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Numerical Investigation of Effective Thermal Conductivity of Rock-like Material Using Mesoscopic Method

机译:介读法的岩状材料有效导热率的数值研究

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A two dimensional finite element model is proposed to predict the effective thermal conductivity of rock sample. The heterogeneity of rock is taking into account in the numerical model at mesoscopic level by employ the statistical method. Finite element models simulated a steadystate thermal conductivity measurement device performing measurements on numerical samples with varying heterogeneity. The results obtained by numerical model agree well with that of theoretical serial and parallel model, and seems more accurate to predict effective thermal conductivity of the disordered structure. The simulations of different heterogeneity samples show the relationship between effective thermal conductivity and heterogeneity. For specimens with same geometry and heterogeneity, although the distribution of thermal parameters in each sample are different because of random distribution, numerical results show that they are almost the same effective thermal conductivity. The results also indicate that different heterogeneity of the specimen will get different effective thermal conductivity, more homogeneous of the sample, smaller difference with the input thermal conductivity. The heat flux vector of relatively heterogeneous sample is more disordered than that of homogeneous one. It deems that the microfractures in rock have the resistance effect on heat conduction. All of the results reveal that the proposed numerical model efficiently predicting the effective thermal conductivity of the heterogeneity rock.
机译:提出了二维有限元模型,以预测岩石样品的有效导热率。通过采用统计方法,在介术水平的数值模型中考虑了岩石的异质性。有限元模拟模拟具有不同异质性的数值样品对数值样品进行测量的稳态热导率测量装置。通过数值模型获得的结果与理论串行和平行模型的结果很好,似乎更准确地预测无序结构的有效导热率。不同异质性样品的模拟显示有效导热率和异质性之间的关系。对于具有相同几何形状和异质性的标本,尽管由于随机分布而在每个样品中的热参数分布不同,但数值结果表明它们几乎是相同的有效导热性。结果还表明,样品的不同异质性将得到不同的有效导热性,更均匀的样品,与输入导热率较小的差异。相对异质样品的热通量载体比均匀的样品更紊乱。它认为岩石中的微磨术具有对热传导的抵抗力。所有结果表明,所提出的数值模型有效地预测异质性岩石的有效导热率。

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