...
首页> 外文期刊>Mineralogical Magazine >The electrical conductivity of dry polycrystalline olivine compacts at high temperatures and pressures
【24h】

The electrical conductivity of dry polycrystalline olivine compacts at high temperatures and pressures

机译:干多晶橄榄石压块在高温和高压下的电导率

获取原文
获取原文并翻译 | 示例
           

摘要

The electrical conductivity of dry polycrystalline olivine compacts (hot-pressed and sintered pellets) was measured at pressures of 1.0-4.0 GPa, at temperatures of 1073-1423 K, and at different oxygen fugacities via the use of a YJ-3000t multi-anvil press. Oxygen fugacity was controlled successfully by means of five solid buffers: Fe_3O_4-Fe_2O_3, Ni-NiO, Fe-Fe_3O_4, Fe-FeO and Mo-MoO_2. Within the selected frequency range of 10~2-10~6 Hz, the experimental results indicate that the grain interior conduction mechanism is characterized by a semi-circular curve on an impedance diagram. As a function of increasing pressure, the electrical conductivity of polycrystalline olivine compacts decreases, whereas the activation enthalpy and the temperature-independent pre-exponential factors increase slightly. The activation energy and activation volume of polycrystalline olivine compacts were determined to be 141.02±2.53 kJ/mol and 0.25±0.05 cm~3/mol, respectively. At a pressure of 4.0 GPa, electrical conductivity was observed to increase as a function of increasing oxygen fugacity, and the relationship between electrical conductivity and oxygen fugacity can be described as log_(10) (σ) = (2.47±0.085) + (0.096±0.023)×log_(10) f_(O_2)+ (-0.55±0.011)/T, which presents the exponential factor q (~0.096). Our observations demonstrate that the primary conduction mechanism for polycrystalline olivine compacts is a small polaron.
机译:通过使用YJ-3000t多砧,在1.0-4.0 GPa的压力,1073-1423 K的温度以及不同的氧气逸度下测量干燥的多晶橄榄石压块(热压和烧结的球团)的电导率按。通过五个固体缓冲液成功地控制了氧气逸度:Fe_3O_4-Fe_2O_3,Ni-NiO,Fe-Fe_3O_4,Fe-FeO和Mo-MoO_2。实验结果表明,在选定的10〜2-10〜6 Hz频率范围内,晶粒内部传导机制的特征在于阻抗图上的半圆形曲线。作为增加压力的函数,多晶橄榄石压块的电导率降低,而活化焓和与温度无关的预指数因子则略有增加。确定多晶橄榄石压块的活化能和活化体积分别为141.02±2.53 kJ / mol和0.25±0.05 cm〜3 / mol。在4.0 GPa的压力下,观察到电导率随氧气逸度的增加而增加,并且电导率与氧气逸度之间的关系可以描述为log_(10)(σ)=(2.47±0.085)+(0.096) ±0.023)×log_(10)f_(O_2)+(-0.55±0.011)/ T,表示指数因子q(〜0.096)。我们的观察表明,多晶橄榄石压块的主要传导机制是小的极化子。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号