The Nature and Origin of Low-Redshift O VI Absorbers
Benjamin D. Oppenheimer (Univeristy of Arizona), Romeel A. Dav\'e, (Univeristy of Arizona)

TL;DR
This paper investigates the origin and nature of low-redshift O VI absorbers using cosmological simulations, revealing they are mainly photo-ionized, associated with enriched regions, and influenced by turbulence and recent outflows.
Contribution
It introduces a comprehensive simulation-based analysis of O VI absorbers, highlighting the roles of turbulence, enrichment history, and environment in their properties.
Findings
O VI is predominantly photo-ionized at T≈10^4.2 K.
Turbulence is necessary to match observed O VI properties.
Strong absorbers are often collisionally ionized and linked to recent outflows.
Abstract
The O VI ion observed in quasar absorption line spectra is the most accessible tracer of the cosmic metal distribution in the low redshift (z<0.5) intergalactic medium (IGM). We explore the nature and origin of O VI absorbers using cosmological hydrodynamic simulations including galactic outflows. We consider the effects of ionization background variations, non-equilibrium ionization and cooling, uniform metallicity, and small-scale (sub-resolution) turbulence. Our main results are 1) IGM O VI is predominantly photo-ionized with T= 10^(4.2+/-0.2) K. A key reason for this is that O VI absorbers preferentially trace over-enriched regions of the IGM at a given density, which enhances metal-line cooling such that absorbers can cool within a Hubble time. As such, O VI is not a good tracer of the WHIM. 2) The predicted O VI properties fit observables only if sub-resolution turbulence is…
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