压力对纯的和含硫化亚铁的橄榄石电导率影响的实验研究

刘长财 胡海英 代立东 孙文清

刘长财, 胡海英, 代立东, 孙文清. 压力对纯的和含硫化亚铁的橄榄石电导率影响的实验研究[J]. 高压物理学报, 2019, 33(5): 051201. doi: 10.11858/gywlxb.20180674
引用本文: 刘长财, 胡海英, 代立东, 孙文清. 压力对纯的和含硫化亚铁的橄榄石电导率影响的实验研究[J]. 高压物理学报, 2019, 33(5): 051201. doi: 10.11858/gywlxb.20180674
LIU Changcai, HU Haiying, DAI Lidong, SUN Wenqing. Experimental Study on the Effect of Pressure on the Electrical Conductivity of Pure and Iron Sulfide-Bearing Olivine[J]. Chinese Journal of High Pressure Physics, 2019, 33(5): 051201. doi: 10.11858/gywlxb.20180674
Citation: LIU Changcai, HU Haiying, DAI Lidong, SUN Wenqing. Experimental Study on the Effect of Pressure on the Electrical Conductivity of Pure and Iron Sulfide-Bearing Olivine[J]. Chinese Journal of High Pressure Physics, 2019, 33(5): 051201. doi: 10.11858/gywlxb.20180674

压力对纯的和含硫化亚铁的橄榄石电导率影响的实验研究

doi: 10.11858/gywlxb.20180674
基金项目: 国家自然科学基金(41772042,41774099,41474078);中国科学院前沿科学重点研究项目(QYZDB-SSW-DQC009);国家重点研究发展项目(2016YFC0601101)
详细信息
    作者简介:

    刘长财(1992-),男,硕士研究生,主要从事高温高压下矿物岩石电学性质研究. E-mail:liuchangcai@mail.gyig.ac.cn

    通讯作者:

    胡海英(1983-),女,博士,副研究员,主要从事高温高压下矿物岩石物理性质研究. E-mail:huhaiying@vip.gyig.ac.cn

  • 中图分类号: P319.2

Experimental Study on the Effect of Pressure on the Electrical Conductivity of Pure and Iron Sulfide-Bearing Olivine

  • 摘要: 在YJ-3000 t紧装式六面顶大腔体压机上,用Solartron-1260阻抗/增益-相位分析仪,在1~3 GPa、723~1273 K的条件下,原位测量了纯的和含15%(质量分数)FeS的橄榄石电导率。实验结果表明:在实验温度范围内,含15% FeS的橄榄石电导率比纯橄榄石的电导率高2~3个数量级,且电导率值在0.1~10 S/m范围内;纯的和含15% FeS的橄榄石电导率都随着温度的增加而增大,但是纯的橄榄石电导率对温度的敏感性更强;纯的和含15% FeS的橄榄石电导率随压力变化表现出相反的特性,随着压力的升高,纯橄榄石电导率微弱地降低,而含15% FeS的橄榄石电导率显著地增加。由含15% FeS的橄榄石电导率对温度、压力的效应以及实验获得的活化焓可知,15% FeS在橄榄石中形成了相互连通的网络,主导着橄榄石的导电过程。

     

  • 图  实验样品组装图

    Figure  1.  Experimental setup for electrical conductivity measurements

    图  (a)纯橄榄石和(b)含15% FeS的橄榄石的背散射图

    Figure  2.  Backscattered electron images of (a) pure olivine and (b)15% FeS–bearing olivine

    图  不同温度压力条件下纯橄榄石和含15% FeS的橄榄石复阻抗谱的对比

    Figure  3.  Comparison of complex impedance spectra of pure olivine and 15% FeS–bearing olivine under different temperature and pressure conditions

    图  纯的和含15% FeS橄榄石的电导率对数与温度倒数的关系

    Figure  4.  Logarithm of electrical conductivity reciprocal temperature for pure olivine and 15% FeS–bearing olivine at different pressures

    图  活化焓与压力的关系

    Figure  5.  Activation enthalpy versus pressure

    表  1  样品电导率的Arrhenius关系拟合参数

    Table  1.   Fitted parameters of Arrhenius relation for the electrical conductivity of samples

    Samplep/GPaT/Klg $\sigma_0 $$\sigma_0 $/(S∙m−1)${\Delta H}/{\rm{eV}}$${\gamma^2}$
    1723–12732.53338.841.180.9913
    Olivine2723–12731.96 91.201.110.9781
    3723–12731.05 11.221.030.9867
    1723–12730.47 2.950.200.9953
    FeS-bearing olivine2723–11731.73 53.700.290.9802
    3723–10732.78602.560.390.9845
     Note: ${\gamma}^2 $—adjust R-square.
    下载: 导出CSV
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出版历程
  • 收稿日期:  2018-11-05
  • 修回日期:  2019-01-09

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