岩土力学 ›› 2026, Vol. 47 ›› Issue (6): 2083-2094.doi: 10.16285/j.rsm.2025.0474CSTR: 32223.14.j.rsm.2025.0474

• 基础理论与实验研究 • 上一篇    下一篇

珊瑚碎屑混淤泥土压缩−渗透特性及其影响因素研究

严蕾1, 2,张先伟1,朱华亮1, 2,苟乐宇1,王港3,刘新宇1   

  1. 1. 中国科学院武汉岩土力学研究所 岩土力学与工程安全全国重点实验室,湖北 武汉 430071;2. 中国科学院大学,北京 100049; 3. 香港科技大学 土木与环境工程系,香港 999077
  • 收稿日期:2025-05-12 接受日期:2025-09-16 出版日期:2026-06-11 发布日期:2026-06-06
  • 通讯作者: 张先伟,男,1982年生,博士,研究员,主要从事特殊土土力学基础研究及工程应用。E-mail: xwzhang@whrsm.ac.cn
  • 作者简介:严蕾,女,2002年生,博士研究生,主要从事特殊土土力学等方面的研究。E-mail: yanlei231@mails.ucas.ac.cn
  • 基金资助:
    国家自然科学基金(No.42372313,No.42572367)

Compression-permeability characteristics of coral gravel soil and their influencing factors

YAN Lei1, 2, ZHANG Xian-wei1, ZHU Hua-liang1, 2, GOU Le-yu1, WANG Gang3, LIU Xin-yu1   

  1. 1. State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, Hubei 430071, China; 2. University of Chinese Academy of Sciences, Beijing 100049, China; 3. Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Hong Kong 999077, China
  • Received:2025-05-12 Accepted:2025-09-16 Online:2026-06-11 Published:2026-06-06
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42372313, 42572367).

摘要:

珊瑚碎屑混淤泥土是一种由珊瑚碎屑颗粒与黏土矿物基质组成的生物成因混合土,广泛分布于热带沿海与岛礁地区。该类土通常具有高孔隙率、不规则颗粒形态和较大的破碎潜势,其工程特性与陆源粗粒土显著不同,传统土力学理论难以准确描述其变形和渗流行为。为深入研究其压缩过程中的变形与渗透特性及其影响因素,对不同珊瑚碎屑含量的珊瑚碎屑混淤泥土开展一维等应变速率固结试验,调查压缩性、渗透性与固结特性;引入骨架孔隙比与颗粒破碎率等参数,量化评价压缩过程中的颗粒破碎及其对变形和渗透特性的影响;通过扫描电镜观察试样压缩前后的微观结构变化,最终提出珊瑚碎屑混淤泥土的压缩−渗透特性微观机制。结果表明:珊瑚碎屑含量与有效应力共同控制珊瑚碎屑混淤泥土的压缩−渗透行为;在高有效应力和高珊瑚碎屑含量(体积含量大于30%)条件下,颗粒破碎会显著提高土体压缩指数,导致渗透系数和固结系数大幅降低;珊瑚碎屑混淤泥土的压缩行为实质上是土体微观结构从“骨架型”向“致密填充型”的演化过程;骨架孔隙比e2能够有效表征这一规律,其中e2 = 5可作为不同微观结构特征及其对压缩−渗透特性影响的划分阈值。本研究可为珊瑚岛礁工程建设提供力学参数和技术指导。

关键词: 珊瑚碎屑混淤泥土, 压缩特性, 渗透特性, 骨架孔隙比, 颗粒破碎

Abstract:

Coral gravel soil (CGS) is a biogenic composite material composed of coral gravels (CG) and clay mineral matrix, commonly found in tropical coastal and reef island regions. This type of soil typically exhibits high porosity, irregular particle shapes, and a high breakage potential, making its engineering behavior significantly different from that of terrigenous coarse-grained soils. Traditional soil mechanics theories often fail to accurately describe the deformation and seepage behavior of CGS. To better understand its compression-induced deformation and permeability characteristics, one-dimensional constant rate of strain consolidation tests were conducted on CGS specimens with varying CG content. The compressibility, permeability, and consolidation characteristics were investigated. Parameters such as skeletal void ratio and particle breakage index were introduced to quantify particle breakage during compression and evaluate its effects on deformation and permeability. Microstructural changes before and after compression were observed using scanning electron microscopy, enabling the development of a micro-mechanistic model of CGS compression–permeability behavior. The results indicate that both CG content and effective stress jointly govern the compression–permeability response of CGS. Under high effective stress and high CG content (greater than 30% by volume), significant particle breakage occurs, leading to a notable increase in compressibility and a significant reduction in both permeability and the coefficient of consolidation. The compression behavior of CGS essentially represents a microstructural evolution from a “skeletal framework” to “densely packed” configuration. The skeletal void ratio e2 effectively captures this transformation, with a critical value of e2 = 5 proposed as a threshold to distinguish different microstructural characteristics and their impact on compression–permeability behavior. This study provides mechanical parameters and technical insights valuable for engineering applications on coral reef islands.

Key words: coral gravel soil, compression, permeability, skeleton void ratio, particle breakage

中图分类号: TU449
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