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Modeling Discretely Fractured Geothermal Reservoirs: A Focus on Thermal Recovery, Fracture Intersections, and Fracture Roughness

机译:离散裂缝地热储层建模:以热采,裂缝相交和裂缝粗糙度为重点

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We present a numerical model to address several key reservoir structures of Engineered or Enhanced Geothermal Systems, including intersecting fractures and fracture roughness. The numerically simulated thermal recovery of a depleted model fractured EGS reservoir was similar to previously published findings. Recovery was initially rapid but slows down progressively and is primarily dominated by conduction in one direction. The mean fracture surface temperature can be easily estimated by knowing the total amount of thermal energy extracted and the thermophysical properties of the confining reservoir rocks. We demonstrated the capability of our model to simulate fracture intersections by showing two types of intersections in a two fracture system, an intersection parallel and perpendicular to the line connecting the injection and production well. Depending on the nature of the intersection different thermal performances occurred with the parallel intersection resulting in better performance due to better sweeping of the fracture surface. By studying a distribution of surface roughness within the aperture of a simulated fracture we observed that significant flow channeling occurred within the fracture and greatly affected the thermal performance of the reservoir. The surface roughness was assumed to have a self-affine geometry. For example, for dipole flow, flow channeling led to a better thermal performance in 25% of the simulated reservoirs by having higher production temperatures than the constant aperture case. In future work, we intend to use simulated tracer results predicted by our numerical model as a method to infer reservoir geometry and subsurface thermal conditions.
机译:我们提出了一个数值模型来解决工程或增强型地热系统的几个关键储层结构,包括相交的裂缝和裂缝的粗糙度。耗尽模型裂缝的EGS储层的数值模拟热采收率与先前发表的发现相似。恢复最初是快速的,但逐渐减慢,主要受一个方向的传导支配。通过了解所提取的热能总量和围岩储层的热物理性质,可以很容易地估算出平均裂缝表面温度。通过显示两个裂缝系统中的两种类型的交叉点(平行于并垂直于连接注入井和生产井的线的交叉点),我们证明了模型模拟裂缝交叉点的能力。根据交叉点的性质,平行交叉点会发生不同的热性能,这是由于裂缝表面的扫掠效果更好。通过研究模拟裂缝孔隙内表面粗糙度的分布,我们观察到裂缝内发生了明显的水流窜动,并极大地影响了储层的热力性能。假定表面粗糙度具有自仿射几何形状。例如,对于偶极子流,由于具有比恒定孔径情况更高的生产温度,因此在25%的模拟储层中,流道导致了更好的热性能。在未来的工作中,我们打算将数值模型预测的模拟示踪剂结果用作推断储层几何形状和地下热条件的方法。

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