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何浩松, 滕继东, 张升, 盛岱超. 基于冻胀量与时间平方根之比确定冻胀分级的探讨[J]. 岩土工程学报, 2023, 45(12): 2519-2528. DOI: 10.11779/CJGE20221102
引用本文: 何浩松, 滕继东, 张升, 盛岱超. 基于冻胀量与时间平方根之比确定冻胀分级的探讨[J]. 岩土工程学报, 2023, 45(12): 2519-2528. DOI: 10.11779/CJGE20221102
HE Haosong, TENG Jidong, ZHANG Sheng, SHENG Daichao. Determining frost heave classification by using ratio of frost heave to square root of time[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(12): 2519-2528. DOI: 10.11779/CJGE20221102
Citation: HE Haosong, TENG Jidong, ZHANG Sheng, SHENG Daichao. Determining frost heave classification by using ratio of frost heave to square root of time[J]. Chinese Journal of Geotechnical Engineering, 2023, 45(12): 2519-2528. DOI: 10.11779/CJGE20221102

基于冻胀量与时间平方根之比确定冻胀分级的探讨

Determining frost heave classification by using ratio of frost heave to square root of time

  • 摘要: 冻胀分级指标是寒区基础工程设计和冻胀防治的关键指标,目前既有方法多认为冻胀分级是材料的一种基本属性,常使用经验或半经验的分级指标表示土体冻胀能力,但缺乏理论支撑。而冻胀试验复杂、耗时长,不利于指标测试。为提出合理简单的冻胀分级指标,首先从冻胀机制角度出发,建立非饱和土冻胀解析模型,并对模型进行了验证。基于该模型提出了以冻胀量和时间平方根之比作为确定冻胀分级的新指标R (mm/h0.5),并以大量冻胀试验结果为依据,提出当R<0.21时,对应低冻胀等级,当0.21≤R≤1.18时,对应中等冻胀等级,而当R>1.18时,对应强冻胀等级。此外利用统计概率分析了冻胀过程中各指标数值的概率密度分布,发现新指标R在冻胀过程的集中程度和稳定性是最高的。新指标R具有理论基础,同时耦合了土性参数和冻结环境因素,突破了既有冻胀分级指标的局限性,完善了现有冻胀分级体系,为寒区工程设计和冻胀防治提供理论依据。

     

    Abstract: The frost heave classification is the critical index for the design of foundation engineering in cold regions. At present, it is considered as a basic property of materials. Many criteria belong to empirical or semi-empirical methods and lack theoretical support. The frost heave tests are tedious and long time-consuming, and are not easily operated. To propose a rational and simple frost heave classification index, from the frost heave mechanism, an analytical model for unsaturated frozen soil is established and validated. Then a new frost heave classification index R (mm/h0.5), which is the ratio of frost heave to square root of time, is identified based on the proposed model. Through comparison with the large number of frost heave results, the value of R less than 0.21 indicates the low frost heave classification, that between 0.21 and 1.18 represents the medium heave classification, and that greater than 1.18 means the high frost heave classification. From a statistical probability perspective, the probability density distribution of the values of each classification index is analyzed, and their trends are also compared. It is found that the concentration and stability of the new index R are the highest during freezing process. The new index R has theoretical support and simultaneously couples the basic soil properties and freezing environmental factors. It breaks through the limitation of the existing indexes, and enriches the frost heave classification system, and provides theoretical support for the engineering design in cold regions.

     

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