高压灭菌器
材料科学
多孔性
饱和(图论)
电阻率和电导率
阿累尼乌斯方程
热导率
复合材料
地温梯度
电导率
多孔介质
矿物学
地质学
冶金
活化能
电气工程
化学
组合数学
有机化学
物理化学
工程类
数学
地球物理学
作者
Shuangming Shan,Chaoyi Xiao,Heping Li,Li Xu,Sen Lin,Shengbin Li
摘要
This study presents a method for measuring the electrical conductivity of porous rock materials in situ under a shallow Earth crust environment simulated according to temperature, confining pressure, and liquid water saturation in a high-temperature autoclave. The sample was first encased within a poly tetra fluoroethylene container with two Pt wires leading out and was then placed into the high-temperature autoclave. The lead wires were connected to an external measurement system after passing through the autoclave sealing plug. The electrical conductivity of sandstone was measured under different temperatures (30, 60, 90, 120, 150 °C), liquid water saturation levels (36%, 51%, 100%), and 2 MPa by using this method. The electrical conductivity of the sandstone samples increased with increasing temperature and also increased as the level of water saturation increased. All the results agreed well with the Arrhenius relationship, Archie’s law, and previous experimental study. This method can be used to measure other kinds of porous water-containing rocks, and the results can be applied in geothermal/oil research.
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