陈永贵, 李泽垚, 孙曌, 叶为民, 王琼. 压实膨润土水化膨胀力的跨尺度理论预测模型[J]. 岩土工程学报. DOI: 10.11779/CJGE20250099
    引用本文: 陈永贵, 李泽垚, 孙曌, 叶为民, 王琼. 压实膨润土水化膨胀力的跨尺度理论预测模型[J]. 岩土工程学报. DOI: 10.11779/CJGE20250099
    Cross-scale theoretical prediction model for the hydration swelling pressure of compacted bentonite[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20250099
    Citation: Cross-scale theoretical prediction model for the hydration swelling pressure of compacted bentonite[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20250099

    压实膨润土水化膨胀力的跨尺度理论预测模型

    Cross-scale theoretical prediction model for the hydration swelling pressure of compacted bentonite

    • 摘要: 压实膨润土是高放废物深地质处置理想的缓冲回填材料,其水化膨胀力是缓冲性能评价的重要指标。为理论解析具有多重孔隙结构压实膨润土的膨胀力产生和发展机制,本文开展针对其水化膨胀力跨尺度传递的理论建模。首先依据压实膨润土的颗粒特征和结构特点为土体结构划分微结构元,并计算微结构元的等效物理力学参量;其次基于最小能量、最大熵等原理,求解土体完全水化时微结构元的分布概率;然后在颗粒-微结构元、微结构元-土体间膨胀力传递关系的力学分析基础上,建立微观力学参数与宏观膨胀力之间的联系,从而形成完整的膨润土水化膨胀力跨尺度理论预测模型。同时,以高庙子膨润土为研究对象,通过开展不同干密度、温度条件下宏观土体水化膨胀试验,对理论模型进行适用性检验。结果表明,预测值与试验结果之间的误差不超过16%,模型适用性较好。理论模型诠释了膨润土膨胀力跨尺度传递机制,为膨润土跨尺度结构性研究提供了新思路,可用于支持我国高放废物深地质处置库工程屏障系统的设计和性能评估。

       

      Abstract: Compacted bentonite is an ideal buffer/backfill material for high-level waste repositories, and its hydration swelling pressure is critical to the structural stability of the repository. This work is devoted to a cross-scale theoretical model of the hydration swelling pressure in bentonite. Firstly, the structure of bentonite is divided into microstructure units with their equivalent physical-mechanical properties calculated; secondly, the probability distribution of each microstructure units in soil structures is solved based on the principle of minimum energy and maximum entropy; then, by analyzing the mechanical connection between the particles and the microstructure units, and the microstructure units and the structure of soil, the cross-scale connection between the aggregate particles and the structure of bentonite in terms of physical-mechanical properties is realized. At last, the theoretical prediction model for the hydration swelling pressure of soil is established. At the same time, the hydration swelling test was performed on Gaomiaozi bentonite to measure its hydration swelling pressure. The applicability and accuracy of this theoretical model were examined by comparing the measured values with the predicted values. The results showed that the model applicability was well, the error between the predicted value and the experimental result is less than 16 %. The theoretical model also provides a new idea for the research on the cross-scale structural properties of bentonite. It could be used for the prediction and evaluation of the hydration swelling characteristics of buffer materials, which would contribute to the design and construction of repositories.

       

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