[S-CG62] [EE] 変動帯ダイナミクス

[SCG62-P35] Pressure dependence of electrical conductivity in brine-saturated Berea sandstone and its pore structure

*南部 美菜子¹、渡辺 了² (1.富山大学大学院理工学教育部、2.富山大学大学院理工学研究部)

キーワード：electrical conductivity, sandstone, pore structure

Electrical conductivity in brine-sturated Berea sandstone (porosity~20%) was measured under confining pressures of up to 100 MPa. The pore-fluid pressure was kept at the atmospheric pressure (0.1 MPa). Electrical conductivity decreased by 22% as the confining pressure was increased to 40 MPa. Volumetric strain of a dry rock sample was separately measured under confining pressures. The volume change was 0.7% as the confining pressure was increased to 50 MPa. The change in porosity should be only 1%. The observed relatively large decrease in conductivity shows that the connectivity of pores in the porous Berea sandstone was significantly reduced by a small decrease in porosity. In order to understand the nature of the conduction path, the pore structure in Berea sandstone was observed with X-ray CT conducted at Tokyo Metropolitan Industrial Technology Research Institute. 3D images of pores were constructed by processing X-ray CT images to examine the connectivity of pores.