岩土力学 ›› 2026, Vol. 47 ›› Issue (9): 3069-3078.doi: 10.16285/j.rsm.2025.1012CSTR: 32223.14.j.rsm.2025.1012

• 基础理论与实验研究 • 上一篇    下一篇

各向异性固结下饱和珊瑚砂的固−液相变特性

秦悠1, 2,龙慧1,马维嘉3,陈国兴4,庄海洋2   

  1. 1. 南华大学 土木工程学院,湖南 衡阳 421001;2. 华东交通大学 土木建筑学院,江西 南昌 330013; 3. 南京理工大学 安全科学与工程学院 (应急管理学院),江苏 南京 210094;4. 南京工业大学 岩土工程研究所,江苏 南京 211816
  • 收稿日期:2025-09-18 接受日期:2025-12-11 出版日期:2026-09-11 发布日期:2026-09-01
  • 通讯作者: 陈国兴,男,1963年生,博士,教授,主要从事土动力学与岩土地震工程方面的研究工作。E-mail: gxc6307@163.com
  • 作者简介:秦悠,男,1994年生,博士,教授,主要从事土动力学方面的研究。E-mail: qinyou94@163.com
  • 基金资助:
    国家自然科学基金(No.52278503);湖南省自然科学基金(No.2025JJ60378)。

Solid-liquid phase transition characteristics of saturated coral sand under anisotropic consolidation

QIN You1, 2, LONG Hui1, MA Wei-jia3, CHEN Guo-xing4, ZHUANG Hai-yang2   

  1. 1. School of Civil Engineering, University of South China, Hengyang, Hunan 421001, China; 2. School of Civil Engineering and Architecture, East China Jiaotong University, Nanchang, Jiangxi 330013, China; 3. School of Safe Science and Engineering (School of Emergency Management), Nanjing University of Science and Technology, Nanjing, Jiangsu 210094, China; 4. Institute of Geotechnical Engineering, Nanjing Tech. University, Nanjing, Jiangsu 211816, China
  • Received:2025-09-18 Accepted:2025-12-11 Online:2026-09-11 Published:2026-09-01
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (52278503) and the National Science Foundation of Hunan Province (2025JJ60378).

摘要:

各向异性固结显著影响饱和砂土的液化特性,为探究各向异性固结饱和珊瑚砂在循环荷载下的性质演化规律,开展了不同固结条件下循环应力主轴90º跳转的不排水循环剪切试验。试验结果表明,固结条件对饱和珊瑚砂应力−应变关系影响显著:应力分量与固结应力方向一致时滞回曲线单向累积发展,方向不一致时滞回曲线则交替往复。依据平均流动系数及平均流动系数梯度随循环次数的变化,可将珊瑚砂的性质演化分为三阶段,初始阶段为弹性固态(孔压及流动性低),随后孔压加速累积进入固−液过渡态(流动性显著增强),最终平均流动系数梯度突变后转入瞬时黏性液态。不同固结与循环加载模式下,平均流动系数梯度随孔压比均呈先增后减趋势,其反转点对应临界孔压比ruth 0.9,且该值与试验条件无关。鉴于各向异性固结下珊瑚砂孔压与应变的不协调,此临界孔压比可作为复杂静−动应力作用下饱和砂土的液化触发标准。

关键词: 固?液相变, 各向异性固结, 临界孔压比, 循环加载模式, 液化判别标准

Abstract:

Anisotropic consolidation significantly affects the liquefaction behavior of saturated sand. To investigate the evolution characteristics of anisotropically consolidated saturated coral sand under cyclic loading, undrained cyclic shear tests were conducted with a 90º jump rotation of the principal stresses under varying consolidation conditions. The test results indicate that consolidation conditions significantly affect the stress-strain response of saturated coral sand. The hysteresis curve evolves with unidirectional accumulation when the stress component is collinear with the consolidation stress, whereas alternating cyclic hysteresis responses are observed under misaligned stress orientations. Based on variations in the average flow coefficient and its gradient with the number of cycles, the mechanical evolution of coral sand can be classified into three phases. The initial phase corresponds to an elastic solid state, characterized by low excess pore water pressure and negligible mobility. This is followed by a phase of accelerated pore water pressure accumulation, leading to a solid-liquid transition with increased particle mobility. Finally, a sharp change in the average flow coefficient gradient signifies the onset of a transient viscous-liquid state. Under varying consolidation and cyclic-loading conditions, gradient shows an initial increase followed by a decrease with increasing excess pore water pressure ratio with a turning point at a critical excess pore water pressure ratio ruth of approximately 0.9, which remains invariant across test conditions. Given the observed discrepancy between pore water pressure development and strain response in anisotropically consolidated coral sand, this ruth may serve as a reliable triggering criterion for liquefaction in saturated sandy soils under complex static and dynamic loading.

Key words: solid-liquid phase transition, anisotropic consolidation, critical excess pore water pressure ratio, cyclic loading pattern, liquefaction criteria

中图分类号: TU411
[1] 杨铮涛, 秦悠, 吴琪, 陈国兴, . 循环加载频率对饱和珊瑚砂液化特性的影响[J]. 岩土力学, 2023, 44(9): 2648-2656.
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