate how the delivery of dust and ice after prolonged pebble drift affects the observable reservoir of water vapor in the inner disc. We develop a 1+1D approach based on dust evolution models to determine the delivery and distribution of vapor compared to the height of the $τ= 1$ surface in the dust continuum. We find that the observable column density of water vapor at wavelengths probed by JWST spans many orders of magnitude over time, exhibiting different radial profiles depending on dust properties, drift rate, and local processing. In the presence of a traffic-jam effect inside the snowline, the observable vapor reservoir appears constant in time despite the ongoing delivery by pebble drift, such that water is effectively smuggled unnoticed. Differences in measured column densities then originate not only from variations in bulk vapor content, but also from differences in the properties and distribution of dust particles.
format Preprint
id arxiv_https___arxiv_org_abs_2501_05881
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Smuggling unnoticed: Towards a 2D view of water and dust delivery to the inner regions of protoplanetary discs
Houge, Adrien
Krijt, Sebastiaan
Banzatti, Andrea
Blake, Geoffrey A.
Pinilla, Paola
Pontoppidan, Klaus M.
Trapman, Leon
Williams, Joe
Zhang, Ke
Earth and Planetary Astrophysics
Infrared spectroscopy, e.g., with JWST, provides a glimpse into the chemical inventory of the innermost region of protoplanetary discs, where terrestrial planets eventually form. The chemical make-up of regions inside snowlines is connected to the material drifting from the outer regions, which can be modeled with dust evolution models. However, infrared observations are limited by the high dust extinction in the inner disc, and only probes the abundances of gaseous species in the disc surface layers. As a result, the bulk mass of delivered volatiles is not directly relatable to what is measured through infrared spectra. In this paper, we investigate how the delivery of dust and ice after prolonged pebble drift affects the observable reservoir of water vapor in the inner disc. We develop a 1+1D approach based on dust evolution models to determine the delivery and distribution of vapor compared to the height of the $τ= 1$ surface in the dust continuum. We find that the observable column density of water vapor at wavelengths probed by JWST spans many orders of magnitude over time, exhibiting different radial profiles depending on dust properties, drift rate, and local processing. In the presence of a traffic-jam effect inside the snowline, the observable vapor reservoir appears constant in time despite the ongoing delivery by pebble drift, such that water is effectively smuggled unnoticed. Differences in measured column densities then originate not only from variations in bulk vapor content, but also from differences in the properties and distribution of dust particles.
title Smuggling unnoticed: Towards a 2D view of water and dust delivery to the inner regions of protoplanetary discs
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2501.05881