Disk emission and absorption lines in LMXB. Note on the physical conditions of an absorbing material
Agata Rozanska

TL;DR
This paper models the X-ray spectrum of LMXB 4U 1630-472 using accretion disk atmosphere models, showing that iron absorption lines can originate from the disk atmosphere itself, offering an alternative to wind-based explanations.
Contribution
It introduces detailed radiative transfer modeling of accretion disk atmospheres to explain iron absorption lines, challenging the wind-origin hypothesis in LMXBs.
Findings
Absorption lines can originate from the disk atmosphere, not just winds.
Disk atmosphere models fit high-resolution spectra well.
Wind density and location match the upper disk atmosphere conditions.
Abstract
We show that the continuum X-ray spectrum of 4U 1630-472 with iron absorption lines can be satisfactorily modeled by the spectrum from an accretion disk atmosphere. We performed full radiative transfer calculations using our code ATM21 to model the emission from an accretion disk surface that is seen at different viewing angles. Computed models are then fitted to the high-resolution X-ray spectra of 4U 1630-472 obtained by {\it Suzaku} satellite. Absorption lines of highly ionized iron originating in a hot accretion-disk atmospheres are important part of the observed line profile, and can be an alternative or complementary explanation to the wind model usually favored for this type of sources. Next, assuming that absorption lines originate from the wind illuminated by X-ray central source in LMXBs, we can put constrains on the wind location only if we know the volume density number of…
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Taxonomy
TopicsAstrophysical Phenomena and Observations · Scientific Measurement and Uncertainty Evaluation · Mechanics and Biomechanics Studies
