土工基础 ›› 2026, Vol. 40 ›› Issue (2): 360-365.

• 测试技术 • 上一篇    下一篇

尤溪饱和花岗岩残积土剪切特性的试验研究

段文杰,冯兆圆,杨雪强,林希养   

  1. (广东工业大学土木与交通工程学院,广州 510000)
  • 收稿日期:2024-03-08 修回日期:2024-03-31 出版日期:2026-04-30 发布日期:2026-04-23
  • 通讯作者: 杨雪强(1966-),男,博士,教授,研究方向为土体本构关系及边坡稳定等。
  • 作者简介:段文杰(2000-),男,硕士生,研究方向为边坡稳定。
  • 基金资助:
    国家自然科学基金资助项目(51978177)

Study on Shear Characteristics of Saturated Weathered Granite Residual Soil in Youxi Area

DUAN Wenjie, FENG Zhaoyuan, YANG Xueqiang, LIN Xiyang   

  • Received:2024-03-08 Revised:2024-03-31 Online:2026-04-30 Published:2026-04-23

摘要: 对福建尤溪地区的花岗岩残积土,制作出干密度为1.73,1.64,1.56 g·cm-3的重塑土样,分别开展围压为100,200,300,400 kPa的3组12个常规三轴固结不排水剪切试验。试验表明:①不同干密度条件下的偏应力-轴向应变曲线均呈现应变硬化趋势,在干密度不变的情况下,偏应力随着围压和干密度的增大而增大,围压越大偏应力上升曲线越陡,其增加趋势随着后期应变增大而逐步减缓。②孔压随着轴向应变的增大先呈非线性增长,到达峰值后出现略微缓慢下降趋势或者保持稳定;在相同围压下,干密度越大,孔隙压力峰值越小。③在干密度相同的条件下,围压增加,应力比q/p′随之减小,且减小的幅度随围压的增大而逐渐下降,低围压下的最终应力比相较于高围压下的最终应力比稍高一些;在围压保持不变条件下,应力比q/p′随着干密度的增加而增加;在轴向应力达到30%左右,应力比基本达到稳定状态。④土体的抗剪强度与干密度密切相关,CU下的内摩擦角和黏聚力随干密度的增加而上升,有效内摩擦角和有效黏聚力也随干密度的增加而增加;在干密度相同的条件下,有效粘聚力略大于CU下的黏聚力,有效内摩擦角略大于CU下的内摩擦角。


关键词: 花岗岩残积土, 常规三轴试验, 固结不排水试验, 抗剪强度

Abstract: For weathered granite residual soil obtained from Youxi county of Fujian Province, the remodeled soil samples with three dry densities of 1.73, 1.64 and 1.56 g/cm3 were prepared separately. 12 conventional triaxial consolidated undrained shear tests were carried out in the 3 dry density groups with confining pressures of 100, 200, 300 and 400kPa, respectively. The results show that: 1) the deviational stressaxial strain curves under different dry density conditions show a strain hardening trend. When the dry density remains unchanged, the deviational stresses increase with the increasing of confining pressure and dry density. The greater the confining pressure is, the steeper the deviational stress rising presents as axial strain developing, and the deviational stress increasing trend gradually approaches stable as the axial strain further increasing. 2) Pore pressure increases non-linearly with the increase of axial strain at firstly, and then decreases slightly or remains stable after reaching the peak value; Under the same confining pressure level with the higher the dry density being, soil sample presents the smaller peak pore pressure. 3) Under the condition of the same dry density, as the confining pressure increases the stress ratio q/p,of soil sample decreases, and the decreasing range gradually converges with the increasing of confining pressure. The final stress ratio under low confining pressure is slightly higher than that under high confining pressure level. The stress ratio q/p, increases with the increasing of dry density under constant confining pressure condition. When the axial strain reaches about 30%, the stress ratio basically reaches a stable state. 4) The shear strength of soil is closely related to dry density. The internal friction angle and cohesion of soil under CU condition increase with the increasing of dry density, and the effective internal friction angle and effective cohesion also increase with the increasing of dry density. Under the condition of the same dry density, the effective cohesion is slightly greater than the cohesion under CU status, and the effective internal friction angle is slightly greater than the internal friction under CU condition.

Key words: Weathered Granite Residual Soil, Conventional Triaxial Test, Consolidated Undrained Test, Shearing Strength

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