2011MNRAS.411..826T


Query : 2011MNRAS.411..826T

2011MNRAS.411..826T - Mon. Not. R. Astron. Soc., 411, 826-848 (2011/February-3)

Cosmic evolution of the C IV in high-resolution hydrodynamic simulations.

TESCARI E., VIEL M., D'ODORICO V., CRISTIANI S., CALURA F., BORGANI S. and TORNATORE L.

Abstract (from CDS):

We investigate the properties of triply ionized carbon (C IV) in the intergalactic medium (IGM) using a set of high resolution and large box size cosmological hydrodynamic simulations of a Lambda cold dark matter (ΛCDM) model. We rely on a modification of the publicly available TreeSPH code GADGET-2 that self-consistently follows the metal enrichment mechanism by means of a detailed chemical evolution model. We focus on several numerical implementations of galactic feedback: galactic winds in the energy-driven and momentum-driven prescriptions, galactic winds hydrodynamically coupled to the surrounding gas and active galactic nuclei (AGNs) powered by gas accretion on to massive black holes. Furthermore, our results are compared to a run in which galactic feedback is not present and we also explore different initial stellar mass function. After having addressed some global properties of the simulated volume like the impact on the star formation rate and the content in carbon and C IV, we extract mock IGM transmission spectra in neutral hydrogen (H I) and C IV and perform Voigt profile fitting. The results are then compared with high-resolution quasar (QSO) spectra obtained with the Ultraviolet Echelle Spectrograph (UVES) at the Very Large Telescope (VLT) and the High Resolution Echelle Spectrograph (HIRES) at Keck. We find that feedback has little impact on statistics related to the neutral hydrogen, while C IV is more affected by galactic winds and/or AGN feedback. The feedback schemes investigated have a different strength and redshift evolution with a general tendency for AGN feedback to be more effective at lower redshift than galactic winds. When the same analysis is performed over observed and simulated C IV lines, we find a reasonably good agreement between data and simulations over the column density range N_ C IV_= 1012.5–15/cm2. Also the C IV linewidth distribution appears to be in agreement with the observed values, while the H I Doppler parameters, b_ H I_, are in general too large, showing that the diffuse cosmic web is heated more than what is inferred by observations. The simulation without feedback fails in reproducing the C IV systems at high column densities at all redshift, while the AGN feedback case agrees with observations only at z < 3, when this form of feedback is particularly effective. We also present scatter plots in the b-N and in the N_ C IV_-N_H I_planes, showing that there is rough agreement between observations and simulations only when feedback is taken into account.

Although it seems difficult to constrain the nature and the strength of galactic feedback using the present framework and find a unique model that fits all the observations, these simulations offer the perspective of understanding the galaxy-IGM interplay and how metals produced by stars can reach the low-density IGM.


Abstract Copyright: 2010 The Authors Monthly Notices of the Royal Astronomical Society2010 RAS

Journal keyword(s): methods: numerical - galaxies: formation - intergalactic medium - quasars: absorption lines - cosmology: theory

Simbad objects: 33

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Number of rows : 33
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 QSO J0003-2323 QSO 00 03 44.9144535192 -23 23 55.073021280     16.7     ~ 79 0
2 QSO B0002-422 QSO 00 04 48.2718888096 -41 57 28.148932548   17.44 17.21     ~ 163 0
3 QSO B0055-26 QSO 00 57 58.0253990928 -26 43 14.750912928   17.90 17.47 17.99   ~ 152 1
4 QSO B0109-353 QSO 01 11 43.6321128912 -35 03 00.587535660   16.6 16.9     ~ 79 0
5 QSO B0122-379 QSO 01 24 17.3720154480 -37 44 22.919854020     17.1     ~ 121 0
6 QSO J0153-4311 QSO 01 53 27.1920203376 -43 11 38.095833120     16.80     ~ 51 0
7 QSO B0237-2322 QSO 02 40 08.1743783856 -23 09 15.729012036   16.78 16.63     ~ 516 1
8 QSO B0329-385 QSO 03 31 06.3780612048 -38 24 04.653443772   17.63 16.92     ~ 85 1
9 PHL 4444 Bla 03 31 08.9205317376 -25 24 43.266541032   17.82 17.51 18.2   ~ 107 1
10 QSO J0422-3844 BLL 04 22 14.7829521792 -38 44 52.826059032   17.70 16.92 16.3   ~ 203 2
11 QSO J0455-4216 QSO 04 55 23.0626782912 -42 16 17.398553052   17.77 17.06     ~ 144 0
12 QSO B0636+68 BLL 06 42 04.2572705040 +67 58 35.620484340     16.46 16.01   ~ 234 1
13 QSO B0940-1050 QSO 09 42 53.5078384704 -11 04 25.931336376   16.96 16.6 16.6   ~ 102 0
14 QSO J1057+4555 QSO 10 57 56.2610108784 +45 55 53.070401748   20.19 18.80 17.2 16.8 ~ 118 0
15 QSO B1107+4847 QSO 11 10 38.6370859200 +48 31 15.691679076   17.09 16.87     ~ 94 0
16 QSO B1122-168 QSO 11 24 42.8658917592 -17 05 17.389038732   16.5 16.5 16.1   ~ 132 1
17 QSO B1158-1842 QSO 12 00 44.9451160128 -18 59 44.479378320   17.22 16.93     ~ 59 0
18 QSO J1344-1035 QSO 13 44 27.0637256688 -10 35 41.741388492     17.1     ~ 54 0
19 QSO B1422+2309 BLL 14 24 38.0938 +22 56 00.587   16.77 15.84 14.79   ~ 464 1
20 [PBW92] 1422+231 gLS 14 24 38.09400 +22 56 00.5900   16.77 15.84 14.79   ~ 359 0
21 QSO B1425+606 QSO 14 26 56.1849081360 +60 25 50.813373324   16.82 16.54     ~ 148 0
22 QSO B1442+2931 QSO 14 44 53.5398146832 +29 19 05.691187272   16.59 16.38     ~ 83 0
23 QSO B1448-232 QSO 14 51 02.5093156224 -23 29 31.107548184   17.13 16.96     ~ 135 2
24 QSO J1626+6426 QSO 16 26 45.6720635616 +64 26 55.026430800     15.8     ~ 34 0
25 QSO J1646+5514 QSO 16 46 56.3884451808 +55 14 46.123613484     18.10     ~ 32 0
26 QSO B1937-1009 BLL 19 39 57.2566747152 -10 02 41.522299692   18.800 19.0 17.188   ~ 207 1
27 QSO B1946+770 QSO 19 44 54.8532392016 +77 05 52.673448048     15.8     ~ 156 0
28 QSO B2000-330 Bla 20 03 24.1161711720 -32 51 45.136882080   18.83 18.4 17.11   ~ 279 1
29 QSO B2126-15 Bla 21 29 12.17589329 -15 38 41.0419083   17.61 17.3 17.3   ~ 521 1
30 QSO J2220-2803 QSO 22 20 06.7591541688 -28 03 23.467479516     16.0 16.10   ~ 100 0
31 QSO J2233-606 QSO 22 33 37.5812706336 -60 33 29.149992936 16.90 17.39 17.16 16.93 16.51 ~ 92 0
32 QSO B2237-0607 QSO 22 39 53.6812264896 -05 52 19.996061772     18.3     ~ 120 0
33 QSO B2347-4342 QSO 23 50 34.2593744544 -43 25 59.683985652   16.3 16.3     ~ 172 0

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