Changing disc compositions via internal photoevaporation I: Solar-mass stars
arXiv:2402.09342 · doi:10.1051/0004-6361/202348798
Abstract
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.
References in corpus (56)
- The chemical composition of the Sun
- The Disk Substructures at High Angular Resolution Project (DSHARP): I. Motivation, Sample, Calibration, and Overview
- The effects of snowlines on C/O in planetary atmospheres
- Towards a Deterministic Model of Planetary Formation I: a Desert in the Mass and Semi Major Axis Distributions of Extra Solar Planets
- A simple model for the evolution of the dust population in protoplanetary disks
- Passive irradiated circumstellar disks with an inner hole
- Coagulation, fragmentation and radial motion of solid particles in protoplanetary disks
- Flaring vs. self-shadowed disks: the SEDs of Herbig Ae/Be stars
- X-Shooter spectroscopy of young stellar objects in Lupus: Accretion properties of class II and transitional objects
- Separating gas-giant and ice-giant planets by halting pebble accretion
- Timescale of Mass Accretion in Pre-Main-Sequence Stars
- The imprint of exoplanet formation history on observable present-day spectra of hot Jupiters
- Trapping dust particles in the outer regions of protoplanetary disks
- The GALAH Survey: Second Data Release
- The stickiness of micrometer-sized water-ice particles
- On the theory of disc photoevaporation
- Pebble isolation mass --- scaling law and implications for the formation of super-Earths and gas giants
- Chemical enrichment of giant planets and discs due to pebble drift
- Dust flow in gas disks in the presence of embedded planets
- The New Generation Planetary Population Synthesis (NGPPS). I. Bern global model of planet formation and evolution, model tests, and emerging planetary systems
- Contacts of Water Ice in Protoplanetary Disks - Laboratory Experiments
- A solar C/O and sub-solar metallicity in a hot Jupiter atmosphere
- Formation of planetary systems by pebble accretion and migration: Growth of gas giants
- X-ray irradiated protoplanetary disk atmospheres II: Predictions from models in hydrostatic equilibrium
- How drifting and evaporating pebbles shape giant planets I: Heavy element content and atmospheric C/O
- Dust retention in protoplanetary disks
- Evidence for Disk Photoevaporation Driven by the Central Star
- The dispersal of protoplanetary discs I: A new generation of X-ray photoevaporation models
- Planet-forming material in a protoplanetary disc: the interplay between chemical evolution and pebble drift
- Metallicity, planet formation, and disc lifetimes
- How much does turbulence change the pebble isolation mass for planet formation?
- Super-Earth masses sculpted by pebble isolation around stars of different masses
- Mass-radius relationships for irradiated ocean planets
- C/O and Snowline Locations in Protoplanetary Disks: The Effect of Radial Drift and Viscous Gas Accretion
- Where is the Water? Jupiter-like C/H ratio but strong HO depletion found on Boötis b using SPIRou
- MINDS. The detection of CO with JWST-MIRI indicates abundant CO in a protoplanetary disk
- Planet population synthesis driven by pebble accretion in cluster environments
- Water in the terrestrial planet-forming zone of the PDS 70 disk
- Determination of the minimum masses of heavy elements in the envelopes of Jupiter and Saturn
- Characterizing the variable dust permeability of planet-induced gaps
- Planetary population synthesis
- How drifting and evaporating pebbles shape giant planets II: Volatiles and refractories in atmospheres
- Influence of sub- and super-solar metallicities on the compositions of solid planetary building blocks
- The dispersal of protoplanetary discs. II: Photoevaporation models with observationally derived irradiating spectra
- MINDS. Abundant water and varying C/O across the disk of Sz 98 as seen by JWST/MIRI
- Close-in ice lines and the super-stellar C/O ratio in discs around very low-mass stars
- Dry or water world? How the water contents of inner sub-Neptunes constrain giant planet formation and the location of the water ice line
- Exploring the conditions for forming cold gas giants through planetesimal accretion
- Characterising thermal sweeping: a rapid disc dispersal mechanism
- The role of planetesimal fragmentation on giant planet formation
- How drifting and evaporating pebbles shape giant planets III: The formation of WASP-77A b and Boötis b
- Enriching inner discs and giant planets with heavy elements
- Chemical evolution in ices on drifting, planet-forming pebbles
- Forming super-Mercuries: The role of stellar abundances
- How the origin of stars in the Galaxy impacts the composition of planetary building blocks
- Influence of grain sizes and composition on the contraction rates of planetary envelopes and on planetary migration
Cited by in corpus (10)
- CO2-rich protoplanetary discs as a probe of dust radial drift & trapping
- Burned to ashes: How the thermal decomposition of refractory organics in the inner protoplanetary disc impacts the gas-phase C/O ratio
- MINDS. JWST-MIRI reveals a peculiar CO-rich chemistry in the drift-dominated disk CX Tau
- Chemical transformation of CO in evolving protoplanetary discs across stellar masses: a route to C-rich inner regions
- There is no disk mass budget problem of planet formation
- How external photo-evaporation changes the chemical composition of the inner disc
- Changing disc compositions via internal photoevaporation II: M dwarf systems
- How disc initial conditions sculpt the atmospheric composition of giant planets
- Timescales diagnostics for saving viscous and MHD-driven dusty discs from external photoevaporation
- How leaky? A large parameter study of leaky dust traps to quantify the transport of pebbles and ice in protoplanetary discs