2012MNRAS.427.1801R


Query : 2012MNRAS.427.1801R

2012MNRAS.427.1801R - Mon. Not. R. Astron. Soc., 427, 1801-1815 (2012/December-2)

Evolution of the population of very strong MgII absorbers.

RODRIGUEZ HIDALGO P., WESSELS K., CHARLTON J.C., NARAYANAN A., MSHAR A., CUCCHIARA A. and JONES T.

Abstract (from CDS):

We present a study of the evolution of several classes of MgII absorbers, and their corresponding FeII absorption, over a large fraction of cosmic history: 2.3–8.7Gyr from the big bang. Our sample consists of 87 strong (\mi W\mi r\mo (\mi Mg\mspace \mi i\mi i\mo)\mo >\mn 0.3Å) MgII absorbers, with redshifts 0.2 < z < 2.5, measured in 81 quasar spectra obtained from the Very Large Telescope/Ultraviolet and Visual Echelle Spectrograph archives of high-resolution spectra (R ∼ 45000). No evolutionary trend in \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo)\mo/\mi W\mi r\mo (\mi Mg\mspace \mi i\mi i\mo) is found for moderately strong MgII absorbers (\mn 0.3\mo <\mi W\mi r\mo (\mi Mg \mspace\mi i\mi i\mo)\mo <\mn 1.0Å). However, at lower redshifts we find an absence of very strong MgII absorbers (those with \mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo)\mo >\mn 1Å) with small ratios of equivalent widths of FeII to MgII. At high redshifts, very strong MgII absorbers with both small and large \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo)\mo/\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo) values are present. We compare our findings to a sample of 100 weak MgII absorbers (\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo)\mo <\mn 0.3Å) found in the same quasar spectra by Narayanan et al.

The main effect driving the evolution of very strong MgII systems is the difference between the kinematic profiles at low and high redshift. At high redshift, we observe that, among the very strong MgII absorbers, all of the systems with small ratios of \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo)\mo/\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo ) have relatively large velocity spreads, resulting in less saturated profiles. At low redshift, such kinematically spread systems are absent, and both FeII and MgII are saturated, leading to \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo )\mo/\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo) values that are all close to 1. The high redshift, small \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo)\mo/\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo) systems could correspond to sub-damped Lyman α systems, many of which have large velocity spreads and are possibly linked to superwinds in star-forming galaxies. In addition to the change in saturation due to kinematic evolution, the smaller \mi W\mi r\mo (\mi Fe\mspace\mi i\mi i\mo)\mo/\mi W\mi r\mo (\mi Mg\mspace\mi i\mi i\mo) values could be due to a lower abundance of Fe at high redshifts, which would indicate relatively early stages of star formation in those environments.


Abstract Copyright: © 2012 The Authors Monthly Notices of the Royal Astronomical Society © 2012 RAS

Journal keyword(s): galaxies: evolution - galaxies: haloes - intergalactic medium - quasars: absorption lines

Simbad objects: 46

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Number of rows : 46
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 LBQS 0010-0012 QSO 00 13 06.1519752552 +00 04 31.948605732   19.29 19.05     ~ 102 0
4 LBQS 0013-0029 QSO 00 16 02.4050159808 -00 12 25.077257064   18.67 18.36     ~ 198 0
5 QSO B0055-26 QSO 00 57 58.0253990928 -26 43 14.750912928   17.90 17.47 17.99   ~ 152 1
6 PHL 957 QSO 01 03 11.2741573824 +13 16 17.809871484   16.97 16.57     ~ 350 0
7 QSO B0109-353 QSO 01 11 43.6321128912 -35 03 00.587535660   16.6 16.9     ~ 79 0
8 QSO B0112+03 QSO 01 14 53.2286036664 +03 14 56.953353696     18.6     ~ 62 2
9 QSO B0122-379 QSO 01 24 17.3720154480 -37 44 22.919854020     17.1     ~ 121 0
10 QSO B0130-403 QSO 01 33 01.9294067496 -40 06 27.997379496   17.68 17.02     ~ 89 0
11 QSO B0136-231 Bla 01 38 57.4657042440 -22 54 47.330166204   18.4 18.0 17.6   ~ 63 1
12 QSO J0153-4311 QSO 01 53 27.1920203376 -43 11 38.095833120     16.80     ~ 51 0
13 QSO B0237-2322 QSO 02 40 08.1743783856 -23 09 15.729012036   16.78 16.63     ~ 516 1
14 SDSS J030000.56+004828.0 QSO 03 00 00.5687857104 +00 48 27.963948708   20.18 18.29     ~ 55 0
15 QSO J0330-2704 QSO 03 30 32.5749333264 -27 04 39.242748900     19.00     ~ 23 1
16 QSO B0329-385 QSO 03 31 06.3780612048 -38 24 04.653443772   17.63 16.92     ~ 85 1
17 QSO J0430-4855 QSO 04 30 37.3003527936 -48 55 23.577559068 15.17 16.19 16.09     ~ 17 0
18 QSO J0455-4216 QSO 04 55 23.0626782912 -42 16 17.398553052   17.77 17.06     ~ 144 0
19 QSO B0549-213 QSO 05 51 58.2374330040 -21 19 49.964189484     20.0     ~ 31 1
20 QSO B0551-36 QSO 05 52 46.1824785360 -36 37 27.608212524   17.72 17.57     ~ 98 0
21 QSO B0926-0201 QSO 09 29 13.5729514728 -02 14 46.227751332   16.59 16.31     ~ 22 0
22 QSO B0940-1050 QSO 09 42 53.5078384704 -11 04 25.931336376   16.96 16.6 16.6   ~ 102 0
23 QSO B0952+179 QSO 09 54 56.82361677 +17 43 31.2221518   17.31 17.23     ~ 222 1
24 QSO J1113-1533 QSO 11 13 50.6122921416 -15 33 34.005990672   18.7 18.7     ~ 39 0
25 QSO B1122-168 QSO 11 24 42.8658917592 -17 05 17.389038732   16.5 16.5 16.1   ~ 132 1
26 QSO J1130-1449 Bla 11 30 07.0523452128 -14 49 27.388021944   17.17 16.90 16 16.97 ~ 739 1
27 QSO B1151+068 QSO 11 54 11.0745443880 +06 34 27.165655200     18.6     ~ 59 0
28 QSO B1157+014 QSO 11 59 44.8278142392 +01 12 06.985999764   17.87 17.52     ~ 228 1
29 QSO B1202-074 QSO 12 05 23.1360370080 -07 42 32.759842896     17.5     ~ 389 5
30 4C -02.55 Bla 12 32 00.0159535440 -02 24 04.793069304   17.41 17.06 16.4   ~ 440 1
31 LBQS 1246-0217 QSO 12 49 24.8605898856 -02 33 39.728151576   18.26 18.02     ~ 69 0
32 QSO B1331+170 Bla 13 33 35.7827544072 +16 49 04.013500728   16.84 16.71 16.41   ~ 469 1
33 QSO B1337+11 QSO 13 40 02.5419344664 +11 06 30.181521168     18.7     ~ 120 0
34 QSO J1344-1035 QSO 13 44 27.0637256688 -10 35 41.741388492     17.1     ~ 54 0
35 QSO B1418-064 Bla 14 21 07.75560722 -06 43 56.3557864   20.4 18.50 19.1   ~ 78 1
36 LBQS 1444+0126 QSO 14 46 53.0501441856 +01 13 55.924449276   18.71 18.38     ~ 75 0
37 QSO B1618-0035 QSO 16 21 16.9228185456 -00 42 50.909201856   18.92 17.97     ~ 86 0
38 4C 23.43 Bla 16 24 39.0838297968 +23 45 12.223370412   17.91 17.47     ~ 343 1
39 4C 12.59 QSO 16 31 45.1708807968 +11 56 03.203387592   18.38 18.40     ~ 122 1
40 QSO B2000-330 Bla 20 03 24.1161711720 -32 51 45.136882080   18.83 18.4 17.11   ~ 279 1
41 QSO J2047-1639 Bla 20 47 19.6670792592 -16 39 05.842775556   17.55 17.36     ~ 107 1
42 QSO B2126-15 Bla 21 29 12.17589329 -15 38 41.0419083   17.61 17.3 17.3   ~ 521 1
43 QSO B2206-1959 QSO 22 09 00.6950774976 -19 44 19.743416484     18.65     ~ 85 0
44 QSO J2220-2803 QSO 22 20 06.7591541688 -28 03 23.467479516     16.0 16.10   ~ 100 0
45 QSO J2227-2243 QSO 22 27 56.9352929832 -22 43 02.601281856     17.60     ~ 20 0
46 QSO B2314-409 Bla 23 16 46.91990359 -40 41 21.0863175   17.9 17.9     ~ 76 1

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