We constrained the properties of potential ionized absorbers using the XSTAR analytic model warmabs , relying on all atomic level populations calculated by XSTAR using the same UV-X-ray ionizing SED from §5.1. Fitting the spectrum with the tabulated grids (see §5.2) is much quicker than the warmabs analytic modeling. However, parametric intervals used in the computation of the model grids (see interval sizes in Table 4) could add large uncertainties to derived parameters. Hence, we also used the analytic model to put more accurate constraints on the ionization state and column density of the warm absorbing gas, as well as to explore any variations in elemental abundances. As this approach is computationally expensive, we utilized the parameters determined from the XSTAR table model grids in §5.2 as initial values, and employed warmabs only to make finer estimations of the physical conditions.
For the soft excess, we again use an absorbed disk component.
The high-ionization lines visible in the spectrum
(c.f. Table 3) clearly
require a highly ionized warmabs component.
Given that the tbnew component in our phenomenological model (§4.2) shows
more absorption than expected for foreground Milky Way absorption
(
cm
; Wakker et al., 2011),
we have tried three different options for additional absorption in PG1211+143 .
Specifically, we considered (1) a neutral absorber (tbnew ) at the PG1211+143
systemic redshift,
(2) a mildly ionized warmabs model (also at the PG1211+143 systemic redshift), and
(3) a low-ionization warmabs model at the same observed redshift as the
high-ionization warmabs component.5For this third possibility we also
tied the abundance and turbulent velocity parameters to those of the
high-ionization warmabs component.
Component | Parameter | Value |
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12.0 |
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warmabs |
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All three of these possibilities resulted in essentially identical parameters for the highly ionized absorber. None of the three possibilities produced identifiable spectral features, but rather affected the shape of the low-energy X-ray continuum. Differences among the fits were primarily restricted to the soft excess parameters, with subtler differences in the highest and zpowerlw parameters. In what follows, we only present results for option (3), the additional low-ionization component at the observed redshift of the high-ionization component. However, we consider the high-ionization component to be the only one with well-measured parameters, and we only discuss its physical implications.
In our fits, we used the solar abundances defined by
Wilms et al. (2000), and adjusted the elemental abundances and the
turbulent velocity to match the absorption lines. The
best-fitting parameters derived from our model fits
are listed in Table5.
We determined the fit parameter confidence intervals
by employing the ISIS emcee hammer routine, which is an implementation of
the Markov Chain Monte Carlo (MCMC) Hammer algorithm of
Foreman-Mackey et al. (2013), and now included in the Remeis
ISISscripts6. The
MCMC approach allowed us to improve the best-fitted values of the
ionization parameter (), the column density (
), the
turbulent velocity (
), and the chemical composition of the
warmabs model as well as other phenomenological model parameters
(continuum and iron lines) listed in Table 5
(the fits, however, are not very sensitive to the chemical
composition). Figure 6 shows the 1-sigma
(68%), 2-sigma (95%), and 3-sigma (99%) confidence contours of
versus
,
versus
,
and
versus
. There is a slight
anti-correlation between the absorber column and turbulent velocity
(somewhat expected to fit the equivalent widths of the detected
features). Overall, the main absorber parameters are
well constrained.
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Ashkbiz Danehkar