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Equation of State and Phase Transition of (Mg0.92, Fe0.08)SiO3 Enstatite under Shock Compression and Its Geophysical Implications
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Jin-Ke YANG1, Zi-Zheng GONG1, 2, Li-Wei DENG1, 3, Li ZHANG1, 3, Ying-Wei FEI3
Chinese Journal of High Pressure Physics | 2007, 21(1) : 45 - 54
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Chinese Journal of High Pressure Physics | 2007, 21(1): 45-54
Equation of State and Phase Transition of (Mg0.92, Fe0.08)SiO3 Enstatite under Shock Compression and Its Geophysical Implications
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Jin-Ke YANG1, Zi-Zheng GONG1, 2, Li-Wei DENG1, 3, Li ZHANG1, 3, Ying-Wei FEI3
Affiliations
  • 1.Institute of High Pressure & High Temperature Physics, Southwest Jiaotong University, Chengdu 610031, China
  • 2.Beijing Institute of Spacecraft Environment Engineering, Beijing 100094, China
  • 3.Geophysical Laboratory, Carnegie Institution of Washington, Washington DC 20015, USA
Published: 2007-03-05
Outline
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We performed shock wave experiments on a natural pyroxene with chemical composition close to (Mg0.92, Fe0.08)SiO3 and initial density of 3.06 g/cm3 at pressures between 48 and 140 GPa, using impedance-match method and electrical probe technique. Considering McQueen et. al. data, it is obvious that (Mg0.92, Fe0.08)SiO3 goes through three phase regions in the procedure of shock compression: Low-pressure phase region (LPR), mixed phase region (MPR), and high-pressure phase region (HPR), corresponding to the pressure 0~40 GPa, 40~67 GPa and 68~140 GPa, respectively. In low-pressure phase region, the relationship between shock wave velocity D and particle velocity u was expressed by McQueen et. al. data. Then in high-pressure phase region (at pressures between 68 to 140 GPa), it can be described linearly from our experiment data. The calculated D-u relationship for the assemblage of (Mg0.92, Fe0.08)O(Mw)+SiO2(St) is significantly different from the experimental data, excluding the possibility of chemical decomposition of perovskite to oxides during the shock compression. The Grüneisen parameter γ can be obtained by fitting the experimental data. Using the third-order Birch-Murnaghan finite strain equation of state, the shock experimental data yield a zero-pressure bulk modulus K0S=259.6(9) GPa and its pressure derivative K′0S=4.20(5), with ρ0=4.19 g/cm3. A comparison of the experimental Hugoniot densities of perovskite with the PREM density profile prefers a perovskite-dominant lower mantle model.

(Mg0.92, Fe0.08)SiO3-perovskite  /  shock compression  /  equation of state  /  phase stability  /  lower mantle
杨金科, 龚自正, 邓力维, 张莉, 费英伟. 顽火辉石(Mg0.92,Fe0.08)SiO3的冲击相变和高压状态方程及其地球物理意义. 高压物理学报, 2007 , 21 (1) : 45 -54 .
Jin-Ke YANG, Zi-Zheng GONG, Li-Wei DENG, Li ZHANG, Ying-Wei FEI. Equation of State and Phase Transition of (Mg0.92, Fe0.08)SiO3 Enstatite under Shock Compression and Its Geophysical Implications[J]. Chinese Journal of High Pressure Physics, 2007 , 21 (1) : 45 -54 .
Year 2007 volume 21 Issue 1
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Article Info
  • Receive Date:2005-10-12
  • Online Date:2026-11-01
  • Published:2007-03-05
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  • Received:2005-10-12
  • Revised:2006-01-12
Funding
Affiliations
    1.Institute of High Pressure & High Temperature Physics, Southwest Jiaotong University, Chengdu 610031, China
    2.Beijing Institute of Spacecraft Environment Engineering, Beijing 100094, China
    3.Geophysical Laboratory, Carnegie Institution of Washington, Washington DC 20015, USA
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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