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@ARTICLE{Lee:639756,
author = {Lee, Yun-Hee and Kim, Jin Kyun and Kim, Yongkyu and Kim,
Minju and CHO, DEOK-YONG and Husband, Rachel J. and Strohm,
Cornelius and Ehrenreich-Petersen, Emma and Glazyrin,
Konstantin and Laurus, Torsten and Graafsma, Heinz and
Bauer, Robert and Lehmkühler, Felix and Appel, Karen and
Konôpková, Zuzana and Tang, Minxue and Dwivedi, Anand and
Sztuck-Dambietz, Jolanta and Randolph, Lisa and Buakor,
Khachiwan and Humphries, Oliver and Baehtz, Carsten and
Eklund, Tobias and Mohrbach, Lisa Katharina and Mondal,
Anshuman and Marquardt, Hauke and O’Bannon, Earl Francis
and Amann-Winkel, Katrin and Yoo, Choong-Shik and Zastrau,
Ulf and Liermann, Hanns-Peter and Nada, Hiroki and Lee, Geun
Woo},
title = {{M}ultiple freezing–melting pathways of high-density ice
through ice {XXI} phase at room temperature},
journal = {Nature materials},
volume = {xxx},
number = {xxx},
issn = {1476-1122},
address = {Basingstoke},
publisher = {Nature Publishing Group},
reportid = {PUBDB-2025-04651},
pages = {xxx},
year = {2025},
note = {OnlineFirst VDB},
abstract = {Various metastable ice phases and their complicated
transition pathwayshave been found by pressurization at low
temperatures at which slowkinetics and high metastability
are easily achieved. By contrast, suchdiversity is less
expected at room or elevated temperatures. Here, using
acombination of a dynamic diamond anvil cell and X-ray free
electron lasertechniques, we demonstrate t ha t sup erco mp
ressed water transforms intoice VI through multiple
freezing–melting pathways at room temperature,hidden
within the pressure region of ice VI. These multiple
transitionpathways occur via a metastable ice (more
specifically, ice XXI withbody-centred tetragonal structure
(Ī 42d)) discovered in this study and ametastable ice VII
that exists within the pressure range of ice VI. We find
thatsupercompressed water structurally evolves from
high-density water tovery-high-density water, causing
multiple transition pathways. Thesefindings provide an
insight to find more metastable ice phases and
theirtransition pathways at elevated temperatures.},
cin = {FS-PETRA-D / FS-HIBEF / DOOR ; HAS-User / FS-DS /
$XFEL_DO_DD_DET$ / FS-SMP / $XFEL_E1_FXE$ / $XFEL_E1_HED$},
ddc = {610},
cid = {I:(DE-H253)FS-PETRA-D-20210408 /
I:(DE-H253)FS-HIBEF-20240110 / I:(DE-H253)HAS-User-20120731
/ I:(DE-H253)FS-DS-20120731 /
$I:(DE-H253)XFEL_DO_DD_DET-20210408$ /
I:(DE-H253)FS-SMP-20171124 /
$I:(DE-H253)XFEL_E1_FXE-20210408$ /
$I:(DE-H253)XFEL_E1_HED-20210408$},
pnm = {631 - Matter – Dynamics, Mechanisms and Control
(POF4-631) / 6G3 - PETRA III (DESY) (POF4-6G3) /
FS-Proposal: I-20240991 (I-20240991) / DFG project
G:(GEPRIS)329658874 - Experimentelle Untersuchung von
planetaren Eis-Verbindungen bei hohen Drücken mittels
dynamisch-betriebener Diamantstempelzellen (329658874) /
HiBEF - HIBEF Consortium $(2020_Join2-HiBEF)$ / DFG project
G:(GEPRIS)390715994 - EXC 2056: CUI: Tiefe Einblicke in
Materie (390715994) / FS-Proposal: I-20220299 (I-20220299) /
FS-Proposal: I-20221305 (I-20221305)},
pid = {G:(DE-HGF)POF4-631 / G:(DE-HGF)POF4-6G3 /
G:(DE-H253)I-20240991 / G:(GEPRIS)329658874 /
$G:(DE-HGF)2020_Join2-HiBEF$ / G:(GEPRIS)390715994 /
G:(DE-H253)I-20220299 / G:(DE-H253)I-20221305},
experiment = {EXP:(DE-H253)P-P02.2-20150101 /
EXP:(DE-H253)XFEL-HED-20150101},
typ = {PUB:(DE-HGF)16},
doi = {10.1038/s41563-025-02364-x},
url = {https://bib-pubdb1.desy.de/record/639756},
}