岩土力学 ›› 2023, Vol. 44 ›› Issue (9): 2648-2656.doi: 10.16285/j.rsm.2022.1497

• 基础理论与实验研究 • 上一篇    下一篇

循环加载频率对饱和珊瑚砂液化特性的影响

杨铮涛1,秦悠1,吴琪1, 2,陈国兴1, 2   

  1. 1. 南京工业大学 岩土工程研究所,江苏 南京 210009;2. 江苏省土木工程防震技术研究中心,江苏 南京 210009
  • 收稿日期:2022-09-26 接受日期:2022-12-30 出版日期:2023-09-11 发布日期:2023-09-02
  • 通讯作者: 陈国兴,男,1963年生,博士,教授,主要从事土动力学及岩土地震工程研究。E-mail: gxc6307@163.com E-mail: yzt0628@163.com
  • 作者简介:杨铮涛,男,1998年生,硕士研究生,主要从事土动力学研究。
  • 基金资助:
    国家自然科学基金项目(No.52278503)

Influence of cyclic loading frequency on liquefaction behaviors of saturated coral sand

YANG Zheng-tao1, QIN You1, WU Qi1, 2, CHEN Guo-xing1, 2   

  1. 1. Institute of Geotechnical Engineering, Nanjing Tech University, Nanjing, Jiangsu 210009, China; 2. Civil Engineering and Earthquake Disaster Prevention Center of Jiangsu Province, Nanjing, Jiangsu 210009, China
  • Received:2022-09-26 Accepted:2022-12-30 Online:2023-09-11 Published:2023-09-02
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (52278503).

摘要: 人们对循环加载频率f对饱和石英砂液化特性的影响已进行大量的不排水循环试验研究,但循环加载频率f对饱和珊瑚砂液化特性的影响尚未引起重视。为探究f对饱和珊瑚砂液化特性的影响,针对中密、均等固结的饱和珊瑚砂试样,开展了f = 0.01~1.00 Hz、循环主应力路径90º跳转的系列不排水循环剪切试验。试验表明:孔压比ru和广义剪应变γg的增长速率随f增大而降低,到达初始液化所需的液化次数NL随f增大而增大;不同循环加载方式引起的广义剪应变幅值γga与峰值孔压比rumax存在事实上的唯一性关系,且γga可表示为以rumax为自变量的正切函数;f的增大会减弱试样的剪胀性。引入单元体循环应力比USR作为施加于试样的循环应力水平指标,USR−NL关系曲线随f的增大而移向右上侧,不同f的USR−NL关系曲线均服从相同形式的负幂函数。这意味着饱和珊瑚砂的抗液化强度随f的增大而增大。

关键词: 饱和珊瑚砂, 液化特性, 加载频率, 循环加载模式, 抗液化强度

Abstract: The influence of cyclic loading frequency f on the liquefaction behaviors of saturated quartz sands during undrained cyclic laboratory tests has been investigated extensively, but rare studies reported on the effect of f on the liquefaction behaviors of saturated coral sands. To better understand the effects of the f on the liquefaction behaviors of saturated coral sand, a series of undrained cyclic shear tests is performed on isotropically consolidated, medium dense saturated specimens subjected to the 90º jump of principal stress in the range of f = 0.01−1.0 Hz. For all loading patterns investigated, the growth rates of the excess pore water pressure ratio ru and the generalized shear strain γg decrease with the increase of f; the number of liquefaction NL required to cause the initial liquefaction increases with f; a unique tangent correlation function exists between the generalized shear strain amplitude γga and the peak excess pore pressure ratio rumax (rumax is independent variable); and an increase in f weakens the dilatancy of the specimen. By introducing a unit cyclic stress ratio USR as a proxy for cyclic stress level acting on the specimen during the cyclic testing, USR versus NL curves moves to the upper right with f, a unified form of power-law function of the correlation exists between USR and NL regardless of f. This indicates that liquefaction resistance of saturated coral sands increases with f.

Key words: saturated coral sand, liquefaction behavior, loading frequency, cyclic loading pattern, liquefaction resistance

中图分类号: TU411
[1] 秦悠, 龙慧, 吴琪, 庄海洋, 陈国兴. 复杂应力路径下饱和珊瑚砂孔压增长与刚度退化的阈值应变试验研究[J]. 岩土力学, 2025, 46(11): 3441-3450.
[2] THUY Do Van, TIEP Pham Duc, HIEU Nguyen Van, THANG Pham Cao. 循环三轴试验加载频率和压实度对重塑砂土液化行为的影响[J]. 岩土力学, 2024, 45(6): 1813-1823.
[3] 秦悠, 杜歆宇, 马维嘉, 吴琪, 陈国兴, . 不同循环应力路径下饱和珊瑚砂超静孔压增长的改进应力模型[J]. 岩土力学, 2023, 44(6): 1729-1738.
[4] 李水江, 姚嘉敏, 刘飞禹, 刘洪波, 侯娟, . 法向循环荷载下土石混合料-织物界面剪切特性研究[J]. 岩土力学, 2023, 44(11): 3082-3090.
[5] 刘抗, 陈国兴, 吴琪, 马维嘉, 秦悠, . 循环加载方向对饱和珊瑚砂液化特性的影响[J]. 岩土力学, 2021, 42(7): 1951-1960.
[6] 马维嘉, 陈国兴, 吴琪, . 复杂加载条件下珊瑚砂抗液化强度试验研究[J]. 岩土力学, 2020, 41(2): 535-542.
[7] 王丽艳, 巩文雪, 曹晓婷, 姜朋明, 王炳辉. 砾钢渣抗液化特性试验研究[J]. 岩土力学, 2019, 40(10): 3741-3750.
[8] 王 宇,常德龙,李建林,李春波,胡安龙. 复杂应力路径下饱水砂岩宏细观力学特性研究[J]. , 2016, 37(11): 3105-3114.
[9] 冷 建,叶冠林,王建华,杜守继. 上海软土动剪切模量衰减规律的试验研究[J]. , 2015, 36(S1): 387-391.
[10] 张晓超 ,黄润秋 ,许 模 ,裴向军 ,韩祥森 ,宋丽娟 ,张帆宇,. 石碑塬滑坡黄土液化特征及其影响因素研究[J]. , 2014, 35(3): 801-810.
[11] 严 栋,蒋关鲁,刘先峰,李华明. 京沪高速铁路饱和粉土液化特性试验研究[J]. , 2008, 29(12): 3337-3341.
[12] 程国勇 ,王建华 ,张献民 . 饱和砂土的剪切波速与其抗液化强度关系研究[J]. , 2007, 28(4): 689-693.
[13] 张 超,杨春和. 细粒含量对尾矿材料液化特性的影响[J]. , 2006, 27(7): 1133-1137.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!