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Analytical model for heat transfer between vertical fractures in fractured geothermal reservoirs during water injection

机译:注水裂缝性地热储层垂直裂缝之间传热的解析模型

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In recent years, the demand for energy has vastly increased due to rapid commercialization. This increasing requirement has put a further strain on the conventional power generation units. In this paper, the problem of water injection into a fractured geothermal reservoir in Cartesian coordinate is considered and an exact analytical solution has been presented to describe the transient temperature distribution and advancement of the thermal front generate due to transient temperature of heat depleted water in a coupled fracture matrix system at the scale of a single fracture. This solution is able to explain the following phenomena: convection transport in fractures, conduction heat transfers in matrix block and heat flux transfer between rock matrix and fracture. Also, the heat transfer shape factor can be defined by employing the convection-conduction equation in matrix and fracture. The derived analytical solution was used for investigating early and late time periods of heat transfer phenomenon in naturally fractured reservoirs. In addition, a conceptual definition for thermal recovery efficiency has been offered as the rest of included materials. In order to validate the predicted temperature by analytical model in fractured geothermal reservoirs, the presented analytical model is compared with numerical and pervious analytical model. (C) 2018 Elsevier Ltd. All rights reserved.
机译:近年来,由于快速的商业化,对能源的需求已大大增加。这种不断增长的需求给传统的发电装置带来了进一步的压力。在本文中,考虑了在笛卡尔坐标系中向裂隙地热储层注水的问题,并提出了精确的解析解来描述瞬态温度分布和由于贫水在瞬态温度下瞬态温度引起的热锋产生的进展。单一裂缝尺度的耦合裂缝矩阵系统。该解决方案能够解释以下现象:裂缝中的对流输运,基质块体中的传导热传递以及岩石基质与裂缝之间的热通量传递。同样,可以通过在基质和裂缝中采用对流传导方程来定义传热形状因数。导出的分析解决方案用于调查自然裂缝储层中传热现象的早期和晚期时段。此外,还提供了热回收效率的概念定义,作为所含材料的其余部分。为了通过裂隙地热储层的解析模型验证预测温度,将所提出的解析模型与数值和透水解析模型进行了比较。 (C)2018 Elsevier Ltd.保留所有权利。

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