Ma Ji, Zhang Zizhao, Lai Runsen, Guo Zekun, Shi Guangming, Zhang Yanyang, Huang Junpeng
School of Geology and Mining Engineering, Xinjiang University, Urumqi, 830017, China.
Guangdong Provincial Institute of Mineral Resources Exploration, Guangzhou, 510000, China.
Sci Rep. 2025 Jul 15;15(1):25575. doi: 10.1038/s41598-025-08991-3.
The mechanical properties of the loess in the Ili region of China deteriorate significantly when it is subjected to the dry-wet cycles. Attributed to the critical role played by the mica content for the mechanical deterioration of Ili loess, a series of laboratory tests, including the X-ray diffraction (XRD) tests, the triaxial compression tests, the scanning electron microscopy (SEM), and other methods, were carried out to investigate the macroscopic and microscopic properties of Ili loess under different dry-wet cycles (i.e., 0, 1, 3, 5, 10, 15, 20 cycles) and different mica contents (1.8, 3.8, 5.7, and 7.7%). The main research outcomes are as follows: (1) the cohesion of the loess generally exhibits a fluctuating downward trend under different dry-wet cycles, while the internal friction angle of which shows a slight overall upward trend; (2) the content of small particles for the loess with small mica content (1.8%) gradually increases with the increased number of dry-wet cycles, resulting in a loose structure. It is after 20 dry-wet cycles that the clump-like particles with large size was generated. With the increased content of the mica, a large amount of the mica minerals were embedded and interspersed between skeletal particles of the loess in the flaky form; (3) the pore fractal dimension is highly correlated with the cohesion, while both the equivalent particle diameter and equivalent pore diameter are more closely related to the internal friction angle, for which the pore area ratio shows the least correlation with other parameters; and (4) the mica with small values of content will be embedded and interspersed between skeletal particles of the loess, which restricts the relative slippage of the loess mass. However, the increased mica content leads to the oriented arrangements structures in the loess mass, resulting in the occurrence of sliding surfaces associated with the decreased strength.
中国伊犁地区的黄土在经历干湿循环后,其力学性能会显著恶化。由于云母含量对伊犁黄土力学性能恶化起着关键作用,因此开展了一系列实验室试验,包括X射线衍射(XRD)试验、三轴压缩试验、扫描电子显微镜(SEM)试验等方法,以研究不同干湿循环次数(即0、1、3、5、10、15、20次循环)和不同云母含量(1.8%、3.8%、5.7%和7.7%)下伊犁黄土的宏观和微观特性。主要研究成果如下:(1)在不同干湿循环次数下,黄土的黏聚力总体呈波动下降趋势,而内摩擦角总体呈轻微上升趋势;(2)云母含量较低(1.8%)的黄土中,小颗粒含量随干湿循环次数增加而逐渐增多,导致结构松散。在20次干湿循环后产生了大尺寸的团聚状颗粒。随着云母含量增加,大量云母矿物呈片状嵌入并穿插在黄土骨架颗粒之间;(3)孔隙分形维数与黏聚力高度相关,等效粒径和等效孔径与内摩擦角关系更为密切,而孔隙面积比与其他参数的相关性最小;(4)含量较小的云母会嵌入并穿插在黄土骨架颗粒之间,限制了黄土体的相对滑动。然而,云母含量增加会导致黄土体中出现定向排列结构,从而产生与强度降低相关的滑动面。