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Numerical manifold method for thermal-hydraulic coupling in fractured enhance geothermal system

机译:断裂增强地热系统中热液压耦合的数值歧管方法

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摘要

The geothermal production from enhance geothermal system (EGS) involves complex thermal-hydraulic (TH) coupling process, which may affect the production efficiency and performance of EGS reservoir. In the study, a numerical manifold method (NMM) for TH coupling in fractured EGS is proposed. The EGS reservoir is considered to be formed from intact rock matrix blocks and discrete fractures networks. TH coupling control equations are firstly established using discrete fracture networks model. Then, the weight residual method was used to establish the discretized governing equation for transient heat conduction. Furthermore, the element sub-matrixes for heat conduction were presented. NMM approach simulating the fluid flow, heat conduction in fracture and rock matrix and TH coupling process was established. Finally, a single fracture heat extraction example was used to validate the effectiveness of the proposed method for solving a simplified TH coupling problem. Furthermore, a 2D fracture networks case was conducted to predict the performance of an EGS reservoir. The results in here validate the capability and accuracy of the proposed method and extend the application of NMM.
机译:从增强地热系统(EGS)的地热产量涉及复杂的热液压(TH)耦合过程,这可能影响EGS储层的生产效率和性能。在研究中,提出了一种在裂缝EGS中耦合的数值歧管方法(NMM)。 EGS储库被认为是由完整的岩石矩阵块和离散裂缝网络形成的。首先使用离散裂缝网络模型建立TH耦合控制方程。然后,使用重量残留方法来建立用于瞬态导热的离散控制方程。此外,提出了用于热传导的元素子矩阵。建立了模拟流体流动,建立了骨折和岩石基质的热传导和Th耦合过程的方法。最后,使用单个裂缝热提取例来验证所提出的方法解决简化的TH耦合问题的有效性。此外,进行了2D裂缝网络壳体以预测EGS储存器的性能。结果在这里验证了所提出的方法的能力和准确性并延长了NMM的应用。

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