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High-pressure behaviour and phase stability of Ca2B6O6(OH)10·2(H2O) (meyerhofferite)
Ist Teil von
Physics and chemistry of minerals, 2020-11, Vol.47 (11), Article 50
Ort / Verlag
Berlin/Heidelberg: Springer Berlin Heidelberg
Erscheinungsjahr
2020
Quelle
Alma/SFX Local Collection
Beschreibungen/Notizen
The high-pressure behaviour of meyerhofferite [ideally Ca
2
B
6
O
6
(OH)
10
·2(H
2
O), with
a
~ 6.63 Å,
b
~ 8.34 Å,
c
~ 6.47 Å, α = 90.8°,
β
= 102°, γ = 86.8°, Sp. Gr.
P
1
¯
], a B-bearing raw material (with B
2
O
3
≈ 46 wt%) and a potential B-rich aggregate, has been studied by single-crystal synchrotron X-ray diffraction up to 9 GPa, under hydrostatic conditions. Meyerhofferite undergoes a first-order phase transition to meyerhofferite-II, likely iso-symmetric, bracketed between 3.05 and 3.48 GPa, with a spectacular unit-cell volume discontinuity (
i.e
., Δ
V
~ 30 Å
3
). The isothermal bulk modulus (
K
V0
= β
−1
P0,T0
, where β
P0,T0
is the volume compressibility coefficient) of meyerhofferite, was found to be
K
V0
= 31.6(5) GPa, and a marked anisotropic compressional pattern, with
K
(
a)
0
:
K
(
b)
0
:
K
(
c)
0
~ 1.5:1:3, was observed. The bulk modulus of meyerhofferite-II increases to 55(2) GPa and, differently to the majority of the borates studied at high pressure so far, the anisotropic compressional pattern of meyerhofferite decreases markedly in the high-pressure form. The
P
-induced deformation mechanisms controlling, at the atomic scale, the bulk compression of meyerhofferite are here described. Considerations about the use of meyerhofferite as a potential B-based aggregate in concretes, mortars or resins, are provided.