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@ARTICLE{Corrales:607574,
author = {Corrales, Lia and Gotthelf, Eric V. and Gatuzz, Efrain and
Kallman, Timothy R. and Lee, Julia C. and Martins, Michael
and Paerels, Frits and Psaradaki, Ioanna and Schippers,
Stefan and Savin, Daniel Wolf},
title = {{H}igh-resolution {X}-{R}ay {S}pectroscopy of
{I}nterstellar {I}ron toward {C}ygnus {X}-1 and {GX} 339-4},
journal = {The astrophysical journal / Part 1},
volume = {965},
number = {2},
issn = {0004-637X},
address = {London},
publisher = {Institute of Physics Publ.},
reportid = {PUBDB-2024-01936},
pages = {172},
year = {2024},
abstract = {We present a high-resolution spectral study of Fe L-shell
extinction by the diffuse interstellar medium (ISM) in the
direction of the X-ray binaries Cygnus X-1 and GX 339–4,
using the XMM-Newton reflection grating spectrometer. The
majority of interstellar Fe is suspected to condense into
dust grains in the diffuse ISM, but the compounds formed
from this process are unknown. Here, we use the laboratory
cross sections from Kortright $\&$ Kim (2000) and Lee et al.
(2005) to model the absorption and scattering profiles of
metallic Fe, and the crystalline compounds fayalite
(Fe2SiO4), ferrous sulfate (FeSO4), hematite (α-Fe2O3), and
lepidocrocite (γ-FeOOH), which have oxidation states
ranging from Fe0 to Fe3+. We find that the observed Fe
L-shell features are systematically offset in energy from
the laboratory measurements. An examination of over two
dozen published measurements of Fe L-shell absorption finds
a 1–2 eV scatter in energy positions of the L-shell
features. Motivated by this, we fit for the best
energy-scale shift simultaneously with the fine structure of
the Fe L-shell extinction cross sections. Hematite and
lepidocrocite provide the best fits (≈ + 1.1 eV shift),
followed by fayalite (≈ + 1.8 eV shift). However, fayalite
is disfavored, based on the implied abundances and knowledge
of ISM silicates gained by infrared astronomical
observations and meteoritic studies. We conclude that iron
oxides in the Fe3+ oxidation state are good candidates for
Fe-bearing dust. To verify this, new absolute
photoabsorption measurements are needed on an energy scale
accurate to better than 0.2 eV.},
cin = {DOOR ; HAS-User},
ddc = {520},
cid = {I:(DE-H253)HAS-User-20120731},
pnm = {6G3 - PETRA III (DESY) (POF4-6G3) / FS-Proposal: I-20170574
(I-20170574) / DFG project 510114039 - Dissoziationsdynamik
von rumpfniveauangeregten ionischen, molekularen Radikalen
(510114039) / 05K19GU4 - SFX2: Hochdurchsatz
Serielle-Femtosekunden Kristallographie @ EU XFEL.
(BMBF-05K19GU4)},
pid = {G:(DE-HGF)POF4-6G3 / G:(DE-H253)I-20170574 /
G:(GEPRIS)510114039 / G:(DE-Ds200)BMBF-05K19GU4},
experiment = {EXP:(DE-H253)P-P04-20150101},
typ = {PUB:(DE-HGF)16},
UT = {WOS:001204293700001},
doi = {10.3847/1538-4357/ad2939},
url = {https://bib-pubdb1.desy.de/record/607574},
}