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On the crystal structure and compressional behavior of talc: a mineral of interest in petrology and material science
by
Pavese, Alessandro
, Nénert, Gwilherm
, Valdrè, Giovanni
, Gatta, G. Diego
, Kahlenberg, Volker
, Liermann, Hanns-Peter
, Merlini, Marco
, Rothkirch, André
in
Compressibility
/ Crystal structure
/ Crystallography and Scattering Methods
/ Diamond anvil cells
/ Earth and Environmental Science
/ Earth Sciences
/ Elastic anisotropy
/ Elasticity
/ Equations of state
/ Geochemistry
/ Hydrogen bonding
/ Hydroxyl groups
/ Mineral Resources
/ Mineralogy
/ Neutron diffraction
/ Neutrons
/ Original Paper
/ Petrology
/ Phase transitions
/ Single crystals
/ Talc
/ Tetrahedra
/ X-ray diffraction
2013
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On the crystal structure and compressional behavior of talc: a mineral of interest in petrology and material science
by
Pavese, Alessandro
, Nénert, Gwilherm
, Valdrè, Giovanni
, Gatta, G. Diego
, Kahlenberg, Volker
, Liermann, Hanns-Peter
, Merlini, Marco
, Rothkirch, André
in
Compressibility
/ Crystal structure
/ Crystallography and Scattering Methods
/ Diamond anvil cells
/ Earth and Environmental Science
/ Earth Sciences
/ Elastic anisotropy
/ Elasticity
/ Equations of state
/ Geochemistry
/ Hydrogen bonding
/ Hydroxyl groups
/ Mineral Resources
/ Mineralogy
/ Neutron diffraction
/ Neutrons
/ Original Paper
/ Petrology
/ Phase transitions
/ Single crystals
/ Talc
/ Tetrahedra
/ X-ray diffraction
2013
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On the crystal structure and compressional behavior of talc: a mineral of interest in petrology and material science
by
Pavese, Alessandro
, Nénert, Gwilherm
, Valdrè, Giovanni
, Gatta, G. Diego
, Kahlenberg, Volker
, Liermann, Hanns-Peter
, Merlini, Marco
, Rothkirch, André
in
Compressibility
/ Crystal structure
/ Crystallography and Scattering Methods
/ Diamond anvil cells
/ Earth and Environmental Science
/ Earth Sciences
/ Elastic anisotropy
/ Elasticity
/ Equations of state
/ Geochemistry
/ Hydrogen bonding
/ Hydroxyl groups
/ Mineral Resources
/ Mineralogy
/ Neutron diffraction
/ Neutrons
/ Original Paper
/ Petrology
/ Phase transitions
/ Single crystals
/ Talc
/ Tetrahedra
/ X-ray diffraction
2013
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On the crystal structure and compressional behavior of talc: a mineral of interest in petrology and material science
Journal Article
On the crystal structure and compressional behavior of talc: a mineral of interest in petrology and material science
2013
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Overview
The crystal structure of a natural triclinic talc (1
Tc
polytype) [with composition: (Mg
2.93
Fe
0.06
)
Σ2.99
(Al
0.02
Si
3.97
)
Σ3.99
O
10
(OH)
2.10
] has been investigated by single-crystal X-ray diffraction at 223 and 170 K and by single-crystal neutron diffraction at 20 K. Both the anisotropic X-ray refinements (i.e. at 223 and 170 K) show that the two independent tetrahedra are only slightly distorted. For the two independent Mg-octahedra, the bond distances between cation-hydroxyl groups are significantly shorter than the others. The ditrigonal rotation angle of the six-membered ring of tetrahedra is modest (
α
~ 4°). The neutron structure refinement shows that the hydrogen-bonding scheme in talc consists of one donor site and three acceptors (i.e. trifurcated configuration), all the bonds having O···O ≤ 3.38 Å, H···O ~ 2.8 Å, and O–H···O ~ 111–116°. The three acceptors belong to the six-membered ring of tetrahedra juxtaposed to the octahedral sheet. The vibrational regime of the proton site appears being only slightly anisotropic. The elastic behavior of talc was investigated by means of in situ synchrotron single-crystal diffraction up to 16 GPa (at room temperature) using a diamond anvil cell. No evidence of phase transition has been observed within the pressure range investigated.
P
–
V
data fit, with an isothermal third-order Birch-Murnaghan equation of state, results as follows:
V
0
= 454.7(10) Å
3
,
K
T0
= 56(3) GPa, and
K
′ = 5.4(7). The “Eulerian finite strain” versus “normalized stress” plot yields:
Fe
(0) = 56(2) GPa and
K
′ = 5.3(5). The compressional behavior of talc is strongly anisotropic, as reflected by the axial compressibilities (i.e.
β
(
a
):
β
(
b
):
β
(
c
) = 1.03:1:3.15) as well as by the magnitude and orientation of the unit-strain ellipsoid (with
ε
1
:
ε
2
:
ε
3
= 1:1.37:3.21). A comparison between the elastic parameters of talc obtained in this study with those previously reported is carried out.
Publisher
Springer-Verlag,Springer Nature B.V
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