The innate origin of radial and vertical gradients in a simulated galaxy disc

TL;DR

This study shows that radial and vertical gradients in a simulated galaxy disc originate from the initial conditions and evolution of the gaseous disc, rather than from secular processes like spiral arms or bars.

Contribution

It demonstrates that gradients in galaxy discs can be explained by gas disc evolution and feedback, challenging the idea that secular processes are the primary cause.

Findings

Gradients arise from gaseous disc enrichment and thinning.

Stars' kinematics reflect initial formation conditions.

Gradients are not primarily due to secular evolution.

Abstract

We examine the origin of radial and vertical gradients in the age/metallicity of the stellar component of a galaxy disc formed in the APOSTLE cosmological hydrody- namical simulations. Some of these gradients resemble those in the Milky Way, where they have sometimes been interpreted as due to internal evolution, such as scattering off giant molecular clouds, radial migration driven by spiral patterns, or orbital reso- nances with a bar. Secular processes play a minor role in the simulated galaxy, which lacks strong spiral or bar patterns, and where such gradients arise as a result of the gradual enrichment of a gaseous disc that is born thick but thins as it turns into stars and settles into centrifugal equilibrium. The settling is controlled by the feedback of young stars; which links the star formation, enrichment, and equilibration timescales, inducing radial and vertical gradients in the gaseous disc and its descendent stars. The kinematics of coeval stars evolve little after birth and provide a faithful snapshot of the gaseous disc structure at the time of their formation. In this interpretation, the age-velocity dispersion relation would reflect the gradual thinning of the disc rather than the importance of secular orbit scattering; the outward flaring of stars would result from the gas disc flare rather than from radial migration; and vertical gradients would arise because the gas disc gradually thinned as it enriched. Such radial and vertical trends might just reflect the evolving properties of the parent gaseous disc, and are not necessarily the result of secular evolutionary processes.