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Assessment of soil thermal conduction using artificial neural network models

机译:利用人工神经网络模型评估土壤热传导

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Thermal conductivity is a fundamental engineering property governing heat transfer process in soils. It depends on mineral component, compaction moisture content, dry density, soil gradation and temperature, and usually varies over an order of magnitude in soils with different status. The present study investigated the mechanism of heat transfer in soils and developed new models for thermal conductivity prediction via artificial neural network (ANN) technology. The performance of the proposed models (individual ANN model and generalized ANN model) were evaluated by comparing with three empirical models. Based on the results presented in this study, it is revealed that heat flow through soil was a multi-field coupled process (i.e., thermal-hydro-mechanical process) and was closely related to the intrinsic properties of three phases those constitute a soil. The cross validation was conducted to validate the reliability of the proposed models. It was concluded that both individual and generalized ANN models were able to provide good matching with laboratory measured thermal conductivity values. For each proposed model, the coefficient of correlation (R-2) and variance account for (VAF) values were close to 1, and the mean absolute error (MAE) and root mean square error (RMSE) were lower than 0.360 W/Km and 1.000 W/K m, respectively. Results taken from the comparison of various models showed that the generalized ANN model, with RMSE value lower than 0.100 W/K m, exhibited highest accuracy in thermal conductivity prediction of all types of soil, followed by individual ANN models and the empirical models. A good performance of the proposed models in frozen soils was observed with a limited size of thermal conductivity data.
机译:导热系数是控制土壤传热过程的基本工程特性。它取决于矿物成分,压实水分含量,干密度,土壤等级和温度,并且在状态不同的土壤中通常变化一个数量级。本研究调查了土壤中的传热机理,并开发了通过人工神经网络(ANN)技术预测导热系数的新模型。通过与三个经验模型进行比较,评估了所提出的模型(单个ANN模型和广义ANN模型)的性能。根据本研究的结果,表明通过土壤的热流是一个多场耦合过程(即热-水-机械过程),并且与构成土壤的三相的固有特性密切相关。进行交叉验证以验证所提出模型的可靠性。结论是,单独的和广义的ANN模型都能够与实验室测得的热导率值很好地匹配。对于每个提出的模型,相关系数(R-2)和方差帐户(VAF)值都接近1,平均绝对误差(MAE)和均方根误差(RMSE)低于0.360 W / Km和1.000 W / K m。从各种模型的比较中得出的结果表明,RMSE值低于0.100 W / K m的广义ANN模型在所有类型土壤的热导率预测中表现出最高的准确性,其次是各个ANN模型和经验模型。在有限的热导率数据中,观察到所提出的模型在冻结土壤中具有良好的性能。

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