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高温高压下叶蜡石脱水电导率实验
引用本文:代立东,李和平,刘丛强,苏根利,崔桐娣,单双明,杨昌君,刘庆友.高温高压下叶蜡石脱水电导率实验[J].地质科技情报,2005,24(3):35-37.
作者姓名:代立东  李和平  刘丛强  苏根利  崔桐娣  单双明  杨昌君  刘庆友
作者单位:1. 中国科学院地球化学研究所,贵阳,550002;中国科学院研究生院,北京,100039
2. 中国科学院地球化学研究所,贵阳,550002
3. 贵州大学,贵阳,550004
基金项目:国家自然科学基金,中国科学院知识创新工程项目
摘    要:在压力为1.0~4.0 GPa、温度为873~1 223 K下采用Sarltron-1260阻抗/增益-相位阻抗谱分析仪测定了叶蜡石的电导率.实验结果表明,电导率与温度间的关系符合Arrenhius关系式;叶蜡石的脱水引起电导率的突然变化,使电导率急剧上升;脱水前,电导率随着压力增大而减小,其导电机制为电子导电;脱水后,电导率随着压力增大而增大,其导电机制为离子导电.

关 键 词:叶蜡石  高温高压  电导率  脱水作用
文章编号:1000-7849(2005)03-0035-03
收稿时间:2004-07-05
修稿时间:2004年7月5日

Dehydration Experiment of Electrical Conductivity of Pyrophyllite at HTP
DAI Li-dong,LI He-ping,LIU Cong-qiang,SU Gen-li,CUI Tong-di,SHAN Shuang-ming,YANG Chang-jun,LIU Qing-you.Dehydration Experiment of Electrical Conductivity of Pyrophyllite at HTP[J].Geological Science and Technology Information,2005,24(3):35-37.
Authors:DAI Li-dong  LI He-ping  LIU Cong-qiang  SU Gen-li  CUI Tong-di  SHAN Shuang-ming  YANG Chang-jun  LIU Qing-you
Abstract:Electrical conductivities of pyrophyllite were measured by virtue of Sarltron-1260 frequency and phase impedance spectroscopic analyzer in situation of 1.0-4.0 GPa and 873-1 223 K. The experimental results indicate that the relationships between electrical conductivity and temperature fit Arrenhius equation connection. The pyrophyllite dehydration may lead to abrupt increase; Before dehydration, the electric conduction is electron when the electrical conductivity decreases with the pressure increase. While the electric conduction is ion when the electrical conductivity decreases with the pressure increase after the dehydration.
Keywords:pyrophyllite  high temperature and high pressure  electrical conductivity  dehydration effect
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