双孔隙压实膨润土的细观导热模型
Mesoscale model for thermal conductivity of compacted dual-porosity bentonite
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摘要: 压实膨润土导热系数是评价核废料处置库散热安全以及计算温度场分布的关键指标,准确预测不同条件下压实膨润土导热系数对于处置库的安全设计具有重要意义。数值模拟是预测土体导热系数的有效途径之一,然而,由于压实膨润土双孔隙结构的复杂性,基于细观数值模拟的压实膨润土导热模型较少。建立了一种适用于双孔隙压实膨润土导热系数的细观模型,选取了不同含水率和孔隙比下5种典型压实膨润土160个实测导热数据,并与模型预测导热系数值进行比较。结果显示膨润土导热系数的模型预测值基本在实测值±20%范围内,有效验证了模型的可靠性,表明本文模型在压实膨润土导热系数预测方面的潜力。为复杂双孔隙压实膨润土导热系数的精确预测提供了一种新的思路和方法。Abstract: The thermal conductivity of compacted bentonite is very crucial in evaluating the safety of heat dissipation and in calculating the temperature distribution of radioactive waste repository. An accurate predictive model is of great significance to the calculation of their thermal conductivity under various conditions. A mesoscale model is proposed for the thermal conductivity of compacted dual-porosity bentonite by numerical simulation. The thermal conductivity of 160 measured samples is selected and compared with their simulated one for five typical kinds of compacted bentonite with different dry densities and water contents. The results show that the most predictive values are within ±20% range of the measured ones, which verifies the reliability of the model effectively. The results in this study provide a new approach and/or strategy to predict the thermal conductivity of the compacted dual-porosity bentonite.