High-pressure behavior and stability of synthetic buetschliite K<sub>2</sub>Ca(CO<sub>3</sub>)<sub>2</sub> up to 19 GPa and 300°C

Autor(en)
Anna Yu Likhacheva, Sofija Miloš, Alexandr V. Romanenko, Sergey V. Goryainov, Anna I. Semerikova, Sergey V. Rashchenko, Ronald Miletich, Anton Shatsky
Abstrakt

The occurrence of buetschliite, K2Ca(CO3)2, as inclusions in mantle minerals, is considered as one of the keys to understanding phase relationships of dense carbonates and outlines the potential role of potassium carbonates in the Earth's deep carbon cycle. Within this scope, the high-pressure behavior of synthetic buetschliite is characterized by in situ Raman spectroscopy up to 19 GPa and 300°C. Up to 6 GPa, the compression is regular, then the splitting of some of the lattice and internal modes defines the transition to a low-symmetry phase, in analogy to that observed previously in K2Mg(CO3)2. The temperature rise to 300°C shifts the transition pressure from ~6 to ~8 GPa, but on the whole, it does not change the high-pressure behavior of K2Ca(CO3)2. The observed pressure-induced spectral changes are fully reversible at room and elevated temperature. The findings show the expansion of buetschliite baric stability with temperature, which confirms its importance as a constituent of carbonate inclusions in deep minerals.

Organisation(en)
Institut für Mineralogie und Kristallographie
Externe Organisation(en)
Russian Academy of Sciences, Novosibirsk State University (NSU)
Journal
Journal of Raman Spectroscopy
Band
55
Seiten
517-524
Anzahl der Seiten
8
ISSN
0377-0486
Publikationsdatum
01-2024
Peer-reviewed
Ja
ÖFOS 2012
105116 Mineralogie, 105113 Kristallographie, 104026 Spektroskopie
Schlagwörter
ASJC Scopus Sachgebiete
Allgemeine Materialwissenschaften, Spectroscopy
Link zum Portal
https://ucrisportal.univie.ac.at/de/publications/787b6587-c27e-462b-9616-1783ba8f9fec