The role of incremental stress ratio in mechanical behavior and particle breakage of calcareous sand

被引:1
作者
He, Shao-Heng [2 ]
Yin, Zhen-Yu [2 ,4 ]
Ding, Zhi [1 ]
Sun, Yifei [3 ]
机构
[1] Hangzhou City Univ, Key Lab Safe Construct & Intelligent Maintenance U, Hangzhou 310015, Peoples R China
[2] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Hung Hom, Hong Kong 999077, Peoples R China
[3] Hohai Univ, Key Lab Minist Educ Geomech & Embankment Engn, Nanjing 210024, Peoples R China
[4] Hong Kong Polytech Univ, Res Ctr Resources Engn Carbon Neutral RCRE, Hung Hom, Kowloon, Hong Kong 999077, Peoples R China
关键词
Stress path; Triaxial test; Strength; Dilatancy; Calcareous sand; CRITICAL-STATE; SHEAR; INSTABILITY; STRENGTH; STRAIN; LINE;
D O I
10.1007/s11440-024-02400-1
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Calcareous sand has been used in reclamation for constructing artificial islands. It suffers different stress paths with varying constant incremental stress ratios (Delta q/Delta p'), exhibiting diverse mechanical characteristics with grain crushing. However, previous experimental studies mainly focused on conventional triaxial stress path (Delta q/Delta p' = 3). This study aims to investigate more unconventional shear stress paths, such as constant ratios of Delta q/Delta p' (=-0.5,-1.5,2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$ = -0.5, \, -1.5, \, 2$$\end{document}, where negative ratio corresponding to p'-decreasing, and vice versa) and constant p' (Delta q/Delta p' = infinite) on both anisotropically and isotropically consolidated calcareous sand. For comparison, the conventional triaxial tests under constant confining pressure (Delta q/Delta p' = 3) are also performed. For all tested samples, the grain size distribution is measured to quantify the particle breakage after loading. It is found that shear stress path plays a significant role in the mechanical of calcareous sand. Despite varying degrees of particle breakage caused by different stress paths, the relationship between the peak state friction angle with the maximum dilatancy angle and state parameter is unique. Irrespective of the consolidation/shear stress path, the peak friction angle consistently exhibits a monotonic increase with the maximum dilatancy angle, while exponentially decreases with the increasing of state parameter. Additionally, particle breakage causes a downward curvature of the critical state line (CSL) in the e-lnp' plane. However, irrespective of the stress path, the CSL remains linear when plotted in e-(p'/pa)xi and the e-ln(p' + pr) plane. The findings are helpful for understanding the mechanical behavior and modeling of crushable calcareous sand under complex loads.
引用
收藏
页码:167 / 183
页数:17
相关论文
共 54 条
  • [1] Sand instability under constant shear drained stress path
    Alipour, M. J.
    Lashkari, A.
    [J]. INTERNATIONAL JOURNAL OF SOLIDS AND STRUCTURES, 2018, 150 : 66 - 82
  • [2] American Society for Testing and Materials (ASTM), 2015, STANDARD TEST METHOD
  • [3] [Anonymous], 2013, ASTM C642,
  • [4] [Anonymous], 2011, Standard Test Methods for Chemical Analysis of Hydraulic Cement, DOI 10.1520/D2435_D2435M-11R20
  • [5] [Anonymous], 2014, STANDARD TEST METHOD
  • [6] THE INFLUENCE OF PARTICLE BREAKAGE ON THE LOCATION OF THE CRITICAL STATE LINE OF SANDS
    Bandini, V.
    Coop, M. R.
    [J]. SOILS AND FOUNDATIONS, 2011, 51 (04) : 591 - 600
  • [7] A STATE PARAMETER FOR SANDS
    BEEN, K
    JEFFERIES, MG
    [J]. GEOTECHNIQUE, 1985, 35 (02): : 99 - 112
  • [8] THE STRENGTH AND DILATANCY OF SANDS
    BOLTON, MD
    [J]. GEOTECHNIQUE, 1986, 36 (01): : 65 - 78
  • [9] Permanent deformation characteristics of saturated sand under cyclic loading
    Cai, Yuanqiang
    Sun, Qi
    Guo, Lin
    Juang, C. Hsein
    Wang, Jun
    [J]. CANADIAN GEOTECHNICAL JOURNAL, 2015, 52 (06) : 795 - 807
  • [10] THE MECHANICS OF UNCEMENTED CARBONATE SANDS
    COOP, MR
    [J]. GEOTECHNIQUE, 1990, 40 (04): : 607 - 626