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Polymorphs of the Gadolinite-Type Borates ZrB2 O5 and HfB2 O5 Under Extreme Pressure.


ABSTRACT: Based on the results from previous high-pressure experiments on the gadolinite-type mineral datolite, CaBSiO4 (OH), the behavior of the isostructural borates β-HfB2 O5 and β-ZrB2 O5 have been studied by synchrotron-based in situ high-pressure single-crystal X-ray diffraction experiments. On compression to 120 GPa, both borate layer-structures are preserved. Additionally, at ≈114 GPa, the formation of a second phase can be observed in both compounds. The new high-pressure modification γ-ZrB2 O5 features a rearrangement of the corner-sharing BO4 tetrahedra, while still maintaining the four- and eight-membered rings. The new phase γ-HfB2 O5 contains ten-membered rings including the rare structural motif of edge-sharing BO4 tetrahedra with exceptionally short B-O and B⋅⋅⋅B distances. For both structures, unusually high coordination numbers are found for the transition metal cations, with ninefold coordinated Hf4+ , and tenfold coordinated Zr4+ , respectively. These findings remarkably show the potential of cold compression as a low-energy pathway to discover metastable structures that exhibit new coordinations and structural motifs.

SUBMITTER: Pakhomova A 

PROVIDER: S-EPMC8049040 | biostudies-literature | 2021 Apr

REPOSITORIES: biostudies-literature

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Polymorphs of the Gadolinite-Type Borates ZrB<sub>2</sub> O<sub>5</sub> and HfB<sub>2</sub> O<sub>5</sub> Under Extreme Pressure.

Pakhomova Anna A   Fuchs Birgit B   Dubrovinsky Leonid S LS   Dubrovinskaia Natalia N   Huppertz Hubert H  

Chemistry (Weinheim an der Bergstrasse, Germany) 20210303 19


Based on the results from previous high-pressure experiments on the gadolinite-type mineral datolite, CaBSiO<sub>4</sub> (OH), the behavior of the isostructural borates β-HfB<sub>2</sub> O<sub>5</sub> and β-ZrB<sub>2</sub> O<sub>5</sub> have been studied by synchrotron-based in situ high-pressure single-crystal X-ray diffraction experiments. On compression to 120 GPa, both borate layer-structures are preserved. Additionally, at ≈114 GPa, the formation of a second phase can be observed in both co  ...[more]

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