Chemistry on solar system scales
Abstract
The initial chemical composition of planets, primitive bodies in our solar system, and exoplanets is ultimately set by their nascent protoplanetary disks. Yet observing key carbon-, oxygen-, and nitrogen-bearing molecules (as well as rarer but important sulphur- and phosphorus-bearing species) in the inner (exo)planet-forming zone (≲ 10~au) remains extremely challenging with current facilities. Therefore, to construct a complete picture of the chemistry of planet formation and understand how (exo)planetary composition is set by physical and chemical processes within the protoplanetary disk, a more powerful observing facility, i.e., ALMA2040, is needed. Compared to current ALMA (the Atacama Large Millimeter/submillimeter Array) this new facility must provide >~ a factor of 10 in line sensitivity at a spatial resolution of <~ 5 au at 140 pc, i.e., a factor of 3 - 4 better resolution to low surface brightness emission than currently possible. This distance includes many star-forming regions such as Taurus and Lupus that are host to populations of Sun-like stars. ALMA2040 will enable mapping of disk chemical composition on terrestrial planet-forming scales (within the water snowline) and detect molecules that are the feedstock for potentially habitable worlds.
Related
- Planet formation on solar system scales
- TEMPUS: Relativistic coordinate time scales for any solar-system body from arbitrary ephemerides
- SoFTg: A hybrid segmentation framework for solar granulation revealing turbulent convection statistics at DKIST scales
- The spatial structure of solar magnetoconvection at scales up to $60$~Mm
- Editorial: Dynamic exospheres of terrestrial bodies through the solar system
BibTeX
@misc{walsh2026chemistry,
title = {{Chemistry on solar system scales}},
author = {Catherine Walsh and Maria Drozdovskaya and Dmitry Semenov and Alice Booth and Margot Leemker and Eleonora Bianchi and Pooneh Nazari and Linda Podio and Claudio Codella and Giovanni Sabatini and Elenia Pacetti and Diego Turrini and Danae Polychroni and Myriam Benisty and Claudia Toci and Marta De Simone and Víctor Rivilla and Enrique Macias and Luna Rampinelli and Beatrice Kulterer and Claudio Hernández-Vera and Laura Colzi and Hideko Nomura and Maxime Tanious and Ian Czekala and Shota Notsu and Quentin Kral and Charles Law and Liton Majumdar and Stefano Facchini and Jenny Frediani and Sebastiaan Krijt and Teresa Paneque-Carreño and Ágnes Kóspál and Sébastien Maret and Gianni Cataldi},
howpublished = {arXiv},
year = {2026},
month = oct,
doi = {10.48550/arxiv.2610.22055},
eprint = {2610.22055},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2610.22055},
note = {CC BY 4.0},
}
RIS
TY - UNPB
TI - Chemistry on solar system scales
AU - Catherine Walsh
AU - Maria Drozdovskaya
AU - Dmitry Semenov
AU - Alice Booth
AU - Margot Leemker
AU - Eleonora Bianchi
AU - Pooneh Nazari
AU - Linda Podio
AU - Claudio Codella
AU - Giovanni Sabatini
AU - Elenia Pacetti
AU - Diego Turrini
AU - Danae Polychroni
AU - Myriam Benisty
AU - Claudia Toci
AU - Marta De Simone
AU - Víctor Rivilla
AU - Enrique Macias
AU - Luna Rampinelli
AU - Beatrice Kulterer
AU - Claudio Hernández-Vera
AU - Laura Colzi
AU - Hideko Nomura
AU - Maxime Tanious
AU - Ian Czekala
AU - Shota Notsu
AU - Quentin Kral
AU - Charles Law
AU - Liton Majumdar
AU - Stefano Facchini
AU - Jenny Frediani
AU - Sebastiaan Krijt
AU - Teresa Paneque-Carreño
AU - Ágnes Kóspál
AU - Sébastien Maret
AU - Gianni Cataldi
PY - 2026
DA - 2026/10/15
PB - arXiv
DO - 10.48550/arxiv.2610.22055
UR - https://arxiv.org/abs/2610.22055
AB - The initial chemical composition of planets, primitive bodies in our solar system, and exoplanets is ultimately set by their nascent protoplanetary disks. Yet observing key carbon-, oxygen-, and nitrogen-bearing molecules (as well as rarer but important sulphur- and phosphorus-bearing species) in the inner (exo)planet-forming zone (≲ 10~au) remains extremely challenging with current facilities. Therefore, to construct a complete picture of the chemistry of planet formation and understand how (exo)planetary composition is set by physical and chemical processes within the protoplanetary disk, a more powerful observing facility, i.e., ALMA2040, is needed. Compared to current ALMA (the Atacama Large Millimeter/submillimeter Array) this new facility must provide >~ a factor of 10 in line sensitivity at a spatial resolution of <~ 5 au at 140 pc, i.e., a factor of 3 - 4 better resolution to low surface brightness emission than currently possible. This distance includes many star-forming regions such as Taurus and Lupus that are host to populations of Sun-like stars. ALMA2040 will enable mapping of disk chemical composition on terrestrial planet-forming scales (within the water snowline) and detect molecules that are the feedstock for potentially habitable worlds.
ER -