Intervening O VI Quasar Absorption Systems at Low Redshift: A Significant Baryon Reservoir
T. M. Tripp, B. D. Savage, E. B. Jenkins
Abstract
FUV echelle spectroscopy of the radio-quiet QSO H1821+643 (z = 0.297), obtained with the Space Telescope Imaging Spectrograph (STIS) at 7 km/s resolution, reveals 4 definite O VI absorption line systems and one probable O VI absorber at 0.15 < z(abs) < 0.27. The four definite O VI absorbers are located near galaxies and are highly displaced from the quasar in redshift; these are likely intervening systems unrelated to the background QSO. In the case of the strong O VI system at z(abs) = 0.22497, multiple components are detected in Si III and O VI as well as H I Lyman series lines, and the differing component velocity centroids and b-values firmly establish that this is a multiphase absorption system. A weak O VI absorber is detected at z(abs) = 0.22637, i.e., offset by ~340 km/s from the z(abs) = 0.22497 system. Lya absorption is detected at z(abs) = 0.22613, but no Lya absorption is significantly detected at 0.22637. Other weak O VI absorbers at z(abs) = 0.24531 and 0.26659 and the probable O VI system at 0.21326 have widely diverse O VI/H I column density ratios with N(O VI)/N(H I) ranging from <=0.14+/-0.03 to 5.2+/-1.2. The number density of O VI absorbers with rest equivalent width > 30 mA in the H1821+643 spectrum is remarkably high, dN/dz ~48, with a high (90%) confidence that it is greater than 17. We conservatively estimate that the cosmological mass density of the O VI systems Omegab(O VI) > 0.0008/h75. With an assumed metallicity of 1/10 solar and a conservative assumption that the fraction of oxygen in the O VI ionization stage is 0.2, we obtain Omegab(O VI) > 0.004/h75. This is comparable to the combined cosmological mass density of stars and cool gas in galaxies and X-ray emitting gas in galaxy clusters at low redshift.
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