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Thermal conductivity of soils by the needle probe method, for energy foundation applications

机译:针探针法对土壤的导热性,用于能源基础应用

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摘要

Soil thermal conductivity is an important parameter in the design of ground source heat pump and energy foundation systems. One laboratory method for measuring the soil thermal conductivity is the needle probe method. Previously, analysis of the needle probe test data has been simplistic, relying heavily on human judgment and rules of thumb. This paper presents an alternative method of analyzing the needle probe data with the aid of a MATLAB program. Four agar-kaolin specimens of varying densities were prepared to resemble simple soils. These were tested using the needle probe for a range of heating times and heating powers, to see what effect these parameters would have on the results. The repeatability when keeping the heating time and heating power constant was within ±2%. When the heating time and heating power were varied, the variation in results from the average for a given specimen ranged from ±4% to +10%/-8%. This range is significantly higher than the repeatability. Possible reasons for this are discussed
机译:土壤热导率是地源热泵和能量基础系统设计中的重要参数。测量土壤热导率的一种实验室方法是针探针法。以前,对针探针测试数据的分析非常简单,很大程度上取决于人类的判断力和经验法则。本文介绍了借助MATLAB程序分析针探针数据的另一种方法。准备了四个密​​度不同的琼脂高岭土标本,以模拟简单的土壤。使用针型探针对这些样品进行了一系列加热时间和加热功率的测试,以了解这些参数会对结果产生什么影响。保持加热时间和加热功率恒定时的重复性在±2%以内。当加热时间和加热功率发生变化时,给定样品的平均结果变化范围为±4%至+10%/-8%。该范围明显高于重复性。讨论了可能的原因

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  • 年度 2014
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  • 正文语种 {"code":"en","name":"English","id":9}
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