The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene

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The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene. / Nestola, F.; Boffa Ballaran, T.; Balic Zunic, Tonci; Secco, L.; Dal Negro, A.

In: American Mineralogist, Vol. 93, No. 4, 2008, p. 644-652.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Nestola, F, Boffa Ballaran, T, Balic Zunic, T, Secco, L & Dal Negro, A 2008, 'The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene', American Mineralogist, vol. 93, no. 4, pp. 644-652. https://doi.org/10.2138/am.2008.2693

APA

Nestola, F., Boffa Ballaran, T., Balic Zunic, T., Secco, L., & Dal Negro, A. (2008). The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene. American Mineralogist, 93(4), 644-652. https://doi.org/10.2138/am.2008.2693

Vancouver

Nestola F, Boffa Ballaran T, Balic Zunic T, Secco L, Dal Negro A. The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene. American Mineralogist. 2008;93(4):644-652. https://doi.org/10.2138/am.2008.2693

Author

Nestola, F. ; Boffa Ballaran, T. ; Balic Zunic, Tonci ; Secco, L. ; Dal Negro, A. / The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene. In: American Mineralogist. 2008 ; Vol. 93, No. 4. pp. 644-652.

Bibtex

@article{65488650ea3d11deba73000ea68e967b,
title = "The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene",
abstract = "A single crystal of a natural orthopyroxene with composition M2[Fe2+0.818Mg0.156Ca0.010Mn0.016]M1[Fe2+0.081 Mg0.767Al0.084Fe3+0.068]TA[Si]TB[Si0.848Al0.152]O6 and space group Pbca (sample S95) was investigated at high pressure by X-ray diffraction using a diamond-anvil cell up to 9.56 GPa. No phase transitions were detected in the pressure range investigated. The unit-cell parameters, a, b, and c, decrease non-linearly with pressure and show an axial compression anisotropy with a ratio {\ss}a:{\ss}b:{\ss}c = 1.00:1.64:1.16. The unit-cell volume decreases non-linearly as well and with a negative variation, by about 6.3% up to 9.56 GPa. The equation of state calculated using high-accuracy volume-pressure data up to 5.5 GPa gave the following coefficients: V0 = 846.02(4) {\AA}3, KT0 = 115.4(6) GPa, K' = 7.7(3). Among the Mg-orthopyroxenes investigated at high pressure so far S95 shows the highest bulk modulus. Six complete intensity data were collected at 0, 0.16, 1.72, 3.95, 8.03, and 9.56 GPa. The results confirm previous conclusions regarding the compressional mechanism in orthopyroxenes. At lower pressures, compression is mostly connected to a decrease in volume of the two M-coordination octahedra, accompanied by an increased kink in the B-tetrahedral chain. At higher pressures, compression of the M sites decreases, the kink of the tetrahedral chains stops to change, and reduction in unit-cell volume is accompanied mainly by compression of tetrahedra. This change in compressional trends results in a relatively large K' parameter and a pronounced stiffening of the structure with pressure. The presence of Al in the TB tetrahedral site influences the kink of the B tetrahedral chain, which depends on the ratio of sizes of the M2 and TB coordination polyhedra. The increased stiffness of the M polyhedra, caused by the presence of Fe, is the main reason for the high bulk modulus of S95 and its resistance to shortening of the c axis. This explains the limited shortening of the c axis in S95 and the different compressional axial anisotropy with respect to other orthopyroxenes investigated under high pressure. ",
keywords = "Faculty of Science, Orthopyroxene, r{\o}ntgendiffraktion, krystal strukturer, Orthopyroxene, X-ray diffraction, crystal structure, high pressure",
author = "F. Nestola and {Boffa Ballaran}, T. and {Balic Zunic}, Tonci and L. Secco and {Dal Negro}, A.",
year = "2008",
doi = "10.2138/am.2008.2693",
language = "English",
volume = "93",
pages = "644--652",
journal = "American Mineralogist",
issn = "0003-004X",
publisher = "Mineralogical Society of America",
number = "4",

}

RIS

TY - JOUR

T1 - The high-pressure behavior of an Al- and Fe-rich natural orthopyroxene

AU - Nestola, F.

AU - Boffa Ballaran, T.

AU - Balic Zunic, Tonci

AU - Secco, L.

AU - Dal Negro, A.

PY - 2008

Y1 - 2008

N2 - A single crystal of a natural orthopyroxene with composition M2[Fe2+0.818Mg0.156Ca0.010Mn0.016]M1[Fe2+0.081 Mg0.767Al0.084Fe3+0.068]TA[Si]TB[Si0.848Al0.152]O6 and space group Pbca (sample S95) was investigated at high pressure by X-ray diffraction using a diamond-anvil cell up to 9.56 GPa. No phase transitions were detected in the pressure range investigated. The unit-cell parameters, a, b, and c, decrease non-linearly with pressure and show an axial compression anisotropy with a ratio ßa:ßb:ßc = 1.00:1.64:1.16. The unit-cell volume decreases non-linearly as well and with a negative variation, by about 6.3% up to 9.56 GPa. The equation of state calculated using high-accuracy volume-pressure data up to 5.5 GPa gave the following coefficients: V0 = 846.02(4) Å3, KT0 = 115.4(6) GPa, K' = 7.7(3). Among the Mg-orthopyroxenes investigated at high pressure so far S95 shows the highest bulk modulus. Six complete intensity data were collected at 0, 0.16, 1.72, 3.95, 8.03, and 9.56 GPa. The results confirm previous conclusions regarding the compressional mechanism in orthopyroxenes. At lower pressures, compression is mostly connected to a decrease in volume of the two M-coordination octahedra, accompanied by an increased kink in the B-tetrahedral chain. At higher pressures, compression of the M sites decreases, the kink of the tetrahedral chains stops to change, and reduction in unit-cell volume is accompanied mainly by compression of tetrahedra. This change in compressional trends results in a relatively large K' parameter and a pronounced stiffening of the structure with pressure. The presence of Al in the TB tetrahedral site influences the kink of the B tetrahedral chain, which depends on the ratio of sizes of the M2 and TB coordination polyhedra. The increased stiffness of the M polyhedra, caused by the presence of Fe, is the main reason for the high bulk modulus of S95 and its resistance to shortening of the c axis. This explains the limited shortening of the c axis in S95 and the different compressional axial anisotropy with respect to other orthopyroxenes investigated under high pressure.

AB - A single crystal of a natural orthopyroxene with composition M2[Fe2+0.818Mg0.156Ca0.010Mn0.016]M1[Fe2+0.081 Mg0.767Al0.084Fe3+0.068]TA[Si]TB[Si0.848Al0.152]O6 and space group Pbca (sample S95) was investigated at high pressure by X-ray diffraction using a diamond-anvil cell up to 9.56 GPa. No phase transitions were detected in the pressure range investigated. The unit-cell parameters, a, b, and c, decrease non-linearly with pressure and show an axial compression anisotropy with a ratio ßa:ßb:ßc = 1.00:1.64:1.16. The unit-cell volume decreases non-linearly as well and with a negative variation, by about 6.3% up to 9.56 GPa. The equation of state calculated using high-accuracy volume-pressure data up to 5.5 GPa gave the following coefficients: V0 = 846.02(4) Å3, KT0 = 115.4(6) GPa, K' = 7.7(3). Among the Mg-orthopyroxenes investigated at high pressure so far S95 shows the highest bulk modulus. Six complete intensity data were collected at 0, 0.16, 1.72, 3.95, 8.03, and 9.56 GPa. The results confirm previous conclusions regarding the compressional mechanism in orthopyroxenes. At lower pressures, compression is mostly connected to a decrease in volume of the two M-coordination octahedra, accompanied by an increased kink in the B-tetrahedral chain. At higher pressures, compression of the M sites decreases, the kink of the tetrahedral chains stops to change, and reduction in unit-cell volume is accompanied mainly by compression of tetrahedra. This change in compressional trends results in a relatively large K' parameter and a pronounced stiffening of the structure with pressure. The presence of Al in the TB tetrahedral site influences the kink of the B tetrahedral chain, which depends on the ratio of sizes of the M2 and TB coordination polyhedra. The increased stiffness of the M polyhedra, caused by the presence of Fe, is the main reason for the high bulk modulus of S95 and its resistance to shortening of the c axis. This explains the limited shortening of the c axis in S95 and the different compressional axial anisotropy with respect to other orthopyroxenes investigated under high pressure.

KW - Faculty of Science

KW - Orthopyroxene

KW - røntgendiffraktion

KW - krystal strukturer

KW - Orthopyroxene

KW - X-ray diffraction

KW - crystal structure

KW - high pressure

U2 - 10.2138/am.2008.2693

DO - 10.2138/am.2008.2693

M3 - Journal article

VL - 93

SP - 644

EP - 652

JO - American Mineralogist

JF - American Mineralogist

SN - 0003-004X

IS - 4

ER -

ID: 16304037