Chemistry Along Accretion Streams in a Viscously-Evolving Protoplanetary Disk
arXiv:2002.04651 · doi:10.3847/1538-4357/ab5fd4
Abstract
The composition of a protoplanetary disk is set by a combination of interstellar inheritance and gas and grain surface chemical reactions within the disk. The survival of inherited molecules, as well as the disk in situ chemistry depends on the local temperature, density and irradiation environment, which can change over time due to stellar and disk evolution, as well as transport in the disk. We address one aspect of this coupling between the physical and chemical evolution in disks by following accretion streamlines of gas and small grains in the disk midplane, while simultaneously taking the evolving star into account. This approach is computationally efficient and enables us to take into account changing physical conditions without reducing the chemical network. We find that many species are enhanced in the inner disk midplane in the dynamic model due to inward transport of cosmic-ray driven chemical products, resulting in, e.g., orders-of magnitude hydrocarbon enhancements at 1 au, compared to a static disk. For several other chemical families, there is no difference between the static and dynamic models, indicative of a robust chemical reset, while yet others show differences between static and dynamic models that depend on complex interactions between physics and chemistry during the inward track. The importance of coupling dynamics and chemistry when modeling the chemical evolution of protoplanetary disks is thus depends on what chemistry is of interest.
Accepted for publication in ApJ
References in corpus (10)
- The ancient heritage of water ice in the solar system
- The cometary composition of a protoplanetary disk as revealed by complex cyanides
- H2O and OH gas in the terrestrial planet-forming zones of protoplanetary disks
- Setting the volatile composition of (exo)planet-building material. Does chemical evolution in disk midplanes matter?
- Composition of Early Planetary Atmospheres I: Connecting Disk Astrochemistry to the Formation of Planetary Atmospheres
- Gas-phase CO in protoplanetary disks: a challenge for turbulent mixing
- Exclusion of Cosmic Rays in Protoplanetary Disks. II. Chemical Gradients and Observational Signatures
- Turbulence driven diffusion in protoplanetary disks - chemical effects in the outer disk
- Dynamics and Accretion of Planetesimals
- Effects of accretion flow on the chemical structure in the inner regions of protoplanetary disks