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Study on the Thermal-Hydraulic Coupling Model for the Enhanced Geothermal Systems

机译:增强型地热系统热工水力耦合模型研究

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Enhanced geothermal systems (EGS) are the major way of the hot dry rock (HDR) exploitation. At present, the finite element method (FEM) is often used to simulate the thermal energy extraction process of the EGS. Satisfactory results can be obtained by this method to a certain extent. However, when many discrete fractures exist in the computational domain, a large number of unstructured grids must be used, which seriously affects the computational efficiency. To solve this challenge, based on the embedded discrete fracture model (EDFM), two sets of seepage and energy conservation equations are respectively used to describe the flow and heat transfer processes of the matrix and the fracture media. The main advantages of the proposed model are that the structured grids can be used to mesh the matrix, and there is no need to refine the mesh near the fracture. Compared with commercial software, COMSOL Mul-tiphysics, the accuracy of the proposed model is verified. Subsequently, a specific example of geothermal exploitation is designed, and the spatial-temporal evolutions of pressure and temperature fields are analyzed.
机译:增强的地热系统(EGS)是干热岩(HDR)开发的主要途径。目前,有限元方法(FEM)通常用于模拟EGS的热能提取过程。通过这种方法可以在一定程度上获得满意的结果。但是,当计算域中存在许多离散裂缝时,必须使用大量非结构化网格,这严重影响了计算效率。为了解决这一难题,基于嵌入式离散裂缝模型(EDFM),分别使用两组渗流和能量守恒方程描述基体和裂缝介质的流动和传热过程。提出的模型的主要优点是结构化网格可用于对矩阵进行网格划分,而无需在裂缝附近细化网格。通过与商业软件COMSOL Multiphysics的比较,验证了所提模型的准确性。随后,设计了一个具体的地热开采实例,并分析了压力场和温度场的时空演化。

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