Metallicity, planet formation, and disc lifetimes
Barbara Ercolano (1,2), Cathie Clarke (1) (1, Institute of Astronomy,, University of Cambridge UK, 2, University College London, UK)

TL;DR
This paper investigates how metallicity influences disc dispersal and planet formation, using models and observations to distinguish between photoevaporation and planet formation as dominant dispersal mechanisms.
Contribution
It introduces a metallicity-dependent model of disc dispersal, providing a method to differentiate between photoevaporation and planet formation processes.
Findings
Disc lifetime scales as Z^0.52 in photoevaporation models.
Lower metallicity regions show shorter disc lifetimes, supporting photoevaporation.
Higher metallicity favors gas giant formation in core accretion models.
Abstract
The formation of planets within a disc must operate within the time frame of disc dispersal, it is thus crucial to establish what is the dominant process that disperses the gaseous component of discs around young stars. Planet formation itself as well as photoevaporation by energetic radiation from the central young stellar object have been proposed as plausible dispersal mechanisms. [abridged]. In this paper we use the different metallicity dependance of X-ray photoevaporation and planet formation to discriminate between these two processes. We study the effects of metallicity, Z, on the dispersal timescale, t_phot, in the context of a photoevaporation model, by means of detailed thermal calculations of a disc in hydrostatic equilibrium irradiated by EUV and X-ray radiation from the central source. Our models show t_phot \propto Z^0.52 for a pure photoevaporation model. By means of…
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