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首页> 外文期刊>Energies >Prediction of Layered Thermal Conductivity Using Artificial Neural Network in Order to Have Better Design of Ground Source Heat Pump System
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Prediction of Layered Thermal Conductivity Using Artificial Neural Network in Order to Have Better Design of Ground Source Heat Pump System

机译:为了更好地设计地源热泵系统,使用人工神经网络预测分层导热系数

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Ground source heat pumps (GSHPs) have been widely applied worldwide in recent years because of their high efficiency and environmental friendliness. An accurate estimation of the thermal conductivity of rock and soil layers is important in the design of GSHP systems. The distributed thermal response test (DTRT) method incorporates the standard test with a pair of fiber optic-distributed temperature sensors in the U-tube to accurately calculate the layered thermal conductivity of the rock/soil. In this work, in situ layered thermal conductivity was initially obtained by DTRT for four boreholes in the study region. A series of laboratory tests was also conducted on the rock samples obtained from drilling. Then, an artificial neural network (ANN) model was developed to predict the layered thermal conductivity on the basis of the DTRT results. The primary modeling factors were water content, density, and porosity. The results showed that the ANN models can predict the layered thermal conductivity with an absolute error of less than 0.1 W/(m·K). Finally, the trained ANN models were used to predict the layered thermal conductivity for another study region, in which only the effective thermal conductivity was measured with the thermal response test (TRT). To verify the accuracy of the prediction, the product of pipe depth and layered thermal conductivity was suggested to represent heat transfer capacity. The results showed that the discrepancies between the TRT and ANN models were 5.43% and 6.37% for two boreholes, respectively. The results prove that the proposed method can be used to determine layered thermal conductivity.
机译:近年来,由于地源热泵(GSHP)的高效性和环境友好性,已在世界范围内得到广泛应用。在GSHP系统的设计中,准确估算岩石和土壤层的导热系数非常重要。分布式热响应测试(DTRT)方法将标准测试与U型管中的一对光纤分布式温度传感器结合在一起,以准确计算岩石/土壤的分层导热率。在这项工作中,最初通过DTRT获得了研究区域中四个钻孔的原位分层导热系数。还对从钻孔获得的岩石样品进行了一系列的实验室测试。然后,建立了人工神经网络(ANN)模型,以根据DTRT结果预测层状导热系数。主要的建模因素是水含量,密度和孔隙率。结果表明,人工神经网络模型可以预测层状导热系数,绝对误差小于0.1 W /(m·K)。最后,训练有素的人工神经网络模型用于预测另一个研究区域的分层导热系数,其中仅通过热响应测试(TRT)测量了有效导热系数。为了验证预测的准确性,建议使用管道深度和分层导热系数的乘积来表示传热能力。结果表明,两个井眼的TRT和ANN模型之间的差异分别为5.43%和6.37%。结果证明,该方法可用于确定层状导热系数。

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