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Analytical analysis of borehole experiments for the estimation of subsurface thermal properties

机译:估计地下热性质的钻孔实验分析

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Estimating subsurface thermal properties is required in many research fields and applications. To this end, borehole experiments such as the thermal response test (TRT) and active-line-source (ALS) method are of significant interest because they allow us to determine thermal property estimates in situ. With these methods, the subsurface thermal conductivity and diffusivity are typically estimated using asymptotic analytical expressions, whose simplifying assumptions have an impact on the accuracy of the values obtained. In this paper, we develop new analytical tools for interpreting borehole thermal experiments, and we use these tools to assess the impact of such assumptions on thermal property estimates. Quite importantly, our results show that the simplifying assumptions of currently used analytical models can result in errors in the estimated thermal conductivity and diffusivity of up to 60% and 40%, respectively. We also show that these errors are more important for short-term analysis and can be reduced with an appropriate choice of experimental duration. Our results demonstrate the need for cautious interpretation of the data collected during TRT and ALS experiments as well as for improvement of the existing in-situ experimental methods. (C) 2016 Elsevier Ltd. All rights reserved.
机译:在许多研究领域和应用中都需要估算地下热性质。为此,诸如热响应测试(TRT)和有源线源(ALS)方法之类的钻孔实验引起了人们的极大兴趣,因为它们使我们能够现场确定热属性估算值。使用这些方法,通常使用渐近分析表达式估算地下热导率和扩散率,其简化假设会影响所获得值的准确性。在本文中,我们开发了用于解释井眼热实验的新分析工具,并使用这些工具来评估这些假设对热力估算的影响。非常重要的是,我们的结果表明,当前使用的分析模型的简化假设可能导致估计的热导率和扩散率的误差分别高达60%和40%。我们还表明,这些误差对于短期分析更重要,并且可以通过适当选择实验持续时间来减少。我们的结果表明,需要谨慎解释在TRT和ALS实验期间收集的数据,以及改进现有的原位实验方法。 (C)2016 Elsevier Ltd.保留所有权利。

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