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Mechanical Properties and Strength Evolution Model of Sandstone Subjected to Freeze–Thaw Weathering Process: Considering the Confining Pressure Effect

Author

Listed:
  • Xin Xiong

    (School of Resources and Safety Engineering, Central South University, Changsha 410083, China
    Research Center for Mining Engineering and Technology in Cold Regions, Central South University, Changsha 410083, China)

  • Feng Gao

    (School of Resources and Safety Engineering, Central South University, Changsha 410083, China
    Research Center for Mining Engineering and Technology in Cold Regions, Central South University, Changsha 410083, China)

  • Keping Zhou

    (School of Resources and Safety Engineering, Central South University, Changsha 410083, China
    Research Center for Mining Engineering and Technology in Cold Regions, Central South University, Changsha 410083, China)

  • Chun Yang

    (School of Resources and Safety Engineering, Central South University, Changsha 410083, China
    Research Center for Mining Engineering and Technology in Cold Regions, Central South University, Changsha 410083, China)

  • Jielin Li

    (School of Resources and Safety Engineering, Central South University, Changsha 410083, China
    Research Center for Mining Engineering and Technology in Cold Regions, Central South University, Changsha 410083, China)

Abstract

Freeze-and-thaw (F&T) weathering cycles induced by day–night and seasonal temperature changes cause a large number of rock mass engineering disasters in cold areas. Investigating the impact of F&T weathering process on the strength and deformation characteristics of frozen–thawed rocks is therefore of critical scientific importance for evaluating the stability and optimizing the design of rock mass engineering in these areas. In this research, the evolution characteristics of F&T damage were analyzed based on T 2 spectrum distribution curves of sandstone specimens before and after F&T weathering cycles. The coupling impact of the quantity of F&T weathering cycles and confining pressure on pre-peak and post-peak deformation behaviors of sandstone specimens were analyzed in detail. By introducing the confining pressure increase factor (CPIF), the impact of confining pressure on the triaxial compressive strength (TCS) of sandstone specimens after undergoing different quantities of F&T weathering cycles was further investigated. A novel strength evolution model was proposed that could effectively describe the coupling impact of the quantity of F&T weathering cycles and confining pressure on TCS of rocks after undergoing the F&T weathering process. The proposed strength evolution model was cross-verified with experimental data from the published literature and all correlation coefficients were above 0.95, which proved that the strength evolution model proposed in this paper was reasonable; in addition, this model has strong applicability.

Suggested Citation

  • Xin Xiong & Feng Gao & Keping Zhou & Chun Yang & Jielin Li, 2022. "Mechanical Properties and Strength Evolution Model of Sandstone Subjected to Freeze–Thaw Weathering Process: Considering the Confining Pressure Effect," Mathematics, MDPI, vol. 10(20), pages 1-19, October.
  • Handle: RePEc:gam:jmathe:v:10:y:2022:i:20:p:3841-:d:944974
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    References listed on IDEAS

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    1. Hailiang Jia & Wei Xiang & Michael Krautblatter, 2015. "Quantifying Rock Fatigue and Decreasing Compressive and Tensile Strength after Repeated Freeze‐Thaw Cycles," Permafrost and Periglacial Processes, John Wiley & Sons, vol. 26(4), pages 368-377, October.
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    Cited by:

    1. Linqi Huang & Shaofeng Wang & Xin Cai & Zhengyang Song, 2022. "Mathematical Problems in Rock Mechanics and Rock Engineering," Mathematics, MDPI, vol. 11(1), pages 1-3, December.

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