院报 ›› 2016, Vol. 33 ›› Issue (6): 70-74.DOI: 10.11988/ckyyb.20150166

• 岩土工程 • 上一篇    下一篇

考虑固结路径影响的花岗岩残积土 不排水剪切试验研究

刘攀a,b,周小文a,b,何勇彬a,b,赵仕威a,b   

  1. 华南理工大学 a.土木与交通学院,b.亚热带建筑科学国家重点实验室, 广州 510640
  • 收稿日期:2015-03-09 出版日期:2016-05-25 发布日期:2016-06-12
  • 作者简介:刘 攀(1991-),男,江西吉安人,博士研究生,主要从事土的基本性质及岩土工程问题等方面的研究,(电话) 13427570305(电子信箱)panliu2013@126.com。    通讯作者:周小文(1965-),男,江西吉安人,教授,博士,主要从事土的基本性质及岩土工程问题等方面的研究,(电话) 020-87114373(电子信箱)xwzhou@scut.edu.cn。
  • 基金资助:
    国家自然科学基金项目(51109083);华南理工大学亚热带建筑科学国家重点实验室自主课题 (2013ZC04)

Experimental Study on Undrained Shear Behavior of Granite Residual Soil under Various Consolidation Stress Paths

LIU Pan1,2, ZHOU Xiao-wen1,2, HE Yong-bin1,2, ZHAO Shi-wei1,2   

  1. 1.School of Civil Engineering and Transportation, South China University of Technology, Guangzhou 510640, China;
    2.State Key Laboratory of Subtropical Building Science,South China University of Technology, Guangzhou 510640, China
  • Received:2015-03-09 Online:2016-05-25 Published:2016-06-12

摘要: 针对常规的等向固结剪切试验不能反映实际工程中复杂应力路径对土体力学特性的影响,采用GDS应力路径三轴仪,对华南地区广泛分布的花岗岩残积土进行了不同固结条件下的不排水剪切试验,探讨不同初始平均有效主应力p′c与初始应力比ηc对其不排水特性的影响。结果表明在初始应力比相同的情况下,初始平均有效主应力越大,花岗岩残积土的不排水剪切强度越大,破坏时的孔压也越大;在初始平均有效主应力相同的情况下,初始应力比越大,花岗岩残积土的不排水剪切强度越大,而破坏时的孔压越小。然而,e-p′-q三维空间中的临界状态线是唯一的,不受初始平均有效主应力和初始应力比影响。

关键词: 花岗岩残积土, 三轴试验, 应力路径, 临界状态线, 三维空间

Abstract: In engineering practice, conventional triaxial tests under isotropically consolidated conditions cannot reflect the effects of various stress paths on the mechanical behavior of granite residual soil which is widely distributed in south China. To investigate the influence of the initial mean effective stress p′c and the initial stress ratio ηc on the undrained shear behavior of reconstituted granite residual soil, a series of triaxial tests under different consolidated conditions were conducted on the GDS triaxial apparatus. The test results revealed that both the initial mean effective stress and the initial stress ratio have effects on the undrained shear behavior. It was found that, for the granite residual soil in this study, under the same initial stress ratio, there would be an increase of undrained shear strength and excess pore water pressure with a higher initial mean effective stress. Besides, under the same initial mean effective stress, the higher the initial stress ratio is, the higher the undrained shear strength and the lower the excess pore water pressure would be. However, a unique critical state line can be postulated in e-p′-q space, regardless of the various initial mean effective stress and initial stress ratio.

Key words: granite residual soil, triaxial test, stress path, critical state line, 3-D space

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