Abstract

ABSTRACT While phase equilibria at conditions on Pluto’s surface have been studied, the fate of the equilibria in the lower atmosphere as the altitude increases has not. In this study, the gravitational effect is included in the thermodynamic modelling so that not only the deposition point can be located, but also the vertical pressure and density profiles below the deposition point can be determined, along with the corresponding compositional profiles in the equilibrium phases. The non-ideality of vapour-solid phase equilibria at low pressures and temperatures is also discussed for Pluto’s applications to allow for more accurate calculations if a conventional method, such as modified Raoult’s law, is used.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.