New accurate compression data for γ-Fe2SiO4

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New accurate compression data for γ-Fe2SiO4. / Nestola, Fabrizio; Boffa-Ballaran, Tiziana; Koch-Müller, Monika; Balic Zunic, Tonci; Taran, Michael; Olsen, Lars Arnskov; Princivalle, Francesco; Secco, Luciano; Lundegaard, Lars.

I: Physics of the Earth and Planetary Interiors, Bind 183, Nr. 3-4, 2010, s. 421-425.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Nestola, F, Boffa-Ballaran, T, Koch-Müller, M, Balic Zunic, T, Taran, M, Olsen, LA, Princivalle, F, Secco, L & Lundegaard, L 2010, 'New accurate compression data for γ-Fe2SiO4', Physics of the Earth and Planetary Interiors, bind 183, nr. 3-4, s. 421-425. https://doi.org/10.1016/j.pepi.2010.09.007

APA

Nestola, F., Boffa-Ballaran, T., Koch-Müller, M., Balic Zunic, T., Taran, M., Olsen, L. A., Princivalle, F., Secco, L., & Lundegaard, L. (2010). New accurate compression data for γ-Fe2SiO4. Physics of the Earth and Planetary Interiors, 183(3-4), 421-425. https://doi.org/10.1016/j.pepi.2010.09.007

Vancouver

Nestola F, Boffa-Ballaran T, Koch-Müller M, Balic Zunic T, Taran M, Olsen LA o.a. New accurate compression data for γ-Fe2SiO4. Physics of the Earth and Planetary Interiors. 2010;183(3-4):421-425. https://doi.org/10.1016/j.pepi.2010.09.007

Author

Nestola, Fabrizio ; Boffa-Ballaran, Tiziana ; Koch-Müller, Monika ; Balic Zunic, Tonci ; Taran, Michael ; Olsen, Lars Arnskov ; Princivalle, Francesco ; Secco, Luciano ; Lundegaard, Lars. / New accurate compression data for γ-Fe2SiO4. I: Physics of the Earth and Planetary Interiors. 2010 ; Bind 183, Nr. 3-4. s. 421-425.

Bibtex

@article{72904f31733b4bfbb1e95d4f870c5cd9,
title = "New accurate compression data for γ-Fe2SiO4",
abstract = "The equation of state for ¿-Fe2SiO4 was determined by single-crystal X-ray diffraction up to 10.2 GPa at room temperature. The pressure–volume data, measured at 10 different pressures, do not show any evidence of a phase transformation and were fit by a third-order Birch–Murnaghan equation of state. The following coefficients were refined simultaneously: V0 = 559.44(6) {\AA}3, KT0 = 187.3(1.7) GPa, and K' = 5.5(4). This result implies that the Mg/Fe substitution along the ¿-Fo–Fa join does not significantly affect the bulk modulus. The sample shows higher K' than other compositions along the Fo–Fa join, which generally have K' ~4. Based on our results we can calculate the sound bulk velocity of ¿-Fe2SiO4 up to the pressures of the Transition Zone. Due to the larger K' of ¿-Fe2SiO4, the difference in bulk sound velocity between the two end-members decreases with increasing pressure.",
author = "Fabrizio Nestola and Tiziana Boffa-Ballaran and Monika Koch-M{\"u}ller and {Balic Zunic}, Tonci and Michael Taran and Olsen, {Lars Arnskov} and Francesco Princivalle and Luciano Secco and Lars Lundegaard",
year = "2010",
doi = "10.1016/j.pepi.2010.09.007",
language = "English",
volume = "183",
pages = "421--425",
journal = "Physics of the Earth and Planetary Interiors",
issn = "0031-9201",
publisher = "Elsevier",
number = "3-4",

}

RIS

TY - JOUR

T1 - New accurate compression data for γ-Fe2SiO4

AU - Nestola, Fabrizio

AU - Boffa-Ballaran, Tiziana

AU - Koch-Müller, Monika

AU - Balic Zunic, Tonci

AU - Taran, Michael

AU - Olsen, Lars Arnskov

AU - Princivalle, Francesco

AU - Secco, Luciano

AU - Lundegaard, Lars

PY - 2010

Y1 - 2010

N2 - The equation of state for ¿-Fe2SiO4 was determined by single-crystal X-ray diffraction up to 10.2 GPa at room temperature. The pressure–volume data, measured at 10 different pressures, do not show any evidence of a phase transformation and were fit by a third-order Birch–Murnaghan equation of state. The following coefficients were refined simultaneously: V0 = 559.44(6) Å3, KT0 = 187.3(1.7) GPa, and K' = 5.5(4). This result implies that the Mg/Fe substitution along the ¿-Fo–Fa join does not significantly affect the bulk modulus. The sample shows higher K' than other compositions along the Fo–Fa join, which generally have K' ~4. Based on our results we can calculate the sound bulk velocity of ¿-Fe2SiO4 up to the pressures of the Transition Zone. Due to the larger K' of ¿-Fe2SiO4, the difference in bulk sound velocity between the two end-members decreases with increasing pressure.

AB - The equation of state for ¿-Fe2SiO4 was determined by single-crystal X-ray diffraction up to 10.2 GPa at room temperature. The pressure–volume data, measured at 10 different pressures, do not show any evidence of a phase transformation and were fit by a third-order Birch–Murnaghan equation of state. The following coefficients were refined simultaneously: V0 = 559.44(6) Å3, KT0 = 187.3(1.7) GPa, and K' = 5.5(4). This result implies that the Mg/Fe substitution along the ¿-Fo–Fa join does not significantly affect the bulk modulus. The sample shows higher K' than other compositions along the Fo–Fa join, which generally have K' ~4. Based on our results we can calculate the sound bulk velocity of ¿-Fe2SiO4 up to the pressures of the Transition Zone. Due to the larger K' of ¿-Fe2SiO4, the difference in bulk sound velocity between the two end-members decreases with increasing pressure.

U2 - 10.1016/j.pepi.2010.09.007

DO - 10.1016/j.pepi.2010.09.007

M3 - Journal article

VL - 183

SP - 421

EP - 425

JO - Physics of the Earth and Planetary Interiors

JF - Physics of the Earth and Planetary Interiors

SN - 0031-9201

IS - 3-4

ER -

ID: 34371655