The impact of soil layering and groundwater flow on energy pile thermal performance

IF 3.3 2区 工程技术 Q3 ENERGY & FUELS
Qusi I. Alqawasmeh , Guillermo A. Narsilio , Nikolas Makasis , Monika J. Kreitmair
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引用次数: 0

Abstract

Shallow geothermal energy pile systems have emerged as cost-effective and low-carbon alternatives for heating and cooling buildings, compared to traditional air-conditioning systems. Geothermal applications have been researched extensively in recent years under the assumption of ground homogeneity, and the effect of ground stratification remains mostly unexplored. To investigate this, a 3D finite element numerical model is developed and validated against laboratory-scale experimental data, to study the transient diffusion-convection heat transfer linked with Darcy groundwater flow around energy piles in multi-layered lithology. The model is used to undertake long-term assessments under balanced and unbalanced thermal loads to evaluate the thermal effects of soil layering and discrepancies against commonly assumed equivalent homogeneous stratum, for soil profiles with different thermal conductivity distributions. The groundwater flow effect at various depths and seepage velocities on the thermal performance of the energy pile is investigated as well. Results demonstrate the need to account for the spatial variability in thermal properties, particularly for unbalanced thermal loading scenarios. The thermal yield can be underestimated by up to 19.6 % due to an inaccuracy of 48.2 % in the accumulated temperature after 25-year of operation with respect to an equivalent homogeneous ground with depth-weighted average thermal conductivity. This discrepancy grows as the contrast between layers increases. An empirical derived formula is presented and tested, presenting a correction to the effective thermal conductivity of the layered systems in this study that considers the thermal contribution of the ground beneath the pile. Groundwater seepage is shown to have a positive impact on the heat exchanger efficiency, and in the layered geology the efficiency under-estimation becomes more critical at low to moderate Darcy velocities, if neglected or inaccurately measured. These findings contribute to a broader understanding of energy piles and can assist engineers and practitioners in optimising energy geo-structure design, boosting the technology’s viability.

土壤分层和地下水流对能源桩热性能的影响
与传统的空调系统相比,浅层地热能桩系统已成为建筑物供暖和制冷的一种具有成本效益的低碳替代方案。近年来,在地层均匀性的假设下,地热应用得到了广泛的研究,而地层分层的影响大部分仍未得到探讨。为了研究这个问题,我们开发了一个三维有限元数值模型,并根据实验室规模的实验数据进行了验证,以研究多层岩性中能源桩周围与达西地下水流相关的瞬态扩散对流传热。该模型用于在平衡和不平衡热负荷下进行长期评估,以评估土壤分层的热效应,以及不同导热系数分布的土壤剖面与通常假设的等效均匀地层之间的差异。此外,还研究了不同深度和渗流速度的地下水流对能源桩热性能的影响。结果表明,需要考虑热性能的空间变化,特别是在不平衡热负荷情况下。与具有深度加权平均导热系数的等效均质地面相比,运行 25 年后的累积温度误差达 48.2%,因此热收益率可被低估达 19.6%。随着层间对比度的增大,这一误差也会增大。本研究提出并测试了一个经验推导公式,对分层系统的有效导热系数进行了修正,考虑了桩下地面的热贡献。结果表明,地下水渗流对热交换器的效率有积极影响,在分层地质中,如果忽略或测量不准确,在中低达西速度下,效率低估会变得更加严重。这些发现有助于人们更广泛地了解能源桩,有助于工程师和从业人员优化能源地质结构设计,提高该技术的可行性。
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来源期刊
Geomechanics for Energy and the Environment
Geomechanics for Energy and the Environment Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
5.90
自引率
11.80%
发文量
87
期刊介绍: The aim of the Journal is to publish research results of the highest quality and of lasting importance on the subject of geomechanics, with the focus on applications to geological energy production and storage, and the interaction of soils and rocks with the natural and engineered environment. Special attention is given to concepts and developments of new energy geotechnologies that comprise intrinsic mechanisms protecting the environment against a potential engineering induced damage, hence warranting sustainable usage of energy resources. The scope of the journal is broad, including fundamental concepts in geomechanics and mechanics of porous media, the experiments and analysis of novel phenomena and applications. Of special interest are issues resulting from coupling of particular physics, chemistry and biology of external forcings, as well as of pore fluid/gas and minerals to the solid mechanics of the medium skeleton and pore fluid mechanics. The multi-scale and inter-scale interactions between the phenomena and the behavior representations are also of particular interest. Contributions to general theoretical approach to these issues, but of potential reference to geomechanics in its context of energy and the environment are also most welcome.
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