2017
DOI: 10.1017/s1743921317009802
View full text
|
|

Abstract: AbstractConnecting 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 … Show more

Help me understand this page

Search citation statements

Order By: Relevance

Paper Sections

0
0
0
0
0

Citation Types

0
0
0

Publication Types

Select...

Relationship

0
0

Authors

Journals