Effect of fracture structure on heat transfer in heat pipes in a submarine hydrothermal reservoir

IF 2.1 3区 地球科学 Q3 COMPUTER SCIENCE, INTERDISCIPLINARY APPLICATIONS Computational Geosciences Pub Date : 2024-06-24 DOI:10.1007/s10596-024-10301-1
Gaowei Yi, Yan Li, Da Zhang, Shiqiao Zhou
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Abstract

Complex geological structures like pores, fractures and faults in submarine hydrothermal reservoirs have significant but unclear effects on internal hydrothermal flow and heat transfer, which hinders reservoir exploitation. This study establishes a heat transfer model of a buried pipe coupled in fracture-porous media based on the reservoir characteristics. The model is verified through experiments using fractured porous media test rigs and computational fluid dynamics simulations. Simulations are performed to investigate the effects of fracture flow velocity, width, cornerstone porosity on the heat transfer efficiency of the buried pipe. Results show that optimizing fracture flow velocity, fracture width and cornerstone porosity can substantially improve the heat transfer performance of the buried pipe. Increasing fracture flow velocity from 10–4 m/s to 10–3 m/s, results in a 161.92% increase of Nusselt number. When the fracture width increases to 5 times the pipe diameter, Nusselt number rises by 35.52%. The heat transfer is optimal at a porosity of 0.3. This study provides theoretical guidance for exploiting submarine hydrothermal resources and designing fracture-porous couplings to enhance buried pipe heat transfer.

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断裂结构对海底热液储层热管传热的影响
海底热液储层中的孔隙、裂缝和断层等复杂地质结构对内部热液流动和传热的影响很大,但尚不明确,这阻碍了储层的开采。本研究根据储层特征,建立了裂缝-多孔介质耦合埋管的传热模型。通过使用裂缝多孔介质试验台进行实验和计算流体动力学模拟,对模型进行了验证。模拟研究了裂缝流速、宽度、基石孔隙度对埋管传热效率的影响。结果表明,优化断裂流速、断裂宽度和基石孔隙率可大幅提高地埋管的传热性能。将断裂流速从 10-4 m/s 提高到 10-3 m/s,可使努塞尔特数增加 161.92%。当裂缝宽度增加到管道直径的 5 倍时,努塞尔特数增加了 35.52%。孔隙率为 0.3 时,传热效果最佳。这项研究为开发海底热液资源和设计裂缝-多孔耦合器以增强埋管传热提供了理论指导。
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来源期刊
Computational Geosciences
Computational Geosciences 地学-地球科学综合
CiteScore
6.10
自引率
4.00%
发文量
63
审稿时长
6-12 weeks
期刊介绍: Computational Geosciences publishes high quality papers on mathematical modeling, simulation, numerical analysis, and other computational aspects of the geosciences. In particular the journal is focused on advanced numerical methods for the simulation of subsurface flow and transport, and associated aspects such as discretization, gridding, upscaling, optimization, data assimilation, uncertainty assessment, and high performance parallel and grid computing. Papers treating similar topics but with applications to other fields in the geosciences, such as geomechanics, geophysics, oceanography, or meteorology, will also be considered. The journal provides a platform for interaction and multidisciplinary collaboration among diverse scientific groups, from both academia and industry, which share an interest in developing mathematical models and efficient algorithms for solving them, such as mathematicians, engineers, chemists, physicists, and geoscientists.
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