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Ground thermal conductivity for (ground source heat pumps) GSHPs in Korea

机译:韩国(地源热泵)GSHP的地面导热系数

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摘要

The aim of this study is to evaluate the characteristic thermal properties of 208 (thermal response test) TRT data sets collected in Korea. In the evaluation, the line-source model is used in conjunction with the step-wise evaluation to validate the applicability of the model. The applicability of the step-wise evaluation is classified focusing on the convergence criterion of ground thermal conductivities. The ground thermal conductivities were evaluated in the range of 1.73 and 8.56 W/m·K with the mean of 2.55 W/m·K. The corresponding borehole thermal resistances were also obtained in the range between 0.06 and 0.20 m·K/W with the mean 0.13 m·K/W. In order to investigate the availability of the thermal conductivity of the test sites from the geothermal database in Korea, the ground thermal conductivity obtained by TRTs was compared with the mean bedrock thermal conductivity. Comparison of the four major bedrocks in the test sites indicated that the mean differences are 0.34, 0.53, 0.22 and 1.39 W/m·K at the bedrocks of the granite, geneiss, tuff and sandstone areas, respectively.
机译:这项研究的目的是评估在韩国收集的208个(热响应测试)TRT数据集的特征热特性。在评估中,线源模型与逐步评估结合使用,以验证模型的适用性。逐步评估的适用性集中在地面热导率的收敛准则上。地热导率在1.73和8.56 W / m·K的范围内评估,平均值为2.55 W / m·K。在0.06至0.20 m·K / W的范围内也获得了相应的钻孔热阻,平均值为0.13 m·K / W。为了从韩国的地热数据库中调查测试地点的热导率的可用性,将通过TRT获得的地面热导率与平均基岩热导率进行了比较。在测试地点对四种主要基岩的比较表明,在花岗岩,岩相,凝灰岩和砂岩地区的基岩处,平均差异分别为0.34、0.53、0.22和1.39 W / m·K。

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