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Experimental Study on Physicomechanical Properties of Deep Sandstone by Coupling of Dry-Wet Cycles and Acidic Environment

机译:干湿循环和酸性环境耦合深层砂岩物理机械性能的实验研究

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Underground engineering, especially deep geotechnical engineering, is often affected alternately by groundwater infiltration and ventilation drying during construction and use. In addition, acid rain, mineral dissolution, acid deposition, and other factors make groundwater acidic. This caused the underground structure to erode and has also threatened its safety and durability. In this study, both the physical and mechanical properties under acid dry-wet (A-D-W) cycles were investigated. Deep sandstone was treated repeatedly under acid cycling, and its physical parameters were measured. Uniaxial compressive strength tests and microtests were carried out. Finally, using a combination of scanning electron microscopy (SEM) and backscatter electron images (BSE), the microstructural changes of sandstone under the combined action of an acidic environment and a dry-wet cycle were described. The test results show that the mass, P-wave velocity, peak stress, and elastic modulus of sandstone after the A-D-W cycles decreased by 0.43%, 7.87%, 70.20%, and 88.10%, respectively. With the increase in the number of cycles, the loss of these indicators increased. However, the peak strain increased with an average increase of 55.8%. In addition, 10 cycles are the critical point for physical and mechanical indicators of the A-D-W cycles. After 10 cycles, the changes of various indicators increase rapidly. Microscopic analysis shows that the reasons of this phenomenon were that the specimen was corroded by the sulfuric acid solution, which resulted in the development of pores and cracks and the decline of physical and mechanical properties. Conversely, the development of pores was hindered by sediment, which slowed down the decline rate of the physical and mechanical indexes of specimens, but this phenomenon disappeared with the increase of A-D-W cycles. Based on the analysis of the experimental phenomena, the constitutive model of uniaxial compression based on Weibull damage variable has been established in this article, and the model has the best effect in acid solution with less cycle times or pH value of solution greater than 6.
机译:地下工程,尤其是深层岩土工程,往往在施工和使用过程中通过地下水渗透和通风干燥时交替地受到影响。此外,酸雨,矿物溶解,酸沉积和其他因素使地下水酸性。这导致地下结构侵蚀并威胁其安全性和耐用性。在该研究中,研究了酸性干湿(A-D-W)循环下的物理和机械性能。在酸循环下重复处理深砂岩,测量其物理参数。进行单轴抗压强度试验和微热。最后,使用扫描电子显微镜(SEM)和反向散射电子图像(BSE)的组合,描述了酸性环境的组合作用下砂岩的微观结构变化和干湿循环。试验结果表明,A-D-W循环后砂岩的质量,P波速度,峰值应力和弹性模量分别降低0.43%,7.87%,70.20%和88.10%。随着循环次数的增加,这些指标的损失增加了。然而,峰值应变增加,平均增加了55.8%。此外,10个周期是A-D-W循环的物理和机械指示器的临界点。 10次​​循环后,各种指标的变化迅速增加。微观分析表明,这种现象的原因是样品被硫酸溶液腐蚀,导致孔隙和裂缝的发育和物理和机械性能的下降。相反,沉积物阻碍了孔隙的发育,减缓了标本的物理和机械指标的下降率,但这种现象随着A-D-W循环的增加而消失。基于对实验现象的分析,本文已经建立了基于Weibull损伤变量的单轴压缩的本构模型,该模型对酸性溶液具有最佳效果,循环时间较少或溶液的pH值大于6。

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