Free Access
Issue
A&A
Volume 656, December 2021
Article Number A107
Number of page(s) 12
Section Cosmology (including clusters of galaxies)
DOI https://doi.org/10.1051/0004-6361/202038021
Published online 09 December 2021

© ESO 2021

1. Introduction

About half of the baryonic matter in the low-z Universe is expected to exist in the form of tenuous, shock–heated, highly–ionized gas accumulated in dark matter dominated large–scale structures, commonly referred to as the warm–hot intergalactic medium (WHIM) (e.g., Cen & Ostriker 1999; Davé et al. 1999; Shull et al. 2012; Nicastro et al. 2017). Unlike the warm (T ∼ 105 − 6 K) WHIM phase that is more readily detected in the far ultraviolet (FUV) (e.g, Savage et al. 2011; Hussain et al. 2015; Pachat et al. 2016), the hot phase (T ∼ 106 − 7 K) remains practically undetected, presumably due to the lower sensitivity of the available X-ray instruments to the weak absorption lines expected to trace this phase. Although a number of observations of hot WHIM systems have been published (e.g., Fang et al. 2012; Bonamente et al. 2016; Nicastro et al. 2018; Kovacs et al. 2019; Ahoranta et al. 2019, among others), the detection significances are typically marginal.

The most important ions for detecting spectral signals of the hot (T ∼ 106 K) WHIM phase are the highly–ionized oxygen species O VII and O VIII. Since the rest wavelengths of the strongest O VII and O VIII lines are located in the soft X-ray band, the properties of hot WHIM absorbers are best studied using high energy–resolution X-ray instruments, such as the XMM-Newton Reflection Grating Spectrometer (RGS) and the Chandra Low Energy Transmission Grating (LETG) spectrometer. However, the EAGLE cosmological, hydrodynamical simulation (Schaye et al. 2015; Crain et al. 2015; McAlpine et al. 2016) predicts that most of the signals from hot WHIM absorbers fall below the current X-ray detection threshold (Nion ≳ 1015 cm−2) and that the abundance of the absorbers begins to drop steeply at the Nion ∼ 1016 cm−2 level (e.g., Wijers et al. 2019). Furthermore, the EAGLE simulation indicates that a large fraction of high column density O VII-VIII absorbers within the cosmic web are associated with the gaseous halos surrounding galaxies (i.e., the circumgalactic medium, CGM), whereas the X-ray detectable absorbers of the intergalactic medium (IGM) are expected to become much rarer with increasing distance from the galactic halos (Johnson et al. 2019).

The rarity of strong X-ray WHIM absorbers and the low expected detection significances of the associated ionic lines reduce the likelihood of identifying X-ray absorbing WHIM systems through a pure blind search. Fortunately, the EAGLE simulation also predicts correlations between the observables of the warm WHIM phase and the hot, X-ray absorbing phase (e.g., between NOVI and NOVII; Chen et al. 2003; Wijers et al. 2019), which can be used to limit hot WHIM searches to the most likely locations.

In this paper, we leverage the prediction of correlated FUV and X-ray absorption, and we study the only significantly detected O VI absorber (zOVI ≈ 0.0458) in the sightline toward Ton S 180 (Danforth et al. 2006; Tilton et al. 2012), a type 1 narrow-line Seyfert galaxy (NLS1) located at z = 0.0617. The spectral properties of Ton S 180 have been studied in multiple wavelength bands, revealing no evidence of ≳103 km s−1 intrinsic outflows (see e.g., Turner et al. 2002; Gofford et al. 2013; Muzahid et al. 2013). The closest detected galaxy to the examined O VI absorber is a late type galaxy with L = 0.4 L*, located at z = 0.0456 with an impact parameter ρ ≈ 290 pkpc to the sightline. It is the only L > 0.1L* galaxy within ρ < 300 kpc near the redshift of the detected O VI absorber (Prochaska et al. 2011), and as discussed in this work, unlikely to produce X-ray detectable column densities by itself. These characteristics of the sightline towards Ton S 180 imply that any detected X-ray absorption lines would be likely associated with intervening WHIM.

This work is a part of a program focused on placing limits on the X-ray band metal absorption at the redshifts of the established O VI absorbers. The full program sample includes all sightlines which have been observed at high spectral resolution both in FUV and X-ray bands. We report the results from the Ton S 180 sightline separately from the rest of the sample, as we have found it to contain an outstandingly strong O VII signal with an associated O VI absorber, thus enabling more detailed analysis methods than would typically be applicable.

2. Observations and data preparation

2.1. X-ray data

Ton S 180 has been observed with XMM-Newton RGS on four occasions, totaling ∼200 ks exposure times for both instruments (Table 1). In addition, there is one Chandra LETG ACIS-S observation (exp. time ≈77 ks). Despite the relatively high X-ray luminosity of Ton S 180 during the Chandra exposure (F0.5 − 2 keV ≈ 1.2 × 10−11 erg cm−2 s−1), the low effective area of LETG ACIS-S at λ ∼ 22 Å ( cm2 compared to cm2) results in only a few first–order counts per channel at the wavelengths around the predicted O VII Heα location. Therefore we did not considered Chandra data in this work.

Table 1.

Summary of XMM-Newton observations.

The RGS first– and second–order data were processed using SAS v.18.0.0 with the latest calibration file libraries (up to XMM-CCF-REL-372). The data were reduced with the rgsproc pipeline adopting the default settings with three exceptions: (1) cool pixels, as identified by the rgsbadpix task, were discarded to exclude possible spectral artifacts due to unaccounted pointing shifts within the observations; (2) aspect drift–based grouping of the data was performed with twice the accuracy of the default setting, and 3) the grating line–spread functions were calculated with the full convolution space. In addition, we examined the light-curves extracted from the RGS CCD9 chips to identify time periods of Solar flares/radiation belt transits in the observational data. The good time interval files were then generated with use of the tabgtigen “rate” option and employed in the data filtering to exclude the time periods of elevated high energy particle fluxes in the detector plane.

The RGS spectra were converted into the SPEX (Kaastra et al. 1996, 2018) format with trafo (v. 1.03). We used trafo to prepare a combined spectral file, in which each RGS1 and RGS2 first–order spectrum allocates a separate SPEX sector and region. Such a combined spectral file was prepared for the analysis because it provides two clear advantages, as compared to analyzing the co–added data. First, in the co-added spectra, observation–specific wavelength grid shifts at the detector plane can induce bias near the pixels and columns with abnormal response; as the X-ray flux from the source varies with time, artificial spectral features resembling emission and absorption lines may emerge in the co-added spectrum as a result (for more detailed description on the formation of such co-addition artifacts, see Kaastra et al. 2011). Second, the combined spectral file enables fitting the time–varying spectral components independently for each observation, while at the same time the static components, such as absorption, can be fitted as a common value between the spectra.

In addition, we generated co–added RGS1 and RGS2 first order spectra (by combining the reduced spectra with the SAS tool rgscombine), and a background–subtracted fluxed spectrum, in which all the RGS1 and RGS2 first– and second–order data were combined to provide the maximum signal–to–noise ratio (S/N) for the spectra (i.e., SAS rgsfluxer task generated spectra combined with the SPEX rgsfluxcombine tool). These two co–added spectra were generated for visual inspection only, not for analysis purposes, because of the co-addition artifacts that these spectra are likely to contain.

2.2. FUV data

Ton S 180 has been observed in the FUV with both the Far-Ultraviolet Spectroscopic Explorer (FUSE) and the Space Telescope Imaging Spectrograph (STIS) on the Hubble Space Telescope (HST). The individual STIS G140M exposures were reduced using the latest STIS pipeline software CALSTIS v. 3.4.2. The flux–calibrated and individually–reduced exposures were co–added using inverse–variance weighting to improve the S/N. The final co–added spectrum covers the 1195 − 1300 Å range with a medium resolution of ≈15000 and with an S/N of 15 − 40 per raw-pixel (≈20 per pixel around 1270 Å, i.e., near the predicted wavelength of H I Lyα at zOVI).

The FUSE analysis was conducted using observation-level spectral files (OID’s P1010502000 and D0280101000, taken 1999-12-12 and 2004-07-13, respectively), available at MAST1. These data files contain fully calibrated, co–added spectra (i.e., combining the sub–exposures) for each FUSE segment and channel, processed with the final version (v. 3.4) of the CalFUSE data reduction pipeline (for more details, see Dixon et al. 2007). While three FUSE channels cover the wavelength band of the examined O VI absorption (i.e., Lif1A, Sic1A and Sic2B), at this band, the Lif1A channel provides an about two times larger effective area than the two Sic detectors combined. Due to the low S/N ratio in the data of the Sic spectra, and the calibration issues that can follow from that, we consider only the Lif1A data in this work. In the analysis presented in Sect. 3, we use co-added Lif1A spectra, where the two observations have been combined using inverse–variance weighting. This spectrum has an S/N of 5 per pixel in the band of interest.

3. FUV analysis near z = 0.04560

As the basis for the search of X-ray absorption lines we begin by re–analyzing the FUV data for the previously detected absorption features near z = 0.0456 (e.g., Danforth et al. 2006; Tilton et al. 2012). This reference redshift corresponds to that of the galaxy with the smallest impact parameter along the sightline near the absorber (as discussed in more detail in Sect. 7).

We analyzed the H I Lyα lines in the STIS data and the H I Lyβ, C III 977, and O VIλλ 1031.9 lines in the FUSE data. The weaker O VIλλ 1037.6 line was not measured owing to the low S/N of the data. For each line, we normalized the data using low–order polynomial fits to surrounding line–free regions. We fit the lines with Voigt profiles convolved with the appropriate line-spread functions (the tabulated STIS LSF2 and an assumed Gaussian FUSE LSF with FWHM = 20 km s−1) using VPFIT3. In each case, we used the minimum number of Voigt components required to produce a reduced χ2 ∼ 1. The resulting fits provide centroid wavelengths, line widths, and column densities from each transition.

The results of the best–fit models of the four absorbers closest to z = 0.04560 are presented in Table 2, and the O VI, C III, H I best-fit models are shown in Fig. 1. The z = 0.04579 O VI line yields a best-fit width, bOVI = 17.0 ± 7.1 km s−1, which is roughly equal to the FUSE limit (R ∼ 15000). A similar result is obtained for the weaker O VI feature at z = 0.04557, thus implying that both of these lines arise from warm/cool gas.

thumbnail Fig. 1.

FUSE and STIS spectral data of O VI, C III, H I in velocity space relative to z = 0.04560. The O VIλ 1037.6 Å line was not included in the fits due to the poor S/N at the relevant wavelengths (top panel). The unlabeled absorption feature blueward of the C III lines is the Galactic Si IIλ 1020 Å line. A binning factor of 3 has been used for FUSE data in this illustration.

Table 2.

Measurements of FUV absorption lines near z = 0.0456.

The best-fit centroid wavelength (λOVI ≈ 1079.18 Å) of the z = 0.04579 O VI line lies close to a Galactic H2 transition (L2R2 1079.2254 Å). However, since the stronger J = 2 rotational level transitions of H2 (such as L3R2 1064.9948 Å, L4R2 1051.4985 Å, L5P2 1040.3672 Å etc.) are not detected, we conclude that the O VI line is not contaminated with Galactic H2 absorption. There is no clear indication of H I absorption associated with the z = 0.04579 O VI line; the velocity offset of the nearest H I Lyα line (Δv ≈ 35 km s−1) is larger than plausible intrumental uncertainties (as discussed e.g., in Danforth et al. 2006). The same is true for the weaker O VI feature detected at z = 0.04557 (Δv ≈ 27 km s−1). We therefore assume that the O VI–H I misalignments are physical, and that the Lyα lines associated with the detected O VI absorbers are not detected due to their low column densities (i.e., high gas metallicity), broad line profiles, fitting complications due to blending with the z = 0.04567 Lyα line, or some combination thereof. In contrast, the only detected C III line is found to match the redshift of the z = 0.04567 Lyα absorber. Our analysis of the FUV data is in general agreement with that of Danforth et al. (2006), who had also found a statistically significant O VIλ 1031.9 Å line at a similar redshift (Δv ≈ 70 km s−1 with respect to zHI = 0.04560), with only marginal evidence of the associated 1037.6 Å line.

4. X-ray spectral modeling

The X-ray spectral analysis of this work was conducted with SPEX vs. 3.03.004 using Lodders & Palme (2009) proto–Solar abundances and Bryans et al. (2009) collisional ionization equilibrium (CIE) ion fractions (i.e., the SPEX default tables). We used SPEX to rebin the data to 20 mÅ wavelength bins, which oversamples the RGS energy resolution by a factor of ≈3. Due to the low number of spectral counts per channel in some of the observations, the spectral models were minimized using Cash statistics (Cash 1979).

We model the X-ray spectra using an absorbed power–law model and fit the data with a (partial) joint fit method. In these fits, the absorption component fit parameters are coupled across spectral observations, while the power–law continua, being highly time variable for Ton S 180, are modeled independently for each observation. The absorption model includes components for (1) the hot Galactic halo; (2) the neutral Galactic halo5, whose NH is free to vary between 1.3 − 1.7 × 1020 cm−2; (3) the hot halo of the source galaxy; (4) a redshifted intergalactic absorber, which is the main component of interest for this paper. Absorption components 1–3 are modeled using the SPEX ‘hot’ components, that is, absorption through an optically thin layer of gas in collisional ionization equilibrium. In case of the neutral halo modeling, we fix the gas temperature to kT = 5 × 10−4 keV, which is a parameter choice for the SPEX ‘neutral plasma’ modeling. Other than that, we let the defining parameters of the continuum shapes (photon index and normalization parameter) and absorption components (NH and kT) vary throughout the analysis. This ensures that the uncertainties of these model parameters are propagated correctly to the uncertainties of the model parameters of interest.

For the redshifted absorption component (4), which models the intervening WHIM absorption, two different model components were used. We begin the analysis by adopting a single–ion absorption model (SPEX ‘slab’), so as to examine oxygen absorption through the absorber. Then, we use the SPEX ‘hot’ CIE absorption component in order to investigate the ionization conditions within the absorber.

5. Results of the X-ray spectral analysis

5.1. Oxygen absorption at z = 0.04579

O VII and O VIII lines at zOVI = 0.04579 were first examined individually with the redshifted ‘slab’ model. We limit the fitting band to 16 − 24 Å which contains all the strongest oxygen lines for the redshifted and the non-redshifted (Galactic) absorber components. The results of the ‘slab’ analysis are presented in the second column of Table 3.

Table 3.

X-ray and FUV measurements of the Ton S 180 oxygen absorber.

The spectral modeling of O VII absorption yields log, corresponding to a 5.0σ statistical significance for the detection of redshifted oxygen. The O VIII signal is not significantly detected in the data, although the fit yields the best-fit value log NOVIII(cm−2)≈15.7. Whereas the best-fit predicted O VIII Lyα signal is not strong enough for visual identification at the S/N level of the individual spectra, we note that this signal does appear more prominent in the fluxed spectrum, where all the data of RGS1, RGS2 first and second spectral orders are combined to attain the maximal S/N spectrum for visual inspection (as is shown later in this paper).

We acknowledge that the RGS instruments contain a large number of instrumental features which can cause measurement bias if coinciding with the wavelength bins of a modeled spectral feature. To test the reliability of the redshifted O VII measurements, we investigate the instrument effective area at the spectral location of the detected O VII Heα line (Fig. 2). We find that the closest instrumental feature is located far enough from the modeled line profile not to affect the measurement, thus indicating that this absorption feature has an astrophysical origin.

thumbnail Fig. 2.

Top panel: zoom in on the non-binned count spectrum of the longest, 124 ks RGS1 first–order exposure near the detected O VII Heα line. The red curve is the best-fit of the redshifted SPEX ‘slab’ model minimized to the data shown, yielding ion column log NOVII (cm−2) = 16.5, i.e., a value consistent with the main analysis. The orange line marks the predicted O VII line centroid and the blue curve the subtracted background in each channel. The missing data bins were removed by the reduction software due to the bad response (see Sect. 2.1 for details). Below: The effective area of the RGS1 instrument in the corresponding wavelength range, showing two instrumental features.

5.2. CIE absorption at z = 0.04579

The high O VII column density measured with the ‘slab’ model is a possible indicator of CIE conditions for the absorbing gas (see e.g., Fig. 11 in Wijers et al. 2019). We examine this scenario by replacing the redshifted ‘slab’ component with a redshifted CIE absorption component with proto–Solar abundances, and we fit the model parameters NH(Z) and kTCIE. For this fit, we expand the fitting band to cover the wavelengths between 13 − 30 Å, so as to include additional model–constraining lines in the analysis, including those of Ne IX, N VII, C VI, and others. The results of the CIE modeling are presented in the third column of Table 3.

The CIE modeling yields tight constraints on the gas temperature, kTCIE = 0.14 ± 0.02 keV (TCIE = 1.7 ± 0.2 × 106 K) with the model scaling parameter cm−2. The best–fit CIE model also indicates that:

(1) the CIE O VII and O VIII ion column densities agree with the ‘slab’ results; (2) the CIE model predicts no other detectable lines in the RGS energy band for the available S/N level, and (3) the CIE model predicts NOVI that matches the FUV measured O VI column associated with the z = 0.04579 O VI line.

The O VI column-density predictions of the CIE model seemingly imply that the FUV detected O VI signal at zOVI = 0.04579 is the counterpart of the hot CIE phase, regardless of what other phases might be present in the absorbing medium. Considering additional information provided by the FUV and X-ray measurements, we examine whether this interpretation is plausible. Namely, if all line detections originate from a common CIE phase, the O VI line profiles should have the following broadening:

(1)

where is the predicted Doppler spread of O VI lines, m the atomic mass of oxygen and bnt the nonthermal velocity dispersion (bnt ≥ 0).

In contrast, the FUV analysis yields bOVI = 17.0 ± 7.1 km s−1 (Table 2), or a 3σ upper limit bOVI < 38.3 km s−1. Assuming the detected O VI line is only thermally broadened, the 3σ upper limit on the O VI ion temperature would correspond to TOVI < 1.4 × 106 K. The information on the line–widths therefore indicates that the FUV and X-ray measurements are unlikely to trace oxygen belonging in the same gas phase.

6. Properties of the FUV/X-ray absorbing medium towards Ton S 180

In Sect. 5.2 we showed that while the X-ray CIE absorption modeling yielded O VI-VIII column density constraints matching their freely fitted ion column densities, the FUV measurement on the O VI line width excludes the possibility of a single–temperature CIE plasma. We note that the disagreement between the obtained TCIE and TOVI cannot be due to transient differences between the electron and ion temperatures in collisionally ionized heating/cooling gas because in low-density (nH ≲ 10−4 cm−3, Z < Z), heating gas, ∼106 K equipartition is reached faster than the ionization equilibrium due to electron collisions. Similarly, recombination–lag–driven over-ionization of cooling gas (e.g., Yoshikawa & Sasaki 2006, and references therein) seems implausible, given that the oxygen ion cooling times exceed the Hubble time for typical WHIM metal number densities (as is shown, e.g., in Bykov et al. 2008).

Alternatively, the absorber could be predominantly in photo–ionization equilibrium (PIE), at a gas temperature within the measured limits of the O VI ion temperature (for which the best–fit value of b predicts TOVI ≈ 3 × 105 K if the line is only thermally broadened). We therefore investigate the WHIM ion mass distributions in Khabibullin & Churazov (2019), which is based on the magneticum6 cosmological, hydrodynamical simulation. Their results show that, in principle ∼106 K CIE–like oxygen ionization conditions can occur in T ∼ 105 K WHIM in PIE. Nevertheless, we find that in the case of the examined absorber, the measurement limits on NOVI, NOVII, NOVIII are inconsistent with the relative abundances of O VI, O VII and O VIII in their simulations, as significant discrepancies remain even at the most closely matching parameter region (T ≈ 4.5 × 105 K, nH ∼ 10−5 cm−3). Considering our measurement constraints on O VI-VIII, we find that the best match with the Khabibullin & Churazov (2019) results occurs at T ≈ 1 − 2 × 106 K and nH ≈ 2 × 10−5 cm−3, which is a solution located in the CIE dominated branch of their WHIM distribution.

6.1. Two–phase model

Because the one–phase hypothesis seems like an improbable interpretation for the O VII, O VI measurements, we instead consider more complex thermal structures by investigating the correlation between the spatial occurrence of warm and hot WHIM absorbers in the EAGLE simulation (Wijers et al. 2019). We focus on a two–temperature scenario in which the X-ray signal arises from a hot CIE phase, whereas the FUV absorber traces warm gas, which may be predominantly photo– or collisionally–ionized, or in a mixed state.

Since the FUV and X-ray detected gas phases are unlikely to be strictly co–spatial, we make use of the well–sampled O VII signal and fit zOVII with the SPEX ‘slab’ model. With this fit we obtain zOVII = 0.0455 ± 0.0005, corresponding to Δv = −16 ± 140 km s−1 with respect to z = 0.0456. The best-fit redshift of the O VII absorption is therefore consistent with both of the detected O VI absorbers (i.e., zOVI = 0.04579, Δv = 61.8 km s−1 and zOVI, weak = 0.04557, Δv = −8.5 km s−1) within the measurement uncertainty.

In addition, we note that the strong O VII Heα signal can be used to constrain bOVII, even if the RGS resolving power does not allow direct measurements of the O VII line widths. This is because at the X-ray–detectable ion column densities (NOVII ≳ 1015 cm−2), the strongest O VII lines will be saturated at the line center to a degree that depends on the O VII ion column density and the line–of–sight velocity dispersion of the absorbing ions. In Fig. 3 we demonstrate the effects of line saturation on observations of X-ray detectable O VII column densities in the WHIM regime. The constant EWHeα (dashed) curves show that the ratio between the lower limit on EWHeα and the upper limit on EWHeβ, constrain the lower limit on bOVII, and vice versa. Indeed, the lower limit on bOVII, being dependent on the lower limit of the stronger and the upper limit of the weaker line, is always obtainable when the O VII Heα line is significantly detected. In contrast, to place an upper limit on bOVII, a detection of the Heβ line is also required. Furthermore, the figure illustrates that the narrow line widths (e.g., bOVII < 100 km s−1), which are most common in O VI absorbers, require higher column densities of O VII for X-ray detection than the broader lines require (as indicated by the crossings of the EWHeα curves over the NOVII curves). It is noteworthy that this scenario contrasts with the limitations of FUV O VI searches, which are most sensitive to narrow lines (e.g., Richter et al. 2006).

thumbnail Fig. 3.

Theoretical O VII Heα and β line equivalent width ratio as a function of line width b. The solid curves show the EWHeα/EWHeβ -ratio for various O VII ion column densities, as labeled. The dashed lines show a selection of constant EWHeα curves in this plane, excluding the parameter regions where the associated ion column densities exceed NOVII = 1017 cm−2. When moving, at fixed column density (i.e., along a solid curve), from high to low b–values, the equivalent width ratio decreases gradually from its optically thin value, due to the stronger saturation of the Heα line relative to that of the weaker β line. When Heα line saturation reaches the damped regime, the opposite behaviour takes place. These properties suggest that the EWHeα/EWHeβ -ratio can be utilized as a sensitive diagnostic tool for b in the range of X-ray detectable O VII ion column densities, especially for low line-of-sight gas velocity dispersions.

Therefore, we free the SPEX ‘slab’ velocity dispersion parameter in the modeling, so that the free parameters of the redshifted absorption component include NOVII, bOVII and zOVII. This fit yields km s−1, which exceeds the thermal broadening for oxygen lines calculated with Eq. (1) (bth ≈ 42 km s−1), and indicates a non–thermal broadening of km s−1. We find that adopting this smaller bOVII–value would increase the statistical significance of the O VII detection from 5.0σ to 6.7σ, thus implying that the O VII line ratio is affected by stronger saturation than what is predicted if one adopts the SPEX default for the line-of-sight velocity dispersion, which corresponds to b = 141 km s−1.

To complete the X-ray analysis, we utilize the information from the O VII ‘slab’ modeling and re-fit the redshifted CIE model and O VIII ‘slab’ while fixing the redshift and non-thermal velocity dispersion to the obtained best-fit values, since one expects these parameters to be shared with all the ionic lines originating from the same gas phase. The results of these fits are presented in Cols. 4 and 5 of Table 3. The X-ray data and the best-fit CIE absorption model is presented in Fig. 4.

thumbnail Fig. 4.

Panels a–d: continuum normalized RGS1 1st order spectra of the reduced observations (binning factor 2), zoomed in around the z = 0.0455 OVII Heα wavelength, indicated by the orange line. The red curve is the best-fit model including the Galactic and redshifted SPEX ‘hot’ absorption components (Sects. 4, and 6.1). These components were jointly–fitted to the individual spectra (i.e., RGS1–RGS2 1st), whereas the emission continua were fitted independently for the data of each observation. The clean times and the source fluxes (0.5–2 keV) are quoted. Due to the failed RGS2 instrument CCD array #4, and zero effective area of higher dispersion orders above λ ≳ 20 Å, only RGS1 1st order data covers this spectral band. Panel e: Co-added spectrum of the RGS1 1st data at the same band. The absorption model is the same as in panels a–d, but the continuum was fitted to the co-added data. Panel f: a fluxed spectrum (binning factor 3) combining all the reduced RGS data (i.e., RGS1–2 1st and 2nd dispersion orders) at the band containing a set of weaker spectral lines produced by the same best-fit absorption model as above. The centroid wavelengths of the z = 0.0455 lines are marked with solid, and the Galactic lines with dotted, lines. From left to right they are: redshifted O VII Heγ, Galactic O VII Heβ, Galactic O VIII Lyα, redshifted O VII Heβ, redshifted O VIII Lyα. The continuum was fitted to the fluxed spectrum.

6.2. Detectability of FUV lines associated with the hot phase

6.2.1. O VI

The CIE model described in Sect. 6.1 predicts km s−1 and log NOVI (cm−2) = 13.9 ± 0.2 for the non-detected, hot phase O VI lines. Such a shallow, broad line profile would be at the limits of detetectability in the FUSE data, and its detection is degenerate with the continuum model (Fig. 1). Additionally, the predicted absorption signal would overlap with the narrower feature from the cooler gas phase, so any model of or limits on the hot phase O VI signal must be determined jointly with the properties of the narrow line and the continuum.

To better understand the range of plausible absorption parameters for both the narrow features and the possible, predicted broad feature, we sampled the posterior probability distribution of the absorption and continuum parameters with version 3.0.2 of emcee (Foreman-Mackey et al. 2013), which implements the affine-invariant Markov chain Monte Carlo (MCMC) ensemble sampler from Goodman & Weare (2010). This Bayesian approach allowed us to consider several combinations of models and prior probability distributions, while avoiding assumptions of Gaussianity in the posterior distribution. In all cases, we optimized the likelihood function using 1000 walkers initialized randomly within the domain. We discarded a number of initial steps equal to twice the maximum autocorrelation time in a parameter as a burn-in period, and we thinned the resulting chains of samples by a factor of half an autocorrelation time to reduce autocorrelation within each chain of samples.

The analysis was conducted using the observation–specific spectral files separately. Though we considered several O VI absorption models with various assumed prior probabilities, we always performed a joint fit to the two available FUSE observations. We assumed a local linear continuum model with a slope that is fixed across the observations, but with different normalizations for the two observations owing to the different flux levels of the background AGN on the two dates. In all subsequent discussion of the absorption parameters, we have marginalized over the posterior continuum parameter distributions.

We first consider a simple single line model to investigate the posterior probability distributions of NOVI, z and b over the FUV O VI absorber. Adopting uniform priors over log NOVI (cm−2) < 17, z = 0.0458 ± 0.0005 and b = 0 − 120 km s−1, this approach yields the median parameter values and 68%-confidence quantiles summarized as MODEL A in Table 4. The posterior probability distributions for this model are shown in Fig. 5.

thumbnail Fig. 5.

Posterior probability distributions for the parameters of the narrow O VI component obtained from the assumptions of MODEL A, marginalizing over the continuum parameters. We note that the allowed redshifts and line widths are incompatible with the expectations from the X-ray analysis.

Table 4.

Posterior probabilities of the Bayesian analysis at the redshift of the oxygen absorber.

However, we know from surveys that IGM absorbers are not uniformly probable in strength or width, and it might be reasonable to adopt more stringent priors based upon these intergalactic O VI absorber surveys. The MODEL B column of Table 4 summarizes the results of such a model, in which the prior on z remains uniform, but the other line parameters use priors taken from IGM surveys. The prior line width distribution above b = 28 km s−1 is described by Gaussian with μ = 28 km s−1 and σ = 16 km s−1, as in Fig. 7 of Tilton et al. (2012). Below b = 28 km s−1, the probability is assumed to be uniform, owing to the incompleteness in the IGM survey arising from line blending and spectral resolution. The log NOVI prior probability distribution is constructed such that above log NOVI (cm−2) = 13, the probability falls off according to a broken power-law distribution as described in Sect. 4.2.1 in Danforth et al. (2016). Below log NOVI (cm−2) = 13, the probability is assumed to be uniform, again owing to the incompleteness of the IGM survey. We note that these are rough approximations of our prior knowledge: they neither account for covariances between the parameters, nor do they address potential incompleteness at the high-b end of the distribution, which might arise, for example, from uncertain continuum models in the surveys. The model given by the median parameter values is plotted in Fig. 6.

thumbnail Fig. 6.

Absorption model using the median parameter values from MODEL B, shown overplotted on the 1999 FUSE data, which is the observation with the highest signal-to-noise ratio. The median values from the other models are not shown, as they qualitatively appear almost identical to this one.

These two single-phase models yield similar results and illustrate that the qualitative results of our single-component fit are fairly robust to our choice of priors. While the most likely column densities are compatible with that predicted by our X-ray analysis, the posterior distributions of the redshift and b-parameter imply that this O VI absorption component is unlikely to trace the same hot phase as the O VII absorption. Specifically, we find that 90.9% (MODEL A) and 96.2% (MODEL B) of the posterior probability falls below b = 42 km s−1, which is smallest width expected of a line arising from a hot phase (Eq. (1)). Obviously, considering the bOVI constraints arising from the X-ray EW -measurements, a one–phase solution appears increasingly less likely.

Because a single O VI absorption component yields results that are incompatible with the X-ray measurements, we also investigated a two-component model to determine if the FUSE data is compatible with an undetected, broader O VI component that could arise from the same gas as the detected O VII line. We considered a simplistic two-phase model with uniform priors on the parameters of a narrow component and the column density of a second component (as in MODEL A), but with the b-parameter of the broad component fixed at 106 km s−1 (as in the best-fit X-ray model) and its redshift prior described by a Gaussian distribution, with mean at z = 0.0455 (as in the best-fit X-ray model) and a variance that includes the X-ray measurement uncertainty, FUSE wavelength calibration uncertainty, and the X-ray wavelength uncertainty added in quadrature. The MODEL C column of Table 4 summarizes the results of this model.

If we further allow the line width of the broad component to vary by adopting a Gaussian prior on b centered on the best-fit X-ray value a variance corresponding to the X-ray measurement’s lower 1σ uncertainty, then we obtain the results given in the MODEL D column of Table 4. As we might expect, this choice of priors weakens the upper limits that the model places on the column density, because broader lines allow higher column densities to be hidden by the noisy continuum. We note that we did not attempt to reproduce the asymmetric uncertainty distribution obtained in the X-ray measurement (due to the measurement technique’s higher sensitivity towards low b–values, see Sect. 6.1), because at extremely high b-values (e.g., b ≫ 150 km s−1), the line profile both reaches unphysically large values and is highly degenerate with the continuum parameters.

Regardless of our choice of priors, the width and redshift of the broader component in these two–phase fits are largely unconstrained by the data, and instead are simply tracing our choice of priors, as we would expect in the case of a non-detection. However, the analysis does provide useful upper limits on the column density of gas. These limits indicate that a broad O VI line would be undetectable over a major fraction of the X-ray constrained parameter space, given the photon–statistics of the available FUV data. In particular, we find the data is consistent with a broad line profile centered at z ≈ 0.0455 − 0.0458 and characterized by b ∼ 100 km s−1 and log NOVI (cm−2)∼13 − 14 (see Table 4). This conclusion is robust to the choice of priors: The peak of the posterior column density probability from MODEL C (which has bOVI fixed to the X-ray best–fit value), lies within 13 < log NOVI (cm−2) = < 14, while 99.7% of the distribution falls below log NOVI (cm−2) = 13.98. In case of MODEL D, which applies the X-ray measurement based bOVI prior, the corresponding 3σ upper limit for log NOVI (cm−2) increases to 15.00, as broader line profiles are allowed. The Bayesian analysis thus indicates that whereas the two–phase scenario is consistent with the measurement data, the one–phase alternative (explaining both the O VI and O VII detections) appears unlikely.

6.2.2. Broad HI Lyman-alpha

In addition, the CIE model predicts a H I Lyα line with km s−1, and log NHI(cm−2) = 12.9 ± 0.2 × log Z/Z. The signal of this line would overlap with the blend of the two detected Lyα lines at z = 0.04512 and z = 0.04567 (Table 2), effectively preventing the spectral modeling of this line.

Therefore, we follow an alternative method that consists of calculating the statistical significance level, Nσ, expected for the X-ray predicted Lyman alpha line present in STIS data by applying the following equation (see Hellsten et al. 1998, for details):

(2)

Here, Npix is the number of detector pixels used in the EW detection, and Δλpix denotes the pixel widths in the spectral wavelength units. Throughout our calculations, we adopt Npix value that corresponds the FWTM (full width at 1/10 maximum) of a Gaussian (bHI = 200 km s−1) line profile convolved with the instrumental LSF (see Sect. 3).

We calculate 3 and 5σ EW limits from the continuum signal-to-noise ratio using Eq. (2), and convert them into column density limits, assuming the line will fall in the linear part of curve of growth. Since the X-ray predicted, broad Lyα line will coincide with the absorption by narrower Lyα features from cooler gas phases, the data cannot be used to directly calculate the upper limits. Thus, we first model out the cooler phase HI contribution (using the best–fit, two–component model presented in Table 2) and use then the standard deviation of the residual continuum fluxes to calculate the desired upper limits.

The analysis yields formal 3σ upper limit log NHI (cm−2)≲13.0, and a 5σ limit log NHI (cm−2)≲13.2 for the broad HI (see Fig. 7). Comparing these limits to the best-fit CIE model predicted NHI, we calculate the corresponding lower limits for the hot phase metallicity, for which we get Z ≳ 0.8 × Z and Z ≳ 0.5 × Z, respectively.

thumbnail Fig. 7.

Upper limits on column density of a broad H I Lyα. Top panel: model of the (narrow) H I Lyα blend used in the upper limit determination. Bottom panel: normalized residual spectrum after model removal. Red and blue curves show the broad (bHI = 200 km s−1) line profiles at limiting column densities as indicated. Purple vertical lines mark the expected centroid wavelength of the broad line, as based on the X-ray prediction.

The obtained metallicity limits appear high for intergalactic gas, for which one would generally expect Z ∼ 0.01 − 0.1 × Z, or Z ≲ 0.4 × Z in the regions close to galactic halos (e.g., Martizzi et al. 2019). While we acknowledge that our approach includes several sources of uncertainties, such as those involved in the z = 0.04512, z = 0.04567 Lyα blend model, and the uncertainties related to the X-ray model predicted BLA line profile (e.g., in zH I, NHI, bHI and the CIE model O/H), the BLA analysis seems to exclude the possibility of much lower metallicities (e.g., that of a typically assumed WHIM metallicity, Z ≈ 0.1 × Z).

It is worth noticing, however, that our limits on metallicity are limited to the measurements of hot, O VII absorbing phase only. It is very well possible that the obtained metallicity limit is not representative outside this phase. Indeed, as shown in Fig 13 in Wijers et al. (2020), the EAGLE simulation predicts highly ionized oxygen absorbers’ ion-weighted metallicities to remain atypically high (i.e., close to ≈Z) up to at least a few r200’s distances from galaxies. While our metallicity limit on the O VII absorbing phase agrees with this prediction, it may also reflect a more general situation when it comes to the observational studies of high column density metal line absorbers; the instrumental sensitivity limits drive a selection effect that favors detections of high metallicity gas.

7. Comparison to the EAGLE simulation

The O VI and O VII column densities inferred from the two-phase model (Sect. 6.1) are now compared to predictions from the EAGLE cosmological, hydrodynamical simulation (Schaye et al. 2015; Crain et al. 2015; McAlpine et al. 2016) for co-spatial O VI and O VII gas in the cosmic web.

In Fig. 8, we show the simulated distributions of O VI and O VII ion column densities through z = 0.1 absorption systems in EAGLE (for details on generating the simulated data, we refer to Wijers et al. 2019). In the context of this work, and with regards to X-ray follow-up studies of FUV detected WHIM absorbers in general, we are particularly interested in examining the EAGLE predictions for typical O VII ion columns co-located with hot/warm O VI absorbers. To study this, we divide the EAGLE (NOVI, NOVII) -distribution into ‘warm’ and ‘hot’ sub–distributions by applying a temperature cut based on the ion-weighted O VI temperature, , through the EAGLE absorbers. The temperature cut was performed at K, according to the derived 3σ upper limit on the FUV-detected, warm phase temperature (Sect. 5.2). We note that the ion-weighted temperatures in EAGLE are averaged for all phases together, and not limited to cooler, detectable gas.

thumbnail Fig. 8.

Ion column density distribution of co-located O VI and O VII in EAGLE (gray histogram in the background). The orange contours show the percentiles of NOVII that are counterparts to O VI absorbers with mean ion-weighted O VI temperature > 106.1 K (hot phase) as a function of the total (i.e., for all phases) O VI column density. The blue contours show the same for TOVI < 106.1 K (warm phase). The pink bars indicate the FUV measured warm O VI column density 1σ uncertainty range, whereas the red point marks the total ion columns of the two–phase model (i.e., hot and warm O VI, hot O VII). The green lines mark the approximate detection thresholds for O VI and O VII in FUV and X-ray bands. Detection thresholds for two representative X-ray instruments are shown: the RGS camera on-board XMM-Newton, and the Athena X-IFU, currently under development.

As illustrated in Fig. 8, the distributions for warm and hot O VI appear to be very different. The warm phase distribution (blue contours) is notably broader, in this parameter space, than that of the hotter phase (orange contours). The two distributions do not overlap within their respective 90 percentile limits, with the hotter absorbers producing systematically higher NOVII at a given NOVI throughout the examined parameter space. At the FUV–measured NOVI level (pink bars), only a small fraction of warm O VI absorbers have a detectable O VII counterpart, whereas this fraction would increase towards higher O VI column densities. Even though the warm phase produces relatively low O VII ion columns, the median of the warm phase (NOVI, NOVII) -distribution has NOVII/NOVI ≈ 101, and there are no absorption systems with NOVII/NOVI < 10−1, showing that O VII is more abundant than O VI in the EAGLE absorption systems, at least in the examined parameter range. We note that a similar conclusion about the O VI, O VII relative abundances can be drawn from the magneticum simulations of the oxygen ion mass distributions in the WHIM, presented in Khabibullin & Churazov (2019).

The two-phase model data point agrees with the hot, K absorption system oxygen distribution, but not with the warm one. This indicates that the CIE assumption adopted for the O VII absorbing phase is generally supported by EAGLE. In EAGLE, column densities as high as those found for O VIII and especially O VII mostly occur in the CGM of relatively massive galaxies (≳1012M). Indeed, the high-end O VII column densities are expected to be found inside galactic halos, and in line with this, EAGLE predicts a steep drop in O VII ion column densities when the sightline impact parameter exceeds ρ ≈ R200, due to decreasing nH and metallicity (Wijers et al. 2020).

To investigate whether halo absorption can explain the measurements for the Ton S 180 absorber, we study the galactic environment surrounding the sightline near zOVII. In the left panel of Fig. 9, we plot all the galaxies with known redshifts around the absorber within a volume corresponding to 9 × 9 pMpc2 transverse and 4 cMpc in depth. These galaxies appear to form a thread–like structure in the 2D–projection, stretching at least a few Mpc in length, while passing the sightline at a close distance. We note that such a spatial distribution of the nearby galaxies could imply that the sightline intercepts a filament of a cosmic web at z ≈ 0.0456, but we cannot confirm this scenario without additional data which is not available at this time.

thumbnail Fig. 9.

Left: galactic environment near the examined absorber. The green cross is the Ton S 180 sightline and the filled circles mark all the detected galaxies within |δz|< 0.005 (corresponding to radial depth |δr|< 2 cMpc) of zOVII. Color coding corresponds to relative radial velocities with respect to zOVII as calculated from the spectroscopic redshifts. The circles around the three galaxies with the smallest impact parameters to the sightline show the predicted R200 s along with the expected 68% variation limits (marked with the bars). The proper distance scale at zOVII is shown. Right: the fraction of EAGLE absorbers like those observed for which the galaxy with M* ≳ 109.0M and |δr|||< 3.125 cMpc that is closest to the sightline has an impact parameter greater that the value plotted along the x-axis (nb.1: orange curve). The blue and light blue curve show the same for the galaxies with the second and third smallest impact parameters, respectively. The vertical lines show the impact parameters of the three nearest galaxies found in this work (see left panel). We note that the apparently large sample of EAGLE absorbers represents only a small fraction of the total volume (1 × 10−5).

To study the origin of the oxygen absorption, we estimate the virial radii of the galactic halos with the smallest distances to the sightline (and z within the uncertainty limits of zOVII). To estimate the stellar masses, M*, for the three closest galaxies, we compared the available B-, R- and K-band photometric data (adopted from Loveday 1996; Skrutskie et al. 2006; Prochaska et al. 2011) to the color–stellar mass distributions of the galaxies with matching absolute magnitudes in the COSMOS2015 galaxy sample (Laigle et al. 2016). We obtain the most likely stellar masses and their 68th percentile limits, for which we get 109.5 ± 0.5, 1010.1 ± 0.5 and 1010.95 ± 0.2M, as listed in order of increasing impact parameter to the sightline. These stellar masses are converted into the halo mass estimations by adopting the best–fit model to the median observed M* − Mh -relationship in the z = 0.1 Universe, as presented in Behroozi et al. (2019). The derived Mh estimates are used to calculate the corresponding R200’s for each of the closest galaxies. The results of the galactic environment analysis are listed in Table 5, and the obtained R200’s illustrated with circles in the left panel of Fig. 9. We find that CGM absorption by the detected nearby galaxies cannot explain the X-ray absorption.

Table 5.

Galactic environment around the Ton S 180 oxygen absorber.

Therefore, and given the apparent galaxy overdensity in the vicinity of the z ≈ 0.0456 absorber, we examine the occurrence of high O VII-VIII ion column absorbers in different galactic environments in EAGLE. In practice, we inspect the correlation between strong O VII-VIII absorbers and their nearest neighboring M* ≳ 109.0M galaxies within 6.25 cMpc thick slices through the EAGLE. In the analysis, the galactic environment is quantified in terms of the 2D (perpendicular) distances of the nearest galaxies to the sightlines. We look for galaxies close to absorbers in EAGLE, rather than the other way around, for two (related) reasons. Firstly, it mimics the selection effects in the observations, where we looked for O VI absorption, then X-ray absorption where we found it, and finally galaxies where we found both. Secondly, absorbers as strong as those we found here, especially for O VII, are rare in EAGLE, and they are rare around galaxies of all masses. However, weaker absorbers might not have been detected, so we do not want to base our comparison too much on how rare such simulated absorption systems may be. Quantifying environments of any strong absorbers that do exist in the simulation avoids this.

In the right panel of Fig. 9 we consider only the subsample of the EAGLE absorbers fulfilling each of the measurement constraints discussed in this work: the FUV measured lower limit on NOVI and the ‘slab’ constraints for O VII-VIII ion columns measured at the same redshift. The orange curve labeled as “nb. 1” shows the fraction of absorbers from this sample for which the nearest galaxy (with M* ≳ 109.0M and |δr|||< 3.125 cMpc) has an impact parameter greater than the value plotted along the x-axis. The blue curves show the same but for the impact parameter of the second closest (nb. 2), and the third closest (nb. 3), galaxy. The analysis reveals that even though the high ion column densities are most often located in close proximity to the galaxies (indicating CGM absorption), the X-ray detectable metal columns span a wide range of environments. The figure also indicates, for instance, that up to ≈10% of the considered EAGLE absorbers occur in environments similar to those we found surrounding the Ton S 180 absorber (orange and blue vertical lines). Overall, our analysis suggests that the strong O VII X-ray absorber in Ton S 180 sightline originates in the transition region between the CGM and the diffuse WHIM.

Finally, we look back to Fig. 8 to interpret it from an observational point of view. We infer that the EAGLE spatial correlation between warm O VI and O VII (and O VIII, not shown here) is likely a manifestation of the complex multiphase structures of the intergalactic absorbers in EAGLE. The narrow O VI lines can therefore be used to trace hot WHIM gas associated with the same multi–temperature structure, whereas the broad O VI lines could reveal the direct counterparts for hot and collisionally ionized absorbers. However, the vast majority of the current FUV detections of intergalactic O VI absorbers have bOVI < 100 km s−1, with the peak of distribution at bOVI ≈ 30 km s−1 (e.g., Sembach et al. 2001; Danforth & Shull 2008; Tripp et al. 2008; Tilton et al. 2012; Danforth et al. 2016), whereas in this work we measured a non-thermal line broadening component km s−1 for the hot phase. We note that if such high bnt values are typical for the X-ray detectable absorbers, then the hot CIE O VI counterparts may often be undetectable in the FUV, due to their broad and shallow line profiles. As discussed in Sect. 6.1, the detectability of O VII lines decreases steeply towards smaller b-values, and therefore the prospects of simultaneous detection of both O VI and O VII from a common WHIM phase may be unlikely with the current observational instruments. As a result, the method utilizing O VI detections to trace X-ray absorbing WHIM seems generally more useful for finding absorption systems with complex thermal structures.

Whereas the number of X-ray detectable WHIM absorbers will likely remain low within the performance limits of current instruments, future X-ray instruments with higher sensitivity, such as the Athena X–IFU (Barret et al. 2018), should reveal a much larger sample of O VII WHIM absorbers (see Fig. 8), with the potential to resolve the missing baryons problem. With statistical data on hot absorbers’ ion column densities and their line-of-sight gas velocity dispersions, combined with the parallel analysis of the associated FUV absorbers, information on the heating mechanisms and evolution of the WHIM could ultimately be obtained.

8. Conclusions

In this paper we have presented the detection of a WHIM X-ray absorber towards the NLS1 galaxy Ton S 180, discovered by following up on the FUV (O VI) detection at redshift zOVI = 0.04579. Our main conclusions are the following:

  • i

    The measurements of O VII (and upper limit on O VIII) absorption line fluxes are consistent with a collisional ionization equilibrium state, characterized by TCIE = 1.7 ± 0.2 × 106 K and cm−2. The X-ray redshift of the absorber, zOVII = 0.0455 ± 0.0005, is consistent with two FUV O VI absorbers locating at z = 0.04557 and z = 0.045979. The latter one of these FUV absorbers is characterized by O VI ion column density matching the CIE model prediction. We link the oxygen absorption to a filamentary concentration of galaxies observed at a consistent redshift (left panel of Fig. 9).

  • ii

    The FUV O VI absorption at z = 0.04579 ± 0.00001 is described by log NOVI (cm−2) = 13.68 ± 0.10 and a 3σ upper limit for Doppler parameter bOVI < 38.1 km s−1. This O VI absorber cannot be the counterpart to the O VII–absorbing phase, as is indicated by the O VI line width constraints on the ion temperature (yielding a 3σ upper limit TOVI < 1.4 × 106 K), and by the inconsistency of bOVI with that of the O VII producing phase, for which we measure km s−1. The hot phase O VI line is not detectable within the S/N of the current FUV data, because of the shallow and broad line profile.

  • iii

    Our interpretation is that the X-ray and FUV signals are due to a multiphase absorber located at/close to an CGM/IGM transition zone of a complex, large scale galactic structure. The FUV measured O VI column density through this absorption system is ∼10−3 times NOVII, indicating that the information on the absorbing oxygen (metal) content is imprinted mainly in the X-ray band. The NOVI − NOVII distribution in the EAGLE cosmological, hydrodynamical simulation suggests that this is the case for all X-ray detectable intergalactic O VII absorbers, and also for a large fraction of absorption systems currently identified only by FUV O VI absorption. Our EAGLE analysis also implies that the X-ray detectable WHIM absorbers are mainly to be found in the vicinity of structures with enhanced galaxy densities.

The results presented in this work highlight the important role of line width measurements in the interpretation of physical conditions in the WHIM. Line width also affects detectability: The broad O VI associated with typical O VII absorbers requires very high quality FUV spectra, while the narrow O VII associated with typical O VI absorbers is hard to detect with X-ray telescopes because the line saturation reduces the equivalent width. We conclude that the line widths will be the key to understanding the physical nature and more accurately estimating the baryon content of highly ionized WHIM absorbers, when higher sensitivity X-ray instruments enable the examination of a large sample of X-ray WHIM absorbers.


Acknowledgments

JA and FA acknowledge the financial support received under ESA Athena grant 3880057 and thank J. Huovelin for supporting the X-IFU science case. SM is supported by the Experienced Researchers fellowship from the Alexander von Humboldt-Stiftung, Germany. We thank E. Churazov for discussions regarding the interpretation of the magneticum WHIM simulation data.

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All Tables

Table 1.

Summary of XMM-Newton observations.

Table 2.

Measurements of FUV absorption lines near z = 0.0456.

Table 3.

X-ray and FUV measurements of the Ton S 180 oxygen absorber.

Table 4.

Posterior probabilities of the Bayesian analysis at the redshift of the oxygen absorber.

Table 5.

Galactic environment around the Ton S 180 oxygen absorber.

All Figures

thumbnail Fig. 1.

FUSE and STIS spectral data of O VI, C III, H I in velocity space relative to z = 0.04560. The O VIλ 1037.6 Å line was not included in the fits due to the poor S/N at the relevant wavelengths (top panel). The unlabeled absorption feature blueward of the C III lines is the Galactic Si IIλ 1020 Å line. A binning factor of 3 has been used for FUSE data in this illustration.

In the text
thumbnail Fig. 2.

Top panel: zoom in on the non-binned count spectrum of the longest, 124 ks RGS1 first–order exposure near the detected O VII Heα line. The red curve is the best-fit of the redshifted SPEX ‘slab’ model minimized to the data shown, yielding ion column log NOVII (cm−2) = 16.5, i.e., a value consistent with the main analysis. The orange line marks the predicted O VII line centroid and the blue curve the subtracted background in each channel. The missing data bins were removed by the reduction software due to the bad response (see Sect. 2.1 for details). Below: The effective area of the RGS1 instrument in the corresponding wavelength range, showing two instrumental features.

In the text
thumbnail Fig. 3.

Theoretical O VII Heα and β line equivalent width ratio as a function of line width b. The solid curves show the EWHeα/EWHeβ -ratio for various O VII ion column densities, as labeled. The dashed lines show a selection of constant EWHeα curves in this plane, excluding the parameter regions where the associated ion column densities exceed NOVII = 1017 cm−2. When moving, at fixed column density (i.e., along a solid curve), from high to low b–values, the equivalent width ratio decreases gradually from its optically thin value, due to the stronger saturation of the Heα line relative to that of the weaker β line. When Heα line saturation reaches the damped regime, the opposite behaviour takes place. These properties suggest that the EWHeα/EWHeβ -ratio can be utilized as a sensitive diagnostic tool for b in the range of X-ray detectable O VII ion column densities, especially for low line-of-sight gas velocity dispersions.

In the text
thumbnail Fig. 4.

Panels a–d: continuum normalized RGS1 1st order spectra of the reduced observations (binning factor 2), zoomed in around the z = 0.0455 OVII Heα wavelength, indicated by the orange line. The red curve is the best-fit model including the Galactic and redshifted SPEX ‘hot’ absorption components (Sects. 4, and 6.1). These components were jointly–fitted to the individual spectra (i.e., RGS1–RGS2 1st), whereas the emission continua were fitted independently for the data of each observation. The clean times and the source fluxes (0.5–2 keV) are quoted. Due to the failed RGS2 instrument CCD array #4, and zero effective area of higher dispersion orders above λ ≳ 20 Å, only RGS1 1st order data covers this spectral band. Panel e: Co-added spectrum of the RGS1 1st data at the same band. The absorption model is the same as in panels a–d, but the continuum was fitted to the co-added data. Panel f: a fluxed spectrum (binning factor 3) combining all the reduced RGS data (i.e., RGS1–2 1st and 2nd dispersion orders) at the band containing a set of weaker spectral lines produced by the same best-fit absorption model as above. The centroid wavelengths of the z = 0.0455 lines are marked with solid, and the Galactic lines with dotted, lines. From left to right they are: redshifted O VII Heγ, Galactic O VII Heβ, Galactic O VIII Lyα, redshifted O VII Heβ, redshifted O VIII Lyα. The continuum was fitted to the fluxed spectrum.

In the text
thumbnail Fig. 5.

Posterior probability distributions for the parameters of the narrow O VI component obtained from the assumptions of MODEL A, marginalizing over the continuum parameters. We note that the allowed redshifts and line widths are incompatible with the expectations from the X-ray analysis.

In the text
thumbnail Fig. 6.

Absorption model using the median parameter values from MODEL B, shown overplotted on the 1999 FUSE data, which is the observation with the highest signal-to-noise ratio. The median values from the other models are not shown, as they qualitatively appear almost identical to this one.

In the text
thumbnail Fig. 7.

Upper limits on column density of a broad H I Lyα. Top panel: model of the (narrow) H I Lyα blend used in the upper limit determination. Bottom panel: normalized residual spectrum after model removal. Red and blue curves show the broad (bHI = 200 km s−1) line profiles at limiting column densities as indicated. Purple vertical lines mark the expected centroid wavelength of the broad line, as based on the X-ray prediction.

In the text
thumbnail Fig. 8.

Ion column density distribution of co-located O VI and O VII in EAGLE (gray histogram in the background). The orange contours show the percentiles of NOVII that are counterparts to O VI absorbers with mean ion-weighted O VI temperature > 106.1 K (hot phase) as a function of the total (i.e., for all phases) O VI column density. The blue contours show the same for TOVI < 106.1 K (warm phase). The pink bars indicate the FUV measured warm O VI column density 1σ uncertainty range, whereas the red point marks the total ion columns of the two–phase model (i.e., hot and warm O VI, hot O VII). The green lines mark the approximate detection thresholds for O VI and O VII in FUV and X-ray bands. Detection thresholds for two representative X-ray instruments are shown: the RGS camera on-board XMM-Newton, and the Athena X-IFU, currently under development.

In the text
thumbnail Fig. 9.

Left: galactic environment near the examined absorber. The green cross is the Ton S 180 sightline and the filled circles mark all the detected galaxies within |δz|< 0.005 (corresponding to radial depth |δr|< 2 cMpc) of zOVII. Color coding corresponds to relative radial velocities with respect to zOVII as calculated from the spectroscopic redshifts. The circles around the three galaxies with the smallest impact parameters to the sightline show the predicted R200 s along with the expected 68% variation limits (marked with the bars). The proper distance scale at zOVII is shown. Right: the fraction of EAGLE absorbers like those observed for which the galaxy with M* ≳ 109.0M and |δr|||< 3.125 cMpc that is closest to the sightline has an impact parameter greater that the value plotted along the x-axis (nb.1: orange curve). The blue and light blue curve show the same for the galaxies with the second and third smallest impact parameters, respectively. The vertical lines show the impact parameters of the three nearest galaxies found in this work (see left panel). We note that the apparently large sample of EAGLE absorbers represents only a small fraction of the total volume (1 × 10−5).

In the text

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