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The atmospheric evolution of small, close-in exoplanets
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Rogers-J-2022-PhD-Thesis.pdf | Thesis | 32.01 MB | Adobe PDF | View/Open |
Title: | The atmospheric evolution of small, close-in exoplanets |
Authors: | Rogers, James |
Item Type: | Thesis or dissertation |
Abstract: | The results from the Kepler space observatory have revealed a wealth of planets with small sizes and small orbital separations, referred to as “super-Earths” or “sub-Neptunes”. This thesis will focus on such planets. Atmospheres of super-Earths/sub-Neptunes are vulnerable to hydrodynamic escape due to the proximity to their host stars. I begin by comparing two mechanisms by which this can occur: photoevaporation, which is caused by high energy radiation from the host star; and core-powered mass-loss, which relies on the stellar bolometric luminosity in conjunction with the cooling luminosity from the planetary core. I construct a robust statistical test that can be performed on future exoplanet surveys in order to determine which of these mechanisms is dominant. I then go on to show that if one takes the population of exoplanets observed today, one can rewind the clock on atmospheric evolution to infer the planet properties at birth. I perform this with photoevaporation models to place constraints on planetary properties that are currently unobservable with standard techniques. I find that a typical super-Earth/sub-Neptune has a core mass of ∼ 4M⊕, a core composition consistent with that of Earth and an initial atmospheric mass fraction after protoplanetary disc dispersal of ∼ 2%. This latter result highlights a discrepancy between atmospheric mass-loss and gas accretion models, the latter of which predicts initial atmospheric masses ≳ 10%. I perform sophisticated evolution models of planets immersed in protoplanetary discs that self-consistently model gas accretion and mass-loss induced by rapid disc dispersal. I find that this mechanism efficiently removes atmospheric mass and provides a robust solution to the aforementioned discrepancy. This mass-loss phase induces rapid contraction and advection of high entropy material into the escaping atmosphere. This process, which I find is strongly controlled by the disc dispersal rate, produces a planet that has prematurely cooled, given its age. |
Content Version: | Open Access |
Issue Date: | Jul-2022 |
Date Awarded: | Oct-2022 |
URI: | http://hdl.handle.net/10044/1/100382 |
DOI: | https://doi.org/10.25560/100382 |
Copyright Statement: | Creative Commons Attribution NonCommercial NoDerivatives Licence |
Supervisor: | Owen, James |
Department: | Physics |
Publisher: | Imperial College London |
Qualification Level: | Doctoral |
Qualification Name: | Doctor of Philosophy (PhD) |
Appears in Collections: | Physics PhD theses |
This item is licensed under a Creative Commons License