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Heterogeneous bedrock investigation for a closed-loop geothermal system: A case study

机译:闭环地热系统的非均质基岩研究:一个案例研究

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摘要

This paper investigates bedrock heterogeneity by applying three different geophysical approaches, in order to study the long-term behaviour and the interaction between closed-loop geothermal systems. The investigated site consists of four boreholes equipped with geothermal pipes on the campus of University of Liege, Belgium. The first approach includes acoustic borehole imaging, gamma-ray logging and cuttings observation and results to a detailed fracture characterisation, rock identification and layer dip angle determination. The second approach consists of measuring the thermal conductivity of cuttings at the laboratory. Study of cuttings thermal conductivity measurements can contribute to bedrock heterogeneity knowledge concerning the transition of one formation to another and the layer dipping. The third approach is based on high-resolution temperature profiles, measured during the hardening of the grouting material and the recovery phase of a Distributed Thermal Response Test. Through this approach a correlation of the temperature profiles to the geological characteristics of the surrounding bedrock is identified. The analysis of this correlation can provide information on fractured zones, alternation of different rock types and layering dipping. This latter approach can be easily applied on closed-loop geothermal systems to characterise the bedrock and investigate its heterogeneity as well as contribute to the their long-term behaviour prediction and to the optimisation of their efficiency. (C) 2016 Elsevier Ltd. All rights reserved.
机译:本文应用三种不同的地球物理方法研究了基岩的非均质性,以研究闭环地热系统的长期行为及其相互作用。被调查的地点由比利时列日大学校园内的四个装有地热管道的钻孔组成。第一种方法包括声学钻孔成像,伽马射线测井和岩屑观测,并得到详细的裂缝特征,岩石识别和层倾角确定的结果。第二种方法包括在实验室测量碎屑的导热率。钻屑热导率测量的研究可以有助于基岩异质性知识,涉及一个地层过渡到另一个地层以及地层倾角。第三种方法基于高分辨率温度曲线,该温度曲线是在灌浆材料硬化和分布式热响应测试的恢复阶段测量的。通过这种方法,可以确定温度剖面与周围基岩地质特征的相关性。对这种相关性的分析可以提供有关断裂带,不同岩石类型的交替和层状倾角的信息。后一种方法可以很容易地应用于闭环地热系统,以表征基岩并研究其非均质性,并有助于其长期行为预测和效率优化。 (C)2016 Elsevier Ltd.保留所有权利。

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