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@ARTICLE{Kaa:480798,
author = {Kaa, Johannes M. and Sternemann, Christian and Appel, Karen
and Cerantola, Valerio and Preston, Thomas and Albers,
Christian and Elbers, Mirko and Libon, Lélia and Makita,
Mikako and Pelka, Alexander and Petitgirard, Sylvain and
Plückthun, Christian and Roddatis, Vladimir and Sahle,
Christoph J. and Spiekermann, Georg and Schmidt, Christian
and Schreiber, Anja and Sakrowski, Robin and Tolan, Metin
and Wilke, Max and Zastrau, Ulf and Konôpková, Zuzana},
title = {{S}tructural and electron spin state changes in an x-ray
heated iron carbonate system at the {E}arth's lower mantle
pressures},
journal = {Physical review research},
volume = {4},
number = {3},
issn = {2643-1564},
address = {College Park, MD},
publisher = {APS},
reportid = {PUBDB-2022-03971},
pages = {033042},
year = {2022},
abstract = {The determination of the spin state of iron-bearing
compounds at high pressure and temperature is crucial for
our understanding of chemical and physical properties of the
deep Earth. Studies on the relationship between the
coordination of iron and its electronic spin structure in
iron-bearing oxides, silicates, carbonates, iron alloys, and
other minerals found in the Earth's mantle and core are
scarce because of the technical challenges to simultaneously
probe the sample at high pressures and temperatures. We used
the unique properties of a pulsed and highly brilliant x-ray
free electron laser (XFEL) beam at the High Energy Density
(HED) instrument of the European XFEL to x-ray heat and
probe samples contained in a diamond anvil cell. We heated
and probed with the same x-ray pulse train and
simultaneously measured x-ray emission and x-ray diffraction
of an FeCO$_3$ sample at a pressure of 51 GPa with up to
melting temperatures. We collected spin state sensitive Fe
Kβ$_{1,3}$ fluorescence spectra and detected the sample's
structural changes via diffraction, observing the inverse
volume collapse across the spin transition. During x-ray
heating, the carbonate transforms into orthorhombic
Fe$_4$C$_3$O$_{12}$ and iron oxides. Incipient melting was
also observed. This approach to collect information about
the electronic state and structural changes from samples
contained in a diamond anvil cell at melting temperatures
and above will considerably improve our understanding of the
structure and dynamics of planetary and exoplanetary
interiors.},
cin = {DOOR ; HAS-User / $XFEL_E1_HED$},
ddc = {530},
cid = {I:(DE-H253)HAS-User-20120731 /
$I:(DE-H253)XFEL_E1_HED-20210408$},
pnm = {6G3 - PETRA III (DESY) (POF4-6G3)},
pid = {G:(DE-HGF)POF4-6G3},
experiment = {EXP:(DE-H253)XFEL-HED-20150101 /
EXP:(DE-H253)P-P02.2-20150101 / EXP:(DE-H253)P-P01-20150101},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000829259500003},
doi = {10.1103/PhysRevResearch.4.033042},
url = {https://bib-pubdb1.desy.de/record/480798},
}