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Deterioration law of intermittent jointed sandstone mechanical properties under water-rock interaction

Wybrane pełne teksty z tego czasopisma
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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
In water-rich mines, water conservancy, and hydropower projects, the rock mass is immersed in water for a long time, which leads to changes in its mechanical properties and affects the safety and stability of the engineering rock mass. Based on the long-term immersion of rock mass with intermittent joints by water, uniaxial compression tests were carried out on prefabricated intermittent jointed sandstone with five inclinations (0°, 30°, 45°, 60°, 90°) and three connectivity ratios (0.25, 0.50, 0.75) under different immersion times to study sandstone with intermittent joints’ mechanical response and deterioration mechanism. The research shows that: (1) With the increase of the joint inclination, the compressive strength and elastic modulus of the sandstone with intermittent joints first decreased and then increased, showing a U-shaped distribution. The compressive strength and elasticity of the sample with an inclination of 60° reach the minimum value; at the initial stage of immersion, the deterioration effect of the sample is more significant, and the deterioration effect decreases gradually with the increase in immersion time; in the initial stage of water immersion, the deterioration effect of the sample is more significant, and with the increase of the immersion time, the deterioration effect gradually weakens. (2) Immersion time and joint inclination have a great influence on the included angle, number, and mode of failure cracks. With the increase in immersion time, the plastic characteristics of the sample increase obviously, showing the characteristics of loose and weak; with the increase in joint inclination, the failure mode of the sample gradually changes from tension failure to tension shear failure, and tension failure. The influence degree of joints on failure is weak-induction-control-induction. (3) Under the water–rock action, the cement between mineral particles of the sample is gradually dissolved, the cementation of mineral particles is weakened, and the mineral particles develop into layered and fake structure, which gradually evolves from dense structure to porous loose structure. (4) The deterioration mechanism of the mechanical properties of the sandstone with intermittent joints under the water–rock action was analyzed from the perspectives of physics, chemistry, and mechanics. The deterioration of the mechanical properties of the sample is a process of gradual accumulation of damage.
Czasopismo
Rocznik
Strony
1923--1935
Opis fizyczny
Bibliogr. 22 poz.
Twórcy
autor
  • Mining Research Institute, Inner Mongolia University of Science and Technology, Baotou 014010, Inner Mongolia, China
  • College of Energy and Mining Engineering, Shandong University of Science and Technology, Qingdao 266590, China
autor
  • Mining Research Institute, Inner Mongolia University of Science and Technology, Baotou 014010, Inner Mongolia, China
autor
  • Mining Research Institute, Inner Mongolia University of Science and Technology, Baotou 014010, Inner Mongolia, China
autor
  • School of Mining Engineering, Heilongjiang University of Science and Technology, Harbin 150022, Heilongjiang, China
Bibliografia
  • 1. Apollaro C, Marini L, Critelli T et al (2013) The standard thermodynamic properties of vermiculites and prediction of their occurrence during water-rock interaction. Appl Geochem 35:264–278
  • 2. Burshtein LS (1969) Effect of moisture on the strength and deformability of sandstone. Sov Min Sci 5(5):573–576
  • 3. Chen ML, Qi SC, Lv PF et al (2021) Hydraulic response and stability of a reservoir slope with landslide potential under the combined effect of rainfall and water level fluctuation. Environ Earth Sci 80(1):1–19
  • 4. Deng HF, Zhang YC, Li JL et al (2017) Effect of moisture content on splitting tensile strength of layered sandstone. Chin J Rock Mech Eng 36(11):2778–2787
  • 5. Deng HF, Qi Y, Li JL et al (2021) Degradation mechanism of intermittent jointed sandstone under water-rock interaction. Chin J Geotech Eng 43(4):634–643
  • 6. Dou ZH, Zhao ZH, Gao TY et al (2021) Evolution law of water-rock interaction on the shear behavior of granite fractures. J Tsinghua Univ 61(8):792–798
  • 7. Hale PA, Shakoor A (2003) A laboratory investigation of the effects of cyclic heating and cooling, wetting and drying, and freezing and thawing on the compressive strength of selected sandstones. Environ Eng Geosci 9(2):117–130
  • 8. Huang YS, Deng JH, Zhong SH et al (2014) Experimental study on mechanical property of argillaceous dolomite with different moisture content. Chin J Undergr Space Eng 10(2):276–284
  • 9. Huang ZG, Zuo QJ, Wu L et al (2020) Nonlinear softening mechanism of argillaceous slate under water–rock interaction. Rock Soil Mech 41(9):2931–2942
  • 10. Jin C, Wang F, Shi C (2017) Experimental study on mechanical properties of soaked shale. J Yangtze River Sci Res Inst 34(9):122–126
  • 11. Li P, Liu J, Zhu JB et al (2008) Research on effects of water content on shear creep behavior of weak structural plane of sandstone. Rock Soil Mech 29(7):1865–1871
  • 12. Liu Q, Sun YJ, Li J et al (2020a) Experimental study on seepage characteristics of jurassic weakly cemented sandstone under water–rock interaction. Geofluids 2020(3):1–12
  • 13. Liu XR, Jing R, Miao LL et al (2020b) Reconstruction models and typical case analysis of the fluctuation belt of reservoir bank slopes in Wushan. Chin J Rock Mech Eng 39(7):1321–1332
  • 14. Liu YL, Wang CY, Li XH (2022) Coupling study of acoustic emission and infrared radiation in sandstone under water–rock interaction. J Yangtze River Sci Res Inst 39(1):127–133
  • 15. Lu J, Xu QY, Ning ZX (2019) Analysis of structural characteristics of the coal with different water immersion time. J Henan Polytech Univ 38(5):28–36
  • 16. Shao MS, Li L, Li ZX (2010) Elastic wave velocity and mechanical properties of sandstone under different water contents at longyou grottoes. Chin J Rock Mech Eng 29(S2):3514–3518
  • 17. Wang Y, Liu J, Ma XF et al (2020) Immersion effect of polyurethane-reinforced sand based on NMR. Chin J Geotech Eng 42(12):2342–2349
  • 18. Xia D, Yang TH, Xu T et al (2015) Experimental study on AE properties during the damage process of water-saturated rock specimens based on time effect. J China Coal Soc 40(S2):337–345
  • 19. Yang ZP, Lai YL, Liu SL et al (2019) Dynamic stability and failure mode of slopes with overlying weak rock mass under frequent micro-seismic actions. Chin J Geotech Eng 41(12):2297–2306
  • 20. Yin XT, Ge XR, Li CG et al (2010)Influences of loading rates on mechanical behaviors of rock materials. Chin J Rock Mech Eng 29(S1):2610–2615
  • 21. Zhao LC (2022) Experimental study on mechanical property softening of water saturated sandstone. Chin J Undergr Space Eng 18(1):154–162
  • 22. Zhao YK, Liu HD, Qiao L (2008) Test study of soil strength with different soaked periods of embankment of Yellow River. Chin J Rock Mech Eng 27(S1):3047–3051
Uwagi
PL
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-74bc0d09-771c-4085-9339-5385f5f7452c
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