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王宇, 夏厚磊, 茆苏徽, 闫亮. 泥岩卸荷损伤-水次序作用下的劣化规律研究[J]. 岩土工程学报, 2024, 46(2): 385-395. DOI: 10.11779/CJGE20221284
引用本文: 王宇, 夏厚磊, 茆苏徽, 闫亮. 泥岩卸荷损伤-水次序作用下的劣化规律研究[J]. 岩土工程学报, 2024, 46(2): 385-395. DOI: 10.11779/CJGE20221284
WANG Yu, XIA Houlei, MAO Suhui, YAN Liang. Deterioration rules of mudstone under unloading damage and water-rock interaction sequence[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(2): 385-395. DOI: 10.11779/CJGE20221284
Citation: WANG Yu, XIA Houlei, MAO Suhui, YAN Liang. Deterioration rules of mudstone under unloading damage and water-rock interaction sequence[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(2): 385-395. DOI: 10.11779/CJGE20221284

泥岩卸荷损伤-水次序作用下的劣化规律研究

Deterioration rules of mudstone under unloading damage and water-rock interaction sequence

  • 摘要: 工程开挖建设导致软岩形成卸荷损伤,其在水-岩作用下的劣化特征与卸荷损伤程度密切相关。以巴东地区红层泥岩为研究对象,设计进行了泥岩卸荷损伤模拟试验,随后对卸荷损伤泥岩试样进行水-岩作用试验,结果显示:卸荷损伤导致泥岩局部矿物颗粒形态破坏、微裂缝发育,在后续水-岩作用下颗粒间胶结程度持续弱化,孔隙、裂缝进一步扩展。宏细观参数随水-岩作用时间的增长,其中质量m呈现先上升后骤然下降再趋于稳定的趋势,纵波波速P呈现先减少后上升的趋势,体积应变 \varepsilon _\textv 呈现逐渐增大的趋势,分形维数K呈逐渐增长的趋势;且各参数的增长速率均随卸荷损伤程度D的增大呈幂函数增加,当D≥0.49时,各参数的增长速率急剧增大;确定以质量、纵波波速、体积应变和分形维数作为与水反应系统的变量,并运用非线性动力学理论建立了水-岩作用下的泥岩劣化模型,并验证了模型的合理性。研究结果表明所建模型能表征卸荷损伤泥岩在水-岩作用下的宏细观特征参数变化趋势提供一定理论参考。

     

    Abstract: Engineering excavation and construction lead to unloading damage of soft rock, and its degradation characteristics under water-rock interaction are closely related to the degree of unloading damage. Taking the red mudstone in Badong area as the research object, the simulation tests on the unloading damage of mudstone are designed and carried out, and then the water-rock interaction tests are carried out on the mudstone samples. The results show that the unloading damage leads to the destruction of the local mineral particle morphology of mudstone and the development of microcracks. Under the subsequent water-rock interaction, the degree of cementation between particles continues to weaken, and the pores and fractures further expand. The macro- and meso-parameters increase with the time of water-rock interaction, in which the mass (m) first rises, then drops suddenly and then tends to be stable, the longitudinal wave velocity (P) first decreases and then rises, and the volume strain \text(\varepsilon _\textv\text) and the fractal dimension (K) increase gradually. The growth rate of each parameter increases exponentially with the increase of unloading damage degree (D). When D ≥ 0.49, the growth rate of each parameter increases sharply. The quality, longitudinal wave velocity, volume strain and fractal dimension are determined as the variables of the reaction system with water, and the nonlinear dynamics theory is used to establish the degradation model for mudstone under water-rock interaction, and the rationality of the model is verified. The results indicate that the proposed model can provide a theoretical reference for characterizing the change trend of macro- and micro-characteristic parameters of unloading damaged mudstone under water-rock interaction.

     

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