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Volume 60 Issue 3
Jun.  2025
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Journal of Southwest Jiaotong University  > 2025  >  60(3): 608-617.
HOU Chao, JIN Xiaoguang, HE Jie, FANG Zhiyuan. Freeze-Thaw Damage Characteristics of Anhydrite Rock Pore Structures Based on Nuclear Magnetic Resonance Technology[J]. Journal of Southwest Jiaotong University, 2025, 60(3): 608-617. doi: 10.3969/j.issn.0258-2724.20230314
Citation: HOU Chao, JIN Xiaoguang, HE Jie, FANG Zhiyuan. Freeze-Thaw Damage Characteristics of Anhydrite Rock Pore Structures Based on Nuclear Magnetic Resonance Technology[J]. Journal of Southwest Jiaotong University, 2025, 60(3): 608-617. doi: 10.3969/j.issn.0258-2724.20230314
shu

Freeze-Thaw Damage Characteristics of Anhydrite Rock Pore Structures Based on Nuclear Magnetic Resonance Technology

doi: 10.3969/j.issn.0258-2724.20230314
  • 1.

    School of Civil Engineering and Architecture, Henan University of Science and Technology, Luoyang 471000, China

  • 2.

    School of Civil Engineering, Chongqing University, Chongqing 400044, China

  • 3.

    Key Laboratory of New Technology for Construction of Cities in Mountain Area, Chongqing 400044 China

  • 4.

    State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, China

  • Received Date: 30 Jun 2023
  • Rev Recd Date: 20 Sep 2023
    • Available Online: 21 Nov 2024
  • Publish Date: 07 Oct 2023
    Abstract

  • In order to study the damage characteristics of meso and micro pore structures of gypsum rock subjected to freeze-thaw cycles in cold regions, anhydrite rock was taken as the research object, and the porosity, pore size, and pore throat distribution characteristics of anhydrite rock were obtained based on nuclear magnetic resonance (NMR) experiments. According to fractal theory, the calculation formulas of the fractal dimension of pore size and pore throat of rock were derived, and the influence of freeze-thaw cycles on the fractal dimension of pore structures of anhydrite rock was discussed. The relationship among different pore structures, fractal dimensions of pores, and porosity was established, and the pore structure types that had a greater impact on porosity were revealed. The results show that the pore size of anhydrite rock under freeze-thaw cycles presents a “three-peak” distribution. With the increase in freeze-thaw cycles, the micropore (r≤0.100 μm), PT-Ⅰ (r∈(0, 0.100] μm) of pore throat, fractal dimension of pore (DP), and fractal dimension of pore throat (DPT) decrease exponentially. While, the mesopores (r∈(0.100, 1.000) μm), macropores (r≥1.000 μm), PT-Ⅱ(r∈(0.100, 4.000] μm) of pore throats, and porosity increase exponentially. It can be concluded that larger pores, as well as smaller pore throats and fractal dimension of pore throats, have a greater influence on the porosity of anhydrite rock.

     

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