中国安全科学学报 ›› 2026, Vol. 36 ›› Issue (5): 207-214.doi: 10.16265/j.cnki.issn1003-3033.2026.05.1794

• 安全技术与工程 • 上一篇    下一篇

太阳辐照与干湿循环耦合作用下压实黄土裂隙演化机制

田新宇1,2(), 梅源1,2, 孙天慧1,2, 余雅楠1,2, 张雨1,2   

  1. 1 西安建筑科技大学 土木工程学院, 陕西 西安 710055
    2 陕西省岩土与地下空间工程重点实验室, 陕西 西安 710055
  • 收稿日期:2026-01-12 修回日期:2026-03-21 出版日期:2026-05-28
  • 作者简介:

    田新宇 (1994—),女,陕西西安人,博士研究生,主要研究方向为土木工程施工安全控制理论与工程应用。E-mail:

    梅源 教授。

  • 基金资助:
    国家自然科学基金资助(52178302)

Mechanism of crack evolution in compacted loess under coupled solar irradiance and wetting-drying cycles

Tian Xinyu1,2(), Mei Yuan1,2, Sun Tianhui1,2, Yu Yanan1,2, Zhang Yu1,2   

  1. 1 College of Civil Engineering, Xi'an University of Architecture and Technology, Xi'an Shaanxi 710055, China
    2 Shaanxi Key Laboratory of Geotechnical and Underground Space Engineering, Xi'an Shaanxi 710055, China
  • Received:2026-01-12 Revised:2026-03-21 Published:2026-05-28

摘要:

为分析太阳辐照与干湿循环对压实黄土裂隙演化的影响及其作用机制,采用氙灯模拟太阳辐照,开展不同辐照度、干密度及干湿循环条件下的压实黄土室内试验,自制图像获取装置定时采集试样表面裂隙图像,利用颗粒与裂隙分析系统(PCAS)提取裂隙形态参数,结合扫描电镜(SEM)图像定量分析微观孔隙结构,从宏-微观尺度系统分析裂隙演化机制。结果表明:辐照度提高使裂隙起裂时间提前,裂隙率、主裂隙长度及分形维数整体增大;干密度1.5~1.7 g/cm3范围内,干密度提高可有效降低裂隙率及连通性,抑制裂隙扩展;干湿循环作用下,孔隙率总体增加,孔隙圆度降低,分形维数先增大后波动,与宏观裂隙演化显著关联;太阳辐照加速土体表层水分蒸发,强化水分迁移与体积变形不均匀性,促进压实黄土由孔隙结构调整向宏观裂隙扩展演化。

关键词: 压实黄土, 太阳辐照, 干湿循环, 裂隙演化, 微观结构

Abstract:

To investigate the effects of solar irradiation and wetting-drying cycles on the crack evolution of compacted loess and clarify the underlying mechanisms, laboratory tests were conducted using a xenon lamp to simulate solar irradiation under varying irradiance levels, dry densities, and wetting-drying cycles. Surface crack images were periodically captured using a self-developed acquisition system. Crack morphological parameters were extracted using the Particle and Crack Analysis System (PCAS), and micro-pore structures were quantitatively analyzed based on scanning electron microscopy (SEM) images, enabling a systematic macro-micro analysis of crack evolution characteristics. Results indicate that increasing irradiance accelerates crack initiation and increases crack ratio, main crack length, and overall fractal dimension. Within the dry density range of 1.5-1.7 g/cm3, higher dry density effectively reduces crack ratio and connectivity, thereby inhibiting crack propagation. Under wetting-drying cycles, porosity generally increases, pore circularity decreases, and fractal dimension shows an initial increase followed by fluctuations, corresponding well with macroscopic crack evolution. Solar irradiation enhances surface evaporation, intensifies moisture migration and deformation heterogeneity, and promotes the transition from pore structure adjustment to macroscopic crack propagation.

Key words: compacted loess, solar radiation, wetting-drying cycles, crack evolution, microstructure

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