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The thermoelastic behavior of clintonite up to 10 GPa and 1,000°C (Articolo in rivista)
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- Label
- The thermoelastic behavior of clintonite up to 10 GPa and 1,000°C (Articolo in rivista) (literal)
- Anno
- 2012-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00269-012-0493-0 (literal)
- Alternative label
Gatta G.D., Merlini M., Liermann H-P., Rothkirch A., Gemmi M., Pavese A (2012)
The thermoelastic behavior of clintonite up to 10 GPa and 1,000°C
in Physics and chemistry of minerals
(literal)
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- Gatta G.D., Merlini M., Liermann H-P., Rothkirch A., Gemmi M., Pavese A (literal)
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- G. Diego Gatta (&) ? M. Merlini ? A. Pavese
Dipartimento of Scienze della Terra, Universita' degli Studi
di Milano, Via Botticelli, 23, 20133 Milan, Italy
e-mail: diego.gatta@unimi.it
G. Diego Gatta ? A. Pavese
CNR-Istituto per la Dinamica dei Processi Ambientali,
Milan, Italy
H.-P. Liermann ? A. Rothkirch
DESY, HASYLAB, PETRA III, Notkestr. 85,
22607 Hamburg, Germany
M. Gemmi
Center for Nanotechnology Innovation@NEST,
Istituto Italiano di Tecnologia, Pisa, Italy (literal)
- Titolo
- The thermoelastic behavior of clintonite up to 10 GPa and 1,000°C (literal)
- Abstract
- The thermoelastic behavior of a natural clintonite-1M [with composition: Ca1.01
(Mg2.29Al0.59Fe0.12
)R3.00
(Si1.20Al2.80)R4.00O10(OH)2] has been investigated up to 10
GPa (at room temperature) and up to 960?C (at room pressure) by means of in situ synchrotron single-crystal and
powder diffraction, respectively. No evidence of phase
transition has been observed within the pressure and temperature range investigated. P-V data fitted with an isothermal third-order Birch-Murnaghan equation of state
(BM-EoS) give V0 = 457.1(2) A? 3
, KT0 = 76(3)GPa, and
K
0
= 10.6(15). The evolution of the ''Eulerian finite strain''
versus ''normalized stress'' shows a linear positive trend.
The linear regression yields Fe(0) = 76(3) GPa as intercept
value, and the slope of the regression line leads to a K
0
value
of 10.6(8). The evolution of the lattice parameters with
pressure is significantly anisotropic [b(a) = 1/3KT0(a) =
0.0023(1) GPa
-1
; b(b) = 1/3KT0(b) = 0.0018(1) GPa
-1
;
b(c) = 1/KT0(c) = 0.0072(3) GPa
-1
]. The b-angle increases in response to the applied P, with: bP = b0 ? 0.033(4)
P (P in GPa). The structure refinements of clintonite up to
10.1 GPa show that, under hydrostatic pressure, the structure
rearranges by compressing mainly isotropically the interlayer Ca-polyhedron. The bulk modulus of the Ca-polyhedron, described using a second-order BM-EoS, is KT0
(Ca-polyhedron) = 41(2) GPa. The compression of the bond
distances between calcium and the basal oxygens of the
tetrahedral sheet leads, in turn, to an increase in the ditrigonal
distortion of the tetrahedral ring, with qa/qP & 0.1?/GPa
within the P-range investigated. The Mg-rich octahedra
appear to compress in response to the applied pressure,
whereas the tetrahedron appears to behave as a rigid unit. The
evolution of axial and volume thermal expansion coefficient
a with temperature was described by the polynomial
a(T) = a0 ? a1T
-1/2
. The refined parameters for clintonite
are as follows: a0 = 2.78(4) 10
-5
?C
-1
and a1 = -4.4(6)
10
-5
?C
1/2
for the unit-cell volume; a0(a) = 1.01(2)
10
-5
?C
-1
and a1(a) = -1.8(3) 10
-5
?C
1/2
for the a-axis;
a0(b) = 1.07(1) 10
-5
?C
-1
and a1(b) = -2.3(2) 10
-5
?C
1/2
for the b-axis; and a0
(c) = 0.64(2) 10
-5
?C
-1
and a1
(c) =
-7.3(30) 10
-6
?C
1/2
for the c-axis. The b-angle appears to be
almost constant within the given T-range. No structure collapsing in response to the T-induced dehydroxylation was
found up to 960?C. The HP- and HT-data of this study show
that in clintonite, the most and the less expandable directions
do not correspond to the most and the less compressible
directions, respectively. A comparison between the thermoelastic parameters of clintonite and those of true micas
was carried out. (literal)
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