ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    干湿循环作用下人工结构性黄土的变形与结构演变机理研究

    Deformation and Structural Evolution Mechanism of Artificial Structured Loess under Wet-Dry Cycles

    • 摘要: 针对中国黄土地区因季节性降雨导致的干湿循环环境,以及由此引发的黄土地基沉降问题,探究干湿循环作用下黄土微观结构损伤与宏观变形演化机理,为黄土地区工程防灾提供理论依据。采用组分可控、结构均一的人工制备结构性黄土模拟天然黄土,通过侧限压缩试验、单线法湿陷试验等宏观力学测试手段,结合扫描电镜(SEM)、颗粒分析及X射线衍射(XRD)等细微观分析方法,系统研究了干湿循环次数(0~9次)对黄土压缩变形、湿陷系数及微观结构特征的影响。试验结果表明:干湿循环对黄土微观结构造成了不可逆损伤。在宏观层面,压缩变形随循环次数增加呈显著正相关;而湿陷系数随循环次数呈现“先增大后减小”的非单调演化规律。结构性参数表现出“初期骤降、后期趋稳”的非线性衰减特征,前3次循环为结构损伤的主要发生期,后5~9次循环的衰减速率显著放缓,仅为初期速率的1/4左右。在微观层面,胶结物质溶解流失导致土体微观结构由“强胶结–大团粒”支撑体系逐渐向“弱胶结–散体单粒”接触体系演变。干湿循环诱导的胶结物质流失与微观结构重排是导致黄土宏观力学性能衰退的本质原因。在循环初期,胶结破坏导致的结构崩解占主导地位;在循环后期,随着孔隙压密和结构重组,抵抗变形的能力有所提升。鉴于此,工程实践中应高度重视地基暴露初期的防水保护,以防范结构损伤累积引发的突发性沉降。

       

      Abstract: The seasonal rainfall leads to a frequent wet-dry cycle environment across the China Loess Plateau. This environment often aggravates foundation settlement and collapsible deformation in loess subgrades. This study investigates the coupling mechanism of microstructural damage and macro-deformation evolution under wet-dry cycles. The findings provide a theoretical basis for engineering disaster prevention in loess regions. Artificially structured loess with controllable composition and uniform structure was prepared to simulate natural loess. This experimental approach facilitated the systematic study of the effects of wet-dry cycles (0~9 cycles) on loess. Macro-mechanical behaviors were tested using confined compression and single-line collapsibility methods. Microstructural characteristics were analyzed via Scanning Electron Microscopy (SEM), particle analysis, and X-ray Diffraction (XRD). The test results indicate that wet-dry cycling causes irreversible damage to the loess microstructure. Macroscopically, compressive deformation shows a significant positive correlation with the number of cycles. Conversely, the collapsibility coefficient follows a non-monotonic evolutionary pattern, first increasing and then decreasing. The structural parameters exhibit a non-linear decay characterized by an "initial sharp drop followed by stabilization". The first three cycles constitute the primary structural damage phase; the decay rate slows down significantly during cycles 5 to 9, reaching only about one-quarter of the initial rate. Microscopically, the dissolution and loss of cementing agents cause the soil structure to evolve. The support system transforms from a "strong cementation-large aggregate" structure to a "weak cementation-loose particle" contact system. This loss of cementing agents and the resulting microstructural rearrangement are the essential causes of macroscopic mechanical degradation. In the initial cycles, structural disintegration driven by cementation failure dominates. This significantly enhances collapsibility sensitivity. In later cycles, pore compaction and structural reorganization increase the soil's resistance to further deformation. Therefore, engineering practices must prioritize waterproofing during the early exposure period of the foundation to prevent sudden settlements caused by accumulated structural damage.

       

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