岩土力学 ›› 2024, Vol. 45 ›› Issue (1): 226-234.doi: 10.16285/j.rsm.2023.0088

• 基础理论与实验研究 • 上一篇    下一篇

加载与干湿循环作用下土石混合料蠕变特性试验

孙晨峰1, 2,王步雪岩1, 2,钱建固1, 2,王家超1, 2,张甲峰3   

  1. 1. 同济大学 地下建筑与工程系,上海 200092;2. 同济大学 岩土及地下工程教育部重点实验室,上海 200092; 3. 上海民航新时代机场设计研究院有限公司,上海 200335
  • 收稿日期:2023-01-30 接受日期:2023-04-19 出版日期:2024-01-10 发布日期:2024-01-17
  • 通讯作者: 钱建固,男,1972年生,博士,教授,博士生导师,主要从事岩土力学与本构理论、软土基础工程和交通岩土工程方面的研究。E-mail: qianjiangu@tongji.edu E-mail:sunchenfeng@tongji.edu.cn
  • 作者简介:孙晨峰,男,1998年生,硕士研究生,主要从事高填方工后沉降方面的研究。
  • 基金资助:
    国家自然科学基金资助项目(No.51238009);中央高校基本科研业务费专项资金(No.22120190220)

Creep characteristics test of soil-rock mixture subjected to loading and dry-wet cycles

SUN Chen-feng1, 2, WANG Bu-xue-yan1, 2, QIAN Jian-gu1, 2, WANG Jia-chao1, 2, ZHANG Jia-feng3   

  1. 1. Department of Geotechnical Engineering, Tongji University, Shanghai 200092, China; 2. Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, China; 3. Shanghai CAAC New Era Airport Design & Research Institute Co., Ltd., Shanghai 200335, China
  • Received:2023-01-30 Accepted:2023-04-19 Online:2024-01-10 Published:2024-01-17
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51238009) and the Fundamental Research Funds for the Central Universities (22120190220).

摘要: 土石混合料在干湿循环作用下具有显著的蠕变性,其对高填方工程蠕变变形的影响不可忽略。为了研究了不同干密度及荷载水平对土石混合料湿化蠕变变形的影响,开展了9组土石混合料干湿循环作用下的压缩蠕变试验。结果表明,土石混合料的湿化蠕变变形随荷载水平的提高而增大,随干密度的提高而显著减小,但随着干密度进一步提高,湿化蠕变变形的减小幅度则明显弱化。土石混合料在干湿循环作用下的湿化蠕变变形与干湿循环次数对数之间较好地满足线性发展规律,初次湿化应变及湿化蠕变速率均同荷载水平及干密度之间符合幂函数特征,在此基础上提出了考虑不同干密度及荷载水平的土石混合料干湿循环蠕变经验模型。

关键词: 填筑土, 土石混合料, 干湿循环, 蠕变, 干密度

Abstract: The study focused on investigating the influence of dry density and load level on the wetting creep deformation of soil-rock mixture. A total of 9 groups of compression creep tests were conducted on the soil-rock mixture under a dry-wet cycle. The results revealed that the wetting creep deformation of the soil-rock mixture increased with higher load levels and decreased significantly with increasing dry density. However, as the dry density further increased, the decrease in wetting creep deformation became less pronounced. The relationship between wetting creep deformation and the logarithm of the number of dry-wet cycles followed a linear development pattern for the soil-rock mixture under the dry-wet cycle conditions. The initial wetting strain and wetting creep rate were found to have power function distribution relationships with the load level and dry density. Based on these findings, an empirical model for the dry-wet cycle creep behavior of the soil-rock mixture was proposed. This model takes into consideration different dry densities and load levels, providing a framework for predicting and understanding the creep deformation of the soil-rock mixture under such conditions.

Key words: filling soil, soil-rock mixture, dry-wet cycles, creep, dry density

中图分类号: TU411
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