高温高压下蛇纹岩电导率的初步研究

刘在洋 王多君 李和平 郭颖星 于英杰

刘在洋, 王多君, 李和平, 郭颖星, 于英杰. 高温高压下蛇纹岩电导率的初步研究[J]. 高压物理学报, 2011, 25(2): 147-152 . doi: 10.11858/gywlxb.2011.02.010
引用本文: 刘在洋, 王多君, 李和平, 郭颖星, 于英杰. 高温高压下蛇纹岩电导率的初步研究[J]. 高压物理学报, 2011, 25(2): 147-152 . doi: 10.11858/gywlxb.2011.02.010
LIU Zai-Yang, WANG Duo-Jun, LI He-Ping, GUO Ying-Xing, YU Ying-Jie. A Preliminary Study on Conductivity of Serpentinite at High Pressure and High Temperature[J]. Chinese Journal of High Pressure Physics, 2011, 25(2): 147-152 . doi: 10.11858/gywlxb.2011.02.010
Citation: LIU Zai-Yang, WANG Duo-Jun, LI He-Ping, GUO Ying-Xing, YU Ying-Jie. A Preliminary Study on Conductivity of Serpentinite at High Pressure and High Temperature[J]. Chinese Journal of High Pressure Physics, 2011, 25(2): 147-152 . doi: 10.11858/gywlxb.2011.02.010

高温高压下蛇纹岩电导率的初步研究

doi: 10.11858/gywlxb.2011.02.010
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    通讯作者:

    王多君

A Preliminary Study on Conductivity of Serpentinite at High Pressure and High Temperature

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    Corresponding author: WANG Duo-Jun
  • 摘要: 在压力为2.0和4.0 GPa、温度为373~933 K的条件下,利用交流阻抗谱仪,在0.1~106 Hz的频率范围内测量了蛇纹岩的电导率。实验结果表明:蛇纹岩的复阻抗对频率有明显的依赖性,电导率受温度的影响较大,压力对电导率的影响相对较弱;当温度为690~761 K时,蛇纹岩发生脱水,致使电导率发生突变;脱水前,蛇纹岩的活化能约为0.6 eV,脱水后则高达2 eV。根据测得的电导率和活化能,分析了蛇纹岩脱水前、后的微观导电机制。分析认为,脱水前蛇纹岩的微观导电机制可能与内部二价铁和三价铁之间的电子移动有关,脱水后则可能是离子导电。

     

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出版历程
  • 收稿日期:  2010-05-13
  • 修回日期:  2010-09-14
  • 发布日期:  2011-04-15

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