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Investigation of Heat and Moisture Migration in Unsaturated Soil Under Natural Boundary Conditions

机译:自然边界条件下非饱和土壤热湿迁移的研究

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Theoretical and experimental investigations were conducted to determine the heat and moisture migration in unsaturated soil under natural surface boundary conditions. Theoretically, a new model of heat and moisture migration in unsaturated porous media was developed, in which the gradients of volume water content, temperature, and partiaI vapor pressure were considered as the main driving forces which influence the process of heat and moisture migration in unsaturated soil. A set of coupled, nonlinear, partial differential equations were developed, which are related dynamically to the surface boundary conditions. Heat and moisture migration in sandy soil under solar radiation and air convection were studied experimentally. Tempera- ture, volume water content, and water table evaporation were measured under unsteady conditions. The predictions are in good agreement with experimental data from a fairly sandy soil.
机译:为了确定自然表面边界条件下非饱和土壤中的热和水分迁移,进行了理论和实验研究。从理论上讲,建立了一种新的非饱和多孔介质中水分和水分迁移的模型,该模型将体积水含量,温度和偏蒸气压的梯度作为影响非饱和物质中水分和水分迁移过程的主要驱动力。泥。开发了一组耦合的非线性偏微分方程,这些方程与表面边界条件动态相关。实验研究了太阳辐射和空气对流作用下沙土中的热和水分迁移。在不稳定条件下测量温度,体积水含量和地下水位蒸发量。这些预测与来自沙质土壤的实验数据非常吻合。

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