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Influence of the Moisture Content and Temperature on the Thermal Properties of Soils: Laboratory Investigation and Theoretical Analysis

机译:水分含量和温度对土壤热特性的影响:实验室调查与理论分析

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The paper presents the results of the laboratory investigation of thermal conductivity of clayey soils subjected to different moisture contents. The conductivities of soil specimens are evaluated at two extreme cases: fully saturated and dried state. The latter state is achieved by drying the soil specimens in the temperature 105°C. The needle probe test is used for laboratory measurements. Theoretical analyses, with the use of two different homogenization approximation schemes, namely the Mori-Tanaka and the Self-consistent are performed. Using laboratory results and treating them as effective conductivities the conductivity of solid as well as the geometry of pores are found. Calibrated model gives the possibility of calculating the effective conductivity of the soil in two considered cases: fully saturated and dried state.
机译:本文介绍了对不同水分含量的粘土土壤热导率的实验室调查结果。土壤样本的导电性在两个极端情况下评估:完全饱和和干燥状态。后一种状态通过在105℃的温度下干燥土壤样品来实现。针头探针试验用于实验室测量。通过使用两种不同的均质近似方案,即森林和自我一致的理论分析。使用实验室结果并将其视为有效的导电性,找到固体的电导率以及孔的几何形状。校准模型提供了在两种所考虑的情况下计算土壤有效电导率的可能性:完全饱和和干燥状态。

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