Table 2.

Best-fitting parameters of the warm absorber components of |$\rm I\:Zw\, 1$| in the 2020 time-averaged spectrum inferred with a standard C-statistic analysis (on the left) and Bayesian framework (on the right).

NHlog ξvturbvoutC-stat/dofNHlog ξvoutlog Z
|$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$||$\rm km\ s^{-1}$||$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$|
Single warm absorber component
LIC|$7.7_{-0.5}^{+0.8}$|−1.0 ± 0.1|$110_{-25}^{+33}$|−1750 ± 1003218/24339.4 ± 0.6−1.2 ± 0.1−1750 ± 100−6.6
Single warm absorber component  + UFO
LIC9.0 ± 0.7−1.0 ± 0.1|$90_{-20}^{+40}$|−1750 ± 1003173/243010.0 ± 0.5−1.2 ± 0.1−1750 ± 1000.0
UFO|$200_{-100}^{+300}$|3.8 ± 0.1100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
Two warm absorber components  + UFO
LIC9 ± 1−1.0 ± 0.1110 ± 30−1750 ± 1003162/24279.4 ± 0.5−1.2 ± 0.1−1750 ± 100−0.3
HIC1.0 ± 0.61.7 ± 0.2100|$-2150_{-250}^{+200}$|0.9 ± 0.31.8 ± 0.3−2150 ± 350
UFO|$200_{-100}^{+300}$||$3.80_{-0.04}^{+0.11}$|100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
NHlog ξvturbvoutC-stat/dofNHlog ξvoutlog Z
|$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$||$\rm km\ s^{-1}$||$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$|
Single warm absorber component
LIC|$7.7_{-0.5}^{+0.8}$|−1.0 ± 0.1|$110_{-25}^{+33}$|−1750 ± 1003218/24339.4 ± 0.6−1.2 ± 0.1−1750 ± 100−6.6
Single warm absorber component  + UFO
LIC9.0 ± 0.7−1.0 ± 0.1|$90_{-20}^{+40}$|−1750 ± 1003173/243010.0 ± 0.5−1.2 ± 0.1−1750 ± 1000.0
UFO|$200_{-100}^{+300}$|3.8 ± 0.1100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
Two warm absorber components  + UFO
LIC9 ± 1−1.0 ± 0.1110 ± 30−1750 ± 1003162/24279.4 ± 0.5−1.2 ± 0.1−1750 ± 100−0.3
HIC1.0 ± 0.61.7 ± 0.2100|$-2150_{-250}^{+200}$|0.9 ± 0.31.8 ± 0.3−2150 ± 350
UFO|$200_{-100}^{+300}$||$3.80_{-0.04}^{+0.11}$|100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000

Note. The dispersion velocity has been fixed to the default value of 100 km s−1.

Table 2.

Best-fitting parameters of the warm absorber components of |$\rm I\:Zw\, 1$| in the 2020 time-averaged spectrum inferred with a standard C-statistic analysis (on the left) and Bayesian framework (on the right).

NHlog ξvturbvoutC-stat/dofNHlog ξvoutlog Z
|$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$||$\rm km\ s^{-1}$||$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$|
Single warm absorber component
LIC|$7.7_{-0.5}^{+0.8}$|−1.0 ± 0.1|$110_{-25}^{+33}$|−1750 ± 1003218/24339.4 ± 0.6−1.2 ± 0.1−1750 ± 100−6.6
Single warm absorber component  + UFO
LIC9.0 ± 0.7−1.0 ± 0.1|$90_{-20}^{+40}$|−1750 ± 1003173/243010.0 ± 0.5−1.2 ± 0.1−1750 ± 1000.0
UFO|$200_{-100}^{+300}$|3.8 ± 0.1100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
Two warm absorber components  + UFO
LIC9 ± 1−1.0 ± 0.1110 ± 30−1750 ± 1003162/24279.4 ± 0.5−1.2 ± 0.1−1750 ± 100−0.3
HIC1.0 ± 0.61.7 ± 0.2100|$-2150_{-250}^{+200}$|0.9 ± 0.31.8 ± 0.3−2150 ± 350
UFO|$200_{-100}^{+300}$||$3.80_{-0.04}^{+0.11}$|100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
NHlog ξvturbvoutC-stat/dofNHlog ξvoutlog Z
|$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$||$\rm km\ s^{-1}$||$10^{20}\ \rm cm^{-2}$||$\rm erg\ cm\ s^{-1}$||$\rm km\ s^{-1}$|
Single warm absorber component
LIC|$7.7_{-0.5}^{+0.8}$|−1.0 ± 0.1|$110_{-25}^{+33}$|−1750 ± 1003218/24339.4 ± 0.6−1.2 ± 0.1−1750 ± 100−6.6
Single warm absorber component  + UFO
LIC9.0 ± 0.7−1.0 ± 0.1|$90_{-20}^{+40}$|−1750 ± 1003173/243010.0 ± 0.5−1.2 ± 0.1−1750 ± 1000.0
UFO|$200_{-100}^{+300}$|3.8 ± 0.1100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000
Two warm absorber components  + UFO
LIC9 ± 1−1.0 ± 0.1110 ± 30−1750 ± 1003162/24279.4 ± 0.5−1.2 ± 0.1−1750 ± 100−0.3
HIC1.0 ± 0.61.7 ± 0.2100|$-2150_{-250}^{+200}$|0.9 ± 0.31.8 ± 0.3−2150 ± 350
UFO|$200_{-100}^{+300}$||$3.80_{-0.04}^{+0.11}$|100−77 100 ± 400200 ± 503.8 ± 0.1−77 000 ± 3000

Note. The dispersion velocity has been fixed to the default value of 100 km s−1.

Close
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Close