The Gaia-ESO Survey: Probes of the inner disk abundance gradient
H. R. Jacobson, E. D. Friel, L. Jilkova, L. Magrini, A. Bragaglia, A., Vallenari, M. Tosi, S. Randich, P. Donati, T. Cantat-Gaudin, R. Sordo, R., Smiljanic, J. C. Overbeek, G. Carraro, G. Tautvaisiene, I. San Roman, S., Villanova, D. Geisler, C. Munoz, F. Jimenez-Esteban

TL;DR
This study uses Gaia-ESO Survey data to analyze the metallicity gradient in the inner Galactic disk, finding a consistent gradient of -0.10 dex/kpc and no steepening inside the solar circle, with an observed age-metallicity relation.
Contribution
It provides a larger sample of inner disk open clusters to better characterize the metallicity gradient and its relation to cluster age, challenging previous claims of steepening.
Findings
Inner disk metallicity gradient is -0.10+-0.02 dex/kpc.
No evidence for steepening of the gradient inside the solar circle.
Older clusters tend to have higher metallicity, consistent with chemical evolution models.
Abstract
The nature of the metallicity gradient inside the solar circle (R_GC < 8 kpc) is poorly understood, but studies of Cepheids and a small sample of open clusters suggest that it steepens in the inner disk. We investigate the metallicity gradient of the inner disk using a sample of inner disk open clusters that is three times larger than has previously been studied in the literature to better characterize the gradient in this part of the disk. We used the Gaia-ESO Survey (GES) [Fe/H] values and stellar parameters for stars in 12 open clusters in the inner disk from GES-UVES data. Cluster mean [Fe/H] values were determined based on a membership analysis for each cluster. Where necessary, distances and ages to clusters were determined via comparison to theoretical isochrones. The GES open clusters exhibit a radial metallicity gradient of -0.10+-0.02 dex/kpc, consistent with the gradient…
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