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nIFTy galaxy cluster simulations–V. Investigation of the cluster infall region

Authors

Jake Arthur, Frazer R Pearce, Meghan E Gray, Pascal J Elahi, Alexander Knebe, Alexander M Beck, Weiguang Cui, Daniel Cunnama, Romeel Davé, Sean February, Shuiyao Huang, Neal Katz, Scott T Kay, Ian G McCarthy, Giuseppe Murante, Valentin Perret, Chris Power, Ewald Puchwein, Alexandro Saro, Federico Sembolini, Romain Teyssier, Gustavo Yepes

Journal Paper

https://doi.org/10.1093/mnras/stw2424

Publisher URL

https://academic.oup.com/mnras

Publication date

September 2016

We examine the properties of the galaxies and dark matter haloes residing in the cluster infall region surrounding the simulated Λ cold dark matter galaxy cluster studied by Elahi et al. at z = 0. The 1.1 × 1015h−1 M galaxy cluster has been simulated with eight different hydrodynamical codes containing a variety of hydrodynamic solvers and sub-grid schemes. All models completed a dark-matter-only, non-radiative and full-physics run from the same initial conditions. The simulations contain dark matter and gas with mass resolution mDM = 9.01 × 108h−1 M and mgas = 1.9 × 108h−1 M, respectively. We find that the synthetic cluster is surrounded by clear filamentary structures that contain ∼60 per cent of haloes in the infall region with mass ∼1012.5–1014h−1 M, including 2–3 group-sized haloes (>1013h−1 M). However, we find that only ∼10 per cent of objects in the infall region are sub-haloes residing in haloes, which may suggest that there is not much ongoing pre-processing occurring in the infall region at z = 0. By examining the baryonic content contained within the haloes, we also show that the code-to-code scatter in stellar fraction across all halo masses is typically ∼2 orders of magnitude between the two most extreme cases, and this is predominantly due to the differences in sub-grid schemes and calibration procedures that each model uses. Models that do not include active galactic nucleus feedback typically produce too high stellar fractions compared to observations by at least ∼1 order of magnitude.