首页> 外文会议>Transportation Research Board Annual meeting >MODELING TEMPERATURE DISTRIBUTION IN SOIL PROFILE: IMPACTS OF MOISTURE TRANSPORT, SNOW COVER, AND SOIL FREEZING
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MODELING TEMPERATURE DISTRIBUTION IN SOIL PROFILE: IMPACTS OF MOISTURE TRANSPORT, SNOW COVER, AND SOIL FREEZING

机译:在土壤剖面中模拟温度分布:水分运输,积雪和土壤冻结的影响

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Prediction of soil temperature is important to simulation of work environment of pavement withsignif icant earth contact. A one-dimensional numerical model for heat and moisture transfer in partiallyfrozen soils has been developed and validated. In addition to modeling conduction heat transfer, modelvariat ions that include moisture transport, snow accumulation and melting and soil freezing and thawingare investigated. This model was evaluated against measured data at depths of 0.5 and 1.0 m for twolocations in the northern United States of America. The results show that the model is capable of providinggood simulat ions of the evolution of temperature all over the year. Comparisons of simulat ion results withfive combinat ions of modeled phenomena to experimental data demonstrate that both snow cover andfreezing and thawing of soil are of important when modeling temperature for soil. However, temperaturewas not substantially affected by the moisture transport.
机译:土壤温度的预测对于模拟沥青路面的工作环境具有重要的意义。 重要的接地接触。局部传热和水分传递的一维数值模型 已经开发并验证了冷冻土壤。除了对传导传热进行建模外,还对模型进行建模。 各种离子,包括水分输送,积雪和融化以及土壤冻结和解冻 被调查。针对两个深度为0.5和1.0 m的实测数据对该模型进行了评估 美利坚合众国北部的位置。结果表明,该模型能够提供 一年四季温度变化的良好模拟。模拟结果与 五个模拟现象与实验数据的结合表明,积雪和 在对土壤温度进行建模时,土壤的冻结和融化非常重要。但是温度 基本上不受水分传输的影响。

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