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High-pressure behaviour and atomic-scale deformation mechanisms in inyoite, CaB3O3(OH)5·4H2O
Ist Teil von
Physics and chemistry of minerals, 2022-02, Vol.49 (2), Article 4
Ort / Verlag
Berlin/Heidelberg: Springer Berlin Heidelberg
Erscheinungsjahr
2022
Quelle
SpringerLink
Beschreibungen/Notizen
The compressional behaviour of inyoite, ideally CaB
3
O
3
(OH)
5
·4H
2
O, has been studied by an in-situ high-pressure single-crystal X-ray experiment, at the ESRF large-scale facility, up to 19.80(5) GPa. Inyoite undergoes a first-order phase transition to inyoite-II, bracketed between 8.25(5) and 8.86(5) GPa, with a large volume discontinuity (Δ
V
⁓ 7.5%). The structure of the high-pressure polymorph has not been solved due to a significant decrease in the number of Bragg reflections. The isothermal bulk modulus (
K
V
0
=
β
−1
P
0,
T
0
, where
β
P
0,
T
0
is the volume compressibility coefficient) of inyoite was found to be
K
V
0
= 26.9(8) GPa, whereas in inyoite-II, the
K
V
0
value increases to 52(5) GPa. The increase of the bulk modulus is paired with a sharp decrease of the anisotropy of compressibility, as shown by the magnitude of the Eulerian finite unit-strain ellipsoid with:
ε
1:
ε
2:
ε
3 = 3.5:2.1:1 in inyoite and
ε
1:
ε
2:
ε
3 = 1.5:1.1:1 in inyoite-II. The
P
-induced deformation mechanisms controlling, at the atomic scale, the bulk compression of inyoite are here described on the basis of a series of structure refinements.