2007ApJ...658..680L


Query : 2007ApJ...658..680L

2007ApJ...658..680L - Astrophys. J., 658, 680-709 (2007/April-1)

Physical properties, baryon content, and evolution of the Lyα forest: new insights from high-resolution observations at z ≲ 0.4.

LEHNER N., SAVAGE B.D., RICHTER P., SEMBACH K.R., TRIPP T.M. and WAKKER B.P.

Abstract (from CDS):

We present a study of the Lyα forest at z≲0.4, from which we conclude that at least 20% of the total baryons in the universe are located in the highly ionized gas traced by broad Lyα absorbers. The cool photoionized low-z intergalactic medium (IGM) probed by narrow Lyα absorbers contains about 30% of the baryons. We further find that the ratio of broad to narrow Lyα absorbers is higher at z≲0.4 than at 1.5≲z≲3.6, implying that a larger fraction of the low-redshift universe is hotter and/or more kinematically disturbed. We base these conclusions on an analysis of seven QSOs observed with both FUSE and the HST STIS E140M ultraviolet echelle spectrograph. Our sample has 341 H I absorbers with a total unblocked redshift path of 2.064. The observed absorber population is complete for logN_HI_≳13.2, with a column density distribution f(N_HI)∝N-β^_HI_. For narrow (b≤40 km/s) absorbers, β=1.76±0.06. The distribution of the Doppler parameter b at low redshift implies two populations: narrow (b≤40 km/s) and broad (b>40 km/s) Lyα absorbers (referred to as NLAs and BLAs, respectively). Both the NLAs and some BLAs probe the cool (T∼104 K) photoionized IGM. The BLAs also probe the highly ionized gas of the warm-hot IGM (T≃105-106 K). The distribution of b has a more prominent high-velocity tail at z≲0.4 than at 1.5≲z≲3.6, which results in median and mean b-values that are 15%-30% higher at low z than at high z. The ratio of the number density of BLAs to NLAs at z≲0.4 is a factor of ∼3 higher than at 1.5≲z≲3.6.

Abstract Copyright: ∼

Journal keyword(s): Cosmology: Observations - Galaxies: Intergalactic Medium - Galaxies: Quasars: Absorption Lines

Errata: errata vol. 661, p. 1347 (2007), vol. 674, p. 613 (2008)

CDS comments: Table 9: Lyman-alpha forest Absorbers toward PKS 0405-123 are not in SIMBAD.

Simbad objects: 22

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Number of rows : 22
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 B0117+2118 QSO 01 20 17.2642359528 +21 33 46.197696168     16.1     ~ 130 0
2 QSO J0143-3917 QSO 01 43 33.6332389872 -39 17 00.066827076     16.28     ~ 28 0
3 HE 0226-4110 Sy1 02 28 15.2391681216 -40 57 14.762648232   17.68 15.2 16.22   ~ 144 1
4 LBQS 0302-0019 QSO 03 04 49.8593341368 -00 08 13.534398816   18.08 17.80 17.5   ~ 261 0
5 PKS 0405-123 Bla 04 07 48.4309841856 -12 11 36.659928408   15.09 14.86 14.7   ~ 531 1
6 HE 0429-4901 ? 04 30.4 -48 55           ~ 4 0
7 HE 0515-4414 QSO 05 17 07.6238702856 -44 10 55.579731312 14.74 15.49 15.16     ~ 129 0
8 QSO B0624+6907 QSO 06 30 02.5051022520 +69 05 03.913837440   14.64 14.16     ~ 97 0
9 QSO B0747+4259 QSO 07 50 54.6474995592 +42 52 19.233881796   16.43 16.23     ~ 56 0
10 PG 0953+414 Sy1 09 56 52.3931554992 +41 15 22.211247636 14.710 15.611 15.546 15.294 14.720 ~ 472 0
11 PG 1101-264 QSO 11 03 25.2993421704 -26 45 15.808554720   16.08 16.02     ~ 247 1
12 Ton 1388 Sy1 11 19 08.6786220240 +21 19 17.987085948   14.91 14.80     ~ 492 0
13 QSO B1122-168 QSO 11 24 42.8658917592 -17 05 17.389038732   16.5 16.5 16.1   ~ 132 1
14 LB 2522 Sy1 13 01 12.9250750776 +59 02 06.693816732   16.04 15.89     ~ 298 0
15 QSO B1630+3744 QSO 16 32 01.1117931960 +37 37 49.980505332   16.50 16.30     ~ 183 0
16 QSO B1634+7037 QSO 16 34 28.9917184368 +70 31 32.393436960   14.90 14.66     ~ 273 0
17 ClG 1821+64 ClG 18 21 56.7276 +64 20 55.841           ~ 511 1
18 7C 1821+6419 Sy1 18 21 57.2130271440 +64 20 36.221312076   14.23 14.24     ~ 632 1
19 QSO B1946+770 QSO 19 44 54.8532392016 +77 05 52.673448048     15.8     ~ 156 0
20 QSO J2220-2803 QSO 22 20 06.7591541688 -28 03 23.467479516     16.0 16.10   ~ 100 0
21 QSO J2227-2243 QSO 22 27 56.9352929832 -22 43 02.601281856     17.60     ~ 20 0
22 QSO J2233-606 QSO 22 33 37.5812706336 -60 33 29.149992936 16.90 17.39 17.16 16.93 16.51 ~ 92 0

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