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@ARTICLE{Lotti:1018015,
author = {Lotti and Gatta, Diego G. and Gigli, Lara and Krüger,
Hannes and Kahlenberg, Volker and Meven, Martin and Comoni,
Davide and Milani, Sula and Merlini, Marco and Liermann,
Hanns Peter},
title = {{T}hermal and combined high-temperature and high-pressure
behavior of a natural intermediate scapolite},
journal = {American mineralogist},
volume = {109},
number = {2},
issn = {0003-004X},
address = {Alexandria, Va.},
publisher = {GeoScienceWorld},
reportid = {FZJ-2023-04485},
pages = {243–254},
year = {2024},
abstract = {A natural intermediate member of the scapolite solid
solution (Me$_{47}$; experimental chemical formula:
(Na$_{1.86}$Ca$_{1.86}$K$_{0.23}$Fe$_{0.01}$)(Al$_{4.36}$Si$_{7.64}$)O$_{24}$[Cl$_{0.48}$(CO$_3$)$_{0.48}$(SO$_4$)$_{0.01}$]),
with the unusual I4/m space group, has been studied at
various temperatures and combined high-$T$ and high-$P$ by
means of in situ single-crystal and powder X-ray
diffraction, at both conventional and synchrotron sources.
In addition, single-crystal neutron diffraction data were
collected at ambient-T and 685 °C. A fit of the
experimental V-T data with a thermal equation of state
yielded a calculated thermal expansion coefficient at
ambient conditions: $α_{V25°C} =
1/V_0·(∂V/∂T)_{P,25°C} = 1.74(3)·10^{-5}$ K$^{-1}$. A
comparative analysis of the elastic behavior of scapolite
based on this study and other high-$T$ XRD data reported in
the literature suggests that a thorough re-investigation of
the different members of the marialite-meionite solid
solution is needed to fully understand the role of crystal
chemistry on the thermal behavior of these complex
non-binary solid solutions. The experimental data obtained
within the full temperature range of analysis at ambient
pressure confirm that the investigated sample always
preserves the I4/m space group, and possible implications on
the metastability of I4/m intermediate scapolite are
discussed. Neutron diffraction data show that no significant
Si and Al re-arrangement among the T sites occurs between 25
and 685 °C. The combined high-$T$ and high-$P$ data show
that at 650 °C and between 10.30(5) and 10.71(5) GPa a
phase transition towards a triclinic polymorph occurs, with
a positive Clapeyron slope (i.e., $dP/dT > 0$). A
comprehensive description of the atomic-scale structure
deformation mechanisms induced by temperature and/or
pressure, including those leading to structural instability,
is provided based on single-crystal structure refinements.},
cin = {JCNS-FRM-II / JARA-FIT / JCNS-2 / MLZ},
ddc = {540},
cid = {I:(DE-Juel1)JCNS-FRM-II-20110218 /
$I:(DE-82)080009_20140620$ / I:(DE-Juel1)JCNS-2-20110106 /
I:(DE-588b)4597118-3},
pnm = {6G4 - Jülich Centre for Neutron Research (JCNS) (FZJ)
(POF4-6G4) / CALIPSOplus - Convenient Access to Light
Sources Open to Innovation, Science and to the World
(730872)},
pid = {G:(DE-HGF)POF4-6G4 / G:(EU-Grant)730872},
experiment = {EXP:(DE-MLZ)HEIDI-20140101 / EXP:(DE-H253)P-P02.2-20150101},
typ = {PUB:(DE-HGF)16},
UT = {WOS:001155433300013},
doi = {10.2138/am-2023-8962},
url = {https://juser.fz-juelich.de/record/1018015},
}