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A Review of Two Methods to Model the Thermal Conductivity of Sands

机译:砂土导热系数的两种建模方法综述

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The effectiveness of two models to estimate the thermal conductivity of sands is reviewed. Haigh (2012) proposed an analytical model based on unidirectional heat flow through a three-phase soil element. Using a database of 155 test measurements, his model performed with similar effectiveness to the empirical model proposed by Chen (2008). The database used by Haigh (2012) depended largely on the measurements conducted by Chen (2008). Eighty of the 155 measurements were conducted on 4 high quartz content sands presented by Chen (2008). In this study thermal conductivity tests were conducted on 3 sands at dry and wet conditions. The effectiveness of the Haigh (2012) and Chen (2008) models are reviewed using the new dataset. Overall, both methods performed reasonably well and the conclusion of Haigh (2012) that his model out performed the empirical models was confirmed.
机译:审查了两种模型估计砂子导热系数的有效性。 Haigh(2012)提出了一种基于通过三相土壤单元的单向热流的分析模型。使用155个测试测量的数据库,他的模型的执行效果与Chen(2008)提出的经验模型相似。 Haigh(2012)使用的数据库在很大程度上取决于Chen(2008)进行的测量。 155次测量中的80次是在Chen(2008)提出的4种高石英含量的沙子上进行的。在这项研究中,在干燥和湿润的条件下在3个沙子上进行了导热系数测试。 Haigh(2012)和Chen(2008)模型的有效性使用新的数据集进行了回顾。总体而言,这两种方法均表现良好,并且Haigh(2012)得出的结论是他的模型执行了经验模型。

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