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考虑冻融循环的季冻区高等级公路路基填土本构模型研究
引用本文:崔宏环,刘建坤,张立群,田亚护. 考虑冻融循环的季冻区高等级公路路基填土本构模型研究[J]. 岩土力学, 2015, 36(8): 2228-2236. DOI: 10.16285/j.rsm.2015.08.014
作者姓名:崔宏环  刘建坤  张立群  田亚护
作者单位:1.北京交通大学 土木建筑工程学院,北京 100044;2.河北建筑工程学院 土木工程学院,河北 张家口 075000; 3.青海省交通科学研究院 多年冻土区公路建设与养护技术交通行业重点实验室青海研究观测基地,青海 西宁 810000
基金项目:国家重点基础研究发展计划(973计划):青藏高原重大冻土工程的基础研究(No. 2012CB026104);国家自然科学基金:严寒高速铁路级配碎石水热稳定性与变形控制(No. 51378057)。
摘    要:在季冻区高等级公路路基场地取土,制成重塑土试件进行冻融循环试验。而后对经历不同冻融循环次数的土体进行三轴固结排水(CD)剪切试验,测得应力、应变数据。在大量试验数据的基础上,遵循岩土本构变化规律,以岩土弹塑性力学为理论基础,在p-q空间,以椭圆方程拟合体变屈服面,以抛物线方程拟合剪切屈服面,采用塑性关联流动,得到考虑冻融循环条件下融土的弹塑性本构方程。通过编程计算后,对比计算与试验结果,证明该双屈服面本构模型能够较为准确地预估冻融循环土体的应力-应变关系,该本构模型对季冻区路基土体长期稳定性分析和工程预测具有重要参考意义。

关 键 词:本构模型  冻融循环  硬化规律  剪切应变  体积应变  屈服函数  
收稿时间:2014-12-18

A constitutive model of subgrade in a seasonally frozen area with considering freeze-thaw cycles
CUI Hong-huan,LIU Jian-kun,ZHANG Li-qun,TIAN Ya-hu. A constitutive model of subgrade in a seasonally frozen area with considering freeze-thaw cycles[J]. Rock and Soil Mechanics, 2015, 36(8): 2228-2236. DOI: 10.16285/j.rsm.2015.08.014
Authors:CUI Hong-huan  LIU Jian-kun  ZHANG Li-qun  TIAN Ya-hu
Affiliation:1. School of Civil Engineering, Beijing Jiaotong University, Beijing 100044, China; 2. School of Civil Engineering, Hebei Institute of Architecture and Civil Engineering, Zhangjiakou, Hebei, 075000, China; 3. Qinghai Research and Observation Base, Key Laboratory of Highway Construction & Maintenance Technology in Permafrost Region, Qinghai Research Institute of Transportation, Xining, Qinghai, 810000
Abstract:The freeze-thaw cycle tests were conducted on the remoulded soil samples taken from a highway subgrade in a seasonally frozen area. The triaxial compression tests under the consolidated-drained condition were carried out on the remoulded samples subjected to freeze-thaw cycle, and stress-strain data were obtained. Based on the experimental results and the theory of elasto- plasticity, an elliptic equation is proposed to fit the yield surface in the p-q coordinate system, while a parabolic equation is proposed to fit shear yield surface, from which an elastic-plastic constitutive equation was developed following an associated flow rule with considering freeze-thaw cycles. By comparing the theoretical calculation with the experimental data, it is shown that the proposed double-yield surface constitutive model can accurately predict the frozen soil stress-strain relationship. The model provides a theoretical basis for long-term stability analysis and engineering prediction of subgrade soil in seasonally frozen areas.
Keywords:constitutive model  freeze-thaw cycle  hardening rules  shear strain  volumetric strain  yield function  
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