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首页> 外文期刊>Hydrogeology journal >The thermal impact of aquifer thermal energy storage (ATES) systems: a case study in the Netherlands, combining monitoring and modeling
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The thermal impact of aquifer thermal energy storage (ATES) systems: a case study in the Netherlands, combining monitoring and modeling

机译:含水层热能存储(ATES)系统的热影响:以荷兰为例,结合了监测和建模

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Results are presented of a comprehensive thermal impact study on an aquifer thermal energy storage (ATES) system in Bilthoven, the Netherlands. The study involved monitoring of the thermal impact and modeling of the three-dimensional temperature evolution of the storage aquifer and over- and underlying units. Special attention was paid to non-uniformity of the background temperature, which varies laterally and vertically in the aquifer. Two models were applied with different levels of detail regarding initial conditions and heterogeneity of hydraulic and thermal properties: a fine-scale heterogeneity model which construed the lateral and vertical temperature distribution more realistically, and a simplified model which represented the aquifer system with only a limited number of homogeneous layers. Fine-scale heterogeneity was shown to be important to accurately model the ATES-impacted vertical temperature distribution and the maximum and minimum temperatures in the storage aquifer, and the spatial extent of the thermal plumes. The fine-scale heterogeneity model resulted in larger thermally impacted areas and larger temperature anomalies than the simplified model. The models showed that scattered and scarce monitoring data of ATES-induced temperatures can be interpreted in a useful way by groundwater and heat transport modeling, resulting in a realistic assessment of the thermal impact.
机译:在荷兰的比尔霍芬,对含水层热能存储(ATES)系统进行的综合热影响研究的结果已提交。该研究涉及热影响的监测以及储层含水层以及上层和下层单元的三维温度演化模型。特别要注意背景温度的不均匀性,该温度在含水层中横向和纵向都变化。应用了两个模型,这些模型在初始条件以及水力和热力特性的非均质性方面有不同的详细程度:一个精细尺度的非均质性模型,它更真实地解释了横向和垂直温度分布;一个简化的模型,它仅表示了有限的含水层系统。均匀层数。研究表明,精细尺度的异质性对于准确模拟ATES影响的垂直温度分布,储层含水层的最高和最低温度以及热羽流的空间范围非常重要。与简化模型相比,精细尺度异质性模型导致更大的热影响面积和更大的温度异常。这些模型表明,可以通过地下水和热传输模型以有用的方式解释ATES引起的温度的零散和稀缺的监测数据,从而对热影响进行实际评估。

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