2017
DOI: 10.1017/s1743921317009802
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Abstract: Connecting the observed composition of exoplanets to their formation sites often involves comparing the atmospheric C/O ratio to a disk midplane model with a fixed chemical composition. In this scenario chemistry during the planet formation era is not considered. However, kinetic chemical evolution during the lifetime of the gaseous disk can change the relative abundances of volatile species, thus altering the C/O ratios of planetary building blocks. In our chemical evolition models we utilize a large network … Show more

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“…4. However, chemical models require the presence of an icy midplane in order to efficiently lock C and O in less volatile species (see e.g., Eistrup et al 2016Eistrup et al , 2018Bosman et al 2017Bosman et al , 2018. Compact disk models are however generally warmer and the reservoir of frozen molecular material is reduced compared to extended disk models (see Fig.…”
Section: Discussionmentioning
confidence: 99%
“…4. However, chemical models require the presence of an icy midplane in order to efficiently lock C and O in less volatile species (see e.g., Eistrup et al 2016Eistrup et al , 2018Bosman et al 2017Bosman et al , 2018. Compact disk models are however generally warmer and the reservoir of frozen molecular material is reduced compared to extended disk models (see Fig.…”
Section: Discussionmentioning
confidence: 99%