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Impurity Effects on the Mechanical Properties and Permeability Characteristics of Salt Rock

Author

Listed:
  • Qiangxing Zhang

    (College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China)

  • Jianfeng Liu

    (College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China)

  • Lu Wang

    (College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China)

  • Min Luo

    (College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China)

  • Hejuan Liu

    (Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, State Key Experiments in Geotechnical Mechanics and Engineering, Wuhan 430071, China)

  • Huining Xu

    (College of Water Resource and Hydropower, Sichuan University, Chengdu 610065, China)

  • Hang Zou

    (Sichuan Water Resources and Hydroelectric Investigation and Design Institute of the Ministry, Chengdu 610072, China)

Abstract

Impure salt rock strata are extensively distributed in China, giving them great significance in the study of the physical properties of impure salt rock for the construction of underground gas storage in salt mines. To investigate the confining pressure and impurity effects on the mechanical properties and gas permeability characteristics of salt rock, permeability tests under hydrostatic confining pressure and conventional triaxial compression (CTC), on salt rock samples with different impurity contents, were carried out. The results demonstrate that the confining pressure effects cause an increase in triaxial compression strength, but a decrease in permeability. However, impurity enhances the bearing capacity and permeability of the salt rock; both rock strength and permeability increase with an increase in impurity content. Moreover, the broken salt rock specimens were analyzed after the CTC test using Computed Tomography (CT) equipment. To understand the relationships between pore volume and permeability, considering the confining pressure and impurity effects, the cracks were divided into four groups according to different crack diameter ranges: ~0.05 mm, 0.05–1 mm, 1–10 mm and ~10 mm. The CT analysis results show that while the pore volume of smaller cracks shows an “increasing–decreasing” trend by increasing confining pressure, the pore volume of large cracks gradually decreases, indicating that the rock permeability is highly related to macro-cracks. However, impurity has more complicated implications on rock permeability and cracks, and needs further investigation.

Suggested Citation

  • Qiangxing Zhang & Jianfeng Liu & Lu Wang & Min Luo & Hejuan Liu & Huining Xu & Hang Zou, 2020. "Impurity Effects on the Mechanical Properties and Permeability Characteristics of Salt Rock," Energies, MDPI, vol. 13(6), pages 1-19, March.
  • Handle: RePEc:gam:jeners:v:13:y:2020:i:6:p:1366-:d:332854
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    Citations

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    Cited by:

    1. Lu Wang & Jianfeng Liu & Yilin Liao & Shuyu Yang & An He & Huining Xu, 2023. "A Study on the Permeability and Damage Characteristics of Limestone under Stress–Seepage Coupling Conditions," Energies, MDPI, vol. 16(19), pages 1-15, September.
    2. Deng Xu & Jianfeng Liu & Zhide Wu & Lu Wang & Hejuan Liu & Fukun Xiao & Yin Zeng & Cheng Lyu, 2020. "Experimental Investigation on Permeability Evolution of Dolomite Caprock under Triaxial Compression," Energies, MDPI, vol. 13(24), pages 1-12, December.

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