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Numerical simulation of Fluid-Rock coupling heat transfer in naturally fractured geothermal system

机译:自然裂缝地热系统中流固耦合传热的数值模拟

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Estimating heat extraction from naturally fractured geothermal systems is a challenging task. Most of the previous works in this area assumed an instantaneous local thermal equilibrium while simulating heat extraction from the fractured geothermal systems. This paper investigates the role of heat transfer between the rock matrix and circulating fluid on economic hot water production from fractured geothermal systems. For this purpose a numerical procedure is developed by coupling fluid flow with heat transfer. The novelty of this approach lies in its dynamic treatment of the characteristic properties (aperture, length and orientation) of individual fractures in simulating fluid flow and heat transfer between rock and circulating fluid. A naturally fractured geothermal system with a medium fracture density of 0.05 m~(-1) is chosen for a case study. The results of this study have shown that heat transfer between rock and fluid and fracture connectivity has a profound effect on the economic potential of a geothermal reservoir.
机译:估算自然裂缝地热系统的热量提取是一项艰巨的任务。在模拟从破裂的地热系统中提取热量的同时,该地区的大多数先前工作都假定了瞬时局部热平衡。本文研究了岩石基质与循环流体之间的热传递对裂缝性地热系统经济热水生产的作用。为此,通过将流体流与热传递耦合来开发数值程序。这种方法的新颖之处在于它在模拟流体流动和岩石与循环流体之间的传热过程中动态处理单个裂缝的特征(孔径,长度和方向)。案例研究选择了中等裂缝密度为0.05 m〜(-1)的天然裂缝地热系统。这项研究的结果表明,岩石与流体之间的传热以及裂缝的连通性对地热储层的经济潜力具有深远的影响。

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