Liu Xiaoxuan, Wang Xingxiao, Wei Xiaobing, Luo Mingxing, Chen Xinlian, Zhong Li
School of Civil Engineering and Architecture, Wuhan University of Technology, Wuhan, 430070, Hubei, China.
Beijing Xinyi Resources Technology Co., Ltd, Zhengzhou, 450000, Henan, China.
Sci Rep. 2024 Mar 21;14(1):6853. doi: 10.1038/s41598-024-57505-0.
The particle breakage effect and compression characteristics of calcareous sand are related to the water content in the sand material. However, the effects of water content on the particle breakage and compression characteristics of calcareous sand have rarely been investigated. In this work, 50 sets of confined compression tests were conducted on calcareous sand specimens, and the compression characteristics and particle breakage effects of two single-particle-size groups (particle size ranges of 1-0.5 mm and 0.5-0.25 mm) of calcareous sand were investigated under five different water contents. The test results showed that with the increase in the water content, the final compression deformation of calcareous sand was positively correlated with the water content. The final compression deformation decreased when the water content reached a certain value. The water content corresponding to the peak final compression deformation was related to the gradation of the calcareous sand; the specific values were 10% and 15% for particle size ranges of 1-0.5 mm and 0.5-0.25 mm, respectively. With the increase in the water content, the slope of the loading curve of calcareous sand appeared to increase and then decrease, reaching maximum when the water content was 10%. Moreover, the slope of the loading curve was close to twice that of the loading curve of dry sand, whereas the slope of the unloading curve changed little. Under the same water content, the initial gradation had no effect on the compression and unloading characteristics of the specimens beyond a vertical pressure of 1 MPa. The effects of the variation in the water content on the particle breakage of calcareous sand were mainly reflected in the softening effect of water on the specimen particles, which reduced the Mohr strength of the particles.
钙质砂的颗粒破碎效应和压缩特性与砂材料中的含水量有关。然而,含水量对钙质砂颗粒破碎和压缩特性的影响鲜有研究。在本研究中,对钙质砂试样进行了50组侧限压缩试验,研究了两种单一粒径组(粒径范围为1 - 0.5mm和0.5 - 0.25mm)的钙质砂在五种不同含水量下的压缩特性和颗粒破碎效应。试验结果表明,随着含水量的增加,钙质砂的最终压缩变形与含水量呈正相关。当含水量达到一定值时,最终压缩变形减小。对应最终压缩变形峰值的含水量与钙质砂的级配有关;粒径范围为1 - 0.5mm和0.5 - 0.25mm时的具体值分别为10%和15%。随着含水量的增加,钙质砂加载曲线的斜率先增大后减小,在含水量为10%时达到最大值。此外,加载曲线的斜率接近干砂加载曲线斜率的两倍,而卸载曲线的斜率变化不大。在相同含水量下,当初始级配超过1MPa垂直压力时,对试样的压缩和卸载特性没有影响。含水量变化对钙质砂颗粒破碎的影响主要体现在水对试样颗粒的软化作用,这降低了颗粒的莫尔强度。