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Elastic P Wave Velocity and Attenuation in Dunite up to 4.0 GPa
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Wei LIU1, 2, Jian-Guo DU1, Hong-Sen XIE3, Wen-Ge ZHOU3, Jie GUO3
Chinese Journal of High Pressure Physics | 2005, 19(4) : 293 - 298
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Chinese Journal of High Pressure Physics | 2005, 19(4): 293-298
Elastic P Wave Velocity and Attenuation in Dunite up to 4.0 GPa
Full
Wei LIU1, 2, Jian-Guo DU1, Hong-Sen XIE3, Wen-Ge ZHOU3, Jie GUO3
Affiliations
  • 1.Institute of Earthquake Sciences, China Earthquake Administration, Beijing 100036, China
  • 2.Mineral Physics Institute, State University of New York at Stony Brook, New York 11794, USA
  • 3.Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
Published: 2005-12-05
Outline
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Elastic P wave velocity (vP) and quality factor value (QP, on behalf of attenuation) of dunite are determined using ultrasonic pulse transmission and spectral ratio methods in a multi-anvil apparatus up to 4.0 GPa at room temperature. During the experimental pressure range (0.4~4.0 GPa), vP and QP increase about 11.8% (from 7.6 km/s to 8.5 km/s) and 393.3% (from 54 to 266.4). The experimental results show that vP and QP are pressure dependent and a greater rising rate at the lower pressures than that at higher pressures: the increase rate of Qp at 0.4~2.4 GPa is 358.5%, while only 7.6% at 2.4~4.0 GPa. At the lower pressures, the pores with low aspect ratio in rocks are easy to close, and almost all of them would close with the pressure increasing. As a result, the samples show the internal inherent elasticity of the whole constituent minerals themselves and the increasing rate of vP turns lower at the higher pressures. As the pressure rising (0.4~2.4 GPa), QP of dunite increases because the energy loss in the pores and between the surfaces of cracks and the mineral boundaries is reduced due to the porosity decreasing and the mineral boundaries contact more tightly. While at higher pressures (2.4~4.0 GPa), most microcracks in dunite have been closed and mineral grains are compacted very tightly, as a result the internal frictional energy loss due to the relative motion at the grain boundaries and across crack surfaces became less, which results in small change of elastic wave attenuation in dunite.

high pressure  /  P wave velocity  /  attenuation  /  quality factor
刘巍, 杜建国, 谢鸿森, 周文戈, 郭捷. 4.0 GPa压力下纯橄岩弹性纵波速度和衰减的实验研究. 高压物理学报, 2005 , 19 (4) : 293 -298 .
Wei LIU, Jian-Guo DU, Hong-Sen XIE, Wen-Ge ZHOU, Jie GUO. Elastic P Wave Velocity and Attenuation in Dunite up to 4.0 GPa[J]. Chinese Journal of High Pressure Physics, 2005 , 19 (4) : 293 -298 .
Year 2005 volume 19 Issue 4
31
10
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Article Info
  • Receive Date:2004-11-01
  • Online Date:2026-11-01
  • Published:2005-12-05
Article Data
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History
  • Received:2004-11-01
  • Revised:2005-01-07
Funding
Affiliations
    1.Institute of Earthquake Sciences, China Earthquake Administration, Beijing 100036, China
    2.Mineral Physics Institute, State University of New York at Stony Brook, New York 11794, USA
    3.Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
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Citations
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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