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Evaluation of ground source heat pump system's enhancement by extracting groundwater and making artificial groundwater velocity

机译:用地下水提取地下源热泵系统增强评价并进行人工地下水速度

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This study used moving line source technique as a practical approach to simultaneously determine effective thermal conductivity, groundwater velocity and borehole resistance. It mainly focused on the applicability of this approach for observing the effect of groundwater extraction, in particular for ungrouted ground heat exchangers. The thermal response tests were carried out for different ground heat exchangers at two sites on the Akita University campus, northern Japan. The test conditions varied, based on different borehole filling condition (grouted/ungrouted), heat loads and presence of an extra pump for groundwater extraction. The hydro-thermal parameters of the ground were determined by a MATLAB code, especially for consideration of the effect of artificial groundwater velocity under a special test, where a water pump extracts the groundwater from the casing of the borehole during the test. This method can estimate the groundwater velocity and the effective thermal conductivity of the soil by reproducing the temperature distribution in the well and minimizing the mot mean squared error between the calculated results and the measured data. As a result, the groundwater velocity and thermal conductivity calculated by this method improved to 205.3 cm/day and 7.48 W/m K, respectively, due to presence of the external pump, whereas the undisturbed groundwater velocity in the other cases without pumping was estimated in the range of 15 to 16 cm/day. Furthermore, the minimum groundwater velocity and thermal conductivity were reported for the grouted well as being equal to 10.79 cm/day and 1.16 W/m K, respectively.
机译:本研究使用了移动线源技术作为同时确定有效的导热性,地下水速度和钻孔抗性的实用方法。它主要集中于这种方法的适用性,用于观察地下水提取的影响,特别是对于未加工的地面热交换器。在日本北部秋田大学校园的两个地点进行了热响应试验。基于不同的钻孔填充条件(灌浆/未放置),热负荷和用于地下水泵的额外泵的存在,试验条件变化。地面的水电热参数由MATLAB码确定,特别是考虑在特殊测试下的人造地下水速度的效果,其中水泵在测试期间从钻孔的壳体中提取地下水。该方法可以通过在井中再现温度分布并最小化计算结果和测量数据之间的温度分布来估计土壤的地下水速度和有效导热率。结果,由于外部泵的存在,通过该方法计算的地下水速度和导热率分别改善为205.3cm /天和7.48W / m k,而估计其他情况下不受干扰的地下水速度而不泵送。在15至16厘米/天的范围内。此外,报告了灌浆的最小地下水速度和导热性,分别等于10.79cm /天和1.16W / m k。

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