首页> 外文期刊>Applied thermal engineering: Design, processes, equipment, economics >Decomposition and coupling of soil domain for modeling vertical ground heat exchangers using the state model size reduction technique
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Decomposition and coupling of soil domain for modeling vertical ground heat exchangers using the state model size reduction technique

机译:使用状态模型尺寸缩减技术对垂直地面换热器进行建模的土壤域的分解和耦合

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摘要

Numerical modeling of the ground heat exchangers requires important computational resources to accurately reproduce the short-time thermal responses over a long-time period. Considering geometries of the vertical ground heat exchanger, domain decomposition is proposed in the vertical and horizontal directions. As the principal direction of the heat transfer in such a system is horizontal and here the cumbersome finite element method in treating the domain decomposition is adopted, only the horizontal soil domain case is investigated in this work. A new type of boundaries to decomposed sub-zones is proposed, and then a restitution method is developed to keep all the matrix terms inherent in initial matrices ahead of decomposition. The state model size reduction technique is used for each sub-zone model to reduce the model size, and then the reduced models are regrouped into a single state model using the new proposed coupling method. Results show that the developed decomposition and coupling methods are pertinent with negligible errors (less than 0.005℃ for the maximum), and the final reduced model gives acceptable results for typical purposes of geothermal simulations. From some sensitivity tests, it is found that accuracy of the reduced model can be systematically improved by increasing the reduced order or the number of sub-zones. The proposed model is remarkably faster than the reference model (more than 300 times), implying that a detailed 3-D numerical model can be used for long-time simulations.
机译:地面换热器的数值建模需要重要的计算资源,才能长时间准确地重现短期热响应。考虑到垂直地面热交换器的几何形状,提出了在垂直和水平方向上的区域分解。由于在这种系统中传热的主要方向是水平的,在此采用处理区域分解的繁琐的有限元方法,因此在此工作中仅研究水平土壤区域的情况。提出了一种新的分解子区域边界,然后开发了一种复原方法,以使初始矩阵中固有的所有矩阵项都保持在分解之前。将状态模型尺寸缩减技术用于每个子区域模型以减小模型尺寸,然后使用新提出的耦合方法将简化后的模型重新组合为单个状态模型。结果表明,所开发的分解和耦合方法的相关误差可忽略不计(最大值小于0.005℃),最终的简化模型给出了可接受的典型地热模拟结果。从一些灵敏度测试中,发现可以通过增加缩小阶数或子区域数来系统地提高缩小模型的精度。所提出的模型比参考模型快得多(超过300倍),这意味着详细的3-D数值模型可用于长时间仿真。

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