Characterization of Pore Electrical Conductivity in Porous Media by Weakly Conductive and Nonconductive Pores

• Published in: Surveys in geophysics Vol. 44; no. 3; pp. 877 - 923
• Main Authors: Zhu, Linqi, Wu, Shiguo, Zhang, Chaomo, Misra, Siddharth, Zhou, Xueqing, Cai, Jianchao
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer Netherlands 01.06.2023; Springer Nature B.V
• Subjects: Astronomy; Earth and Environmental Science; Earth Sciences; Electrical conductivity; Electrical properties; Electrical resistivity; Electrical transmission; Evaluation; Geophysics/Geodesy; Hydrates; Methods; Observations and Techniques; Pores; Porous media; Rocks; Sediment; Sedimentary rocks; Sediments; Shale; Porous media; Nonconductive pores; Formation factor; Weakly conductive pores; Truncated cone pore
• ISSN: 0169-3298; 1573-0956
• DOI: 10.1007/s10712-022-09761-w

The formation factor, which reflects the electrical conductivity of porous sediments and rocks, is widely used in a range of research fields. Consequently, given the discovery of numerous porous reservoir rocks and sediments exhibiting complex conductivity characteristics, methods to quantitatively predict the formation factor have been actively pursued by many scholars. Nevertheless, the agreement between the theoretically calculated and measured formation factors remains unsatisfactory, partially because the distribution characteristics of the entire pore space affect the final formation factor. In this study, a new method for characterizing the formation factor is proposed that considers the impacts of different complex pore structures on the conductivity of pores at different positions in the pore space. With this method, the electrical transmission through a rock can be accurately and quantitatively estimated based on the conductivity and shape of pores, the tortuous conductivity, and the classification of the pore space into conductive, weakly conductive, and nonconductive pores. By evaluating 24 datasets encompassing 7 types of rocks and sediments, including marine hydrate-bearing sediments and shale, the proposed model achieves remarkable agreement with the experimental data. These excellent confirmation results are attributed to the ubiquitous presence of weakly conductive and nonconductive pores in almost all rocks and sediments. Through further research based on this paper, an increasing number of adaptation models and a comprehensive set of evaluation methods can be developed.