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Efficient workflow for simulation of multifractured enhanced geothermal systems (EGS)

机译:高效的多裂隙增强地热系统(EGS)模拟工作流程

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摘要

The increasing demand for clean energy with minimum environmental impact motivates development of geothermal energy. Simulating a geothermal reservoir is complex and time consuming, mainly because of the systems spatial and temporal non-isothermal nature and the enormous size of the domain/reservoir. Simulations become even more complex when representing Enhanced Geothermal Systems (EGS), where wells in a hot, low permeability reservoir are interconnected by hydraulic fracturing to provide pathways for injection of cold water, in situ heating, and consequent production of hot water. In this study, various issues related to simulation of enhanced geothermal systems are investigated and practical solutions are proposed. A comprehensive study was conducted to show the effect of different grid systems on predictions of the transient temperature of the produced water. It is shown that the performance of an EGS is affected by the transmissivity (product of permeability and width of the fracture) of the fracture more so than by the values of permeability and width of the fracture considered individually. A simplified model (downscaled model) reduces the simulation times significantly (by 1.5-14.5 times) without compromising the accuracy of the results. In the proposed model, only two simulations - capturing small portions of the top and bottom of a reservoir with two active hydraulic fractures is used to evaluate performance of the entire reservoir. The proposed model is proved to be robust when exposed to different scenarios created by varying the inclination of the wells with respect to horizontal, spacing of the hydraulic factures, and spacing between the injection and producing wells. Value of R-2 close to unity (0.96-1.0) and smaller value of MAPE (Mean Absolute Percentage Error), less than 3% in comparison to the entire reservoir simulations, indicate the utility of proposed model. (C) 2018 Elsevier Ltd. All rights reserved.
机译:在对环境的影响最小的情况下,对清洁能源的需求不断增长,推动了地热能的发展。模拟地热储层是复杂且耗时的,主要是因为系统的时空非等温性质以及域/储层的巨大规模。当表示增强型地热系统(EGS)时,模拟变得更加复杂,在该系统中,低渗透性热的储层中的井通过水力压裂相互连接,从而为注入冷水,就地加热以及随后的热水生产提供了途径。在这项研究中,研究了与增强地热系统的模拟有关的各种问题,并提出了实际的解决方案。进行了一项综合研究,以显示不同网格系统对产出水瞬态温度预测的影响。结果表明,与单独考虑的裂缝的渗透率和宽度值相比,EGS的性能受裂缝的透射率(裂缝的渗透率和宽度的乘积)的影响更大。简化模型(缩小模型)可以在不影响结果准确性的情况下,显着减少仿真时间(减少1.5-14.5倍)。在提出的模型中,仅使用两个模拟-捕获具有两个活动水力压裂的油藏顶部和底部的一小部分来评估整个油藏的性能。当暴露于通过改变井相对于水平的倾角,水力压裂的间距以及注入井与生产井之间的间距而产生的不同场景时,所提出的模型被证明是可靠的。与整个油藏模拟相比,R-2的值接近于统一值(0.96-1.0),而MAPE(平均绝对百分比误差)值较小,小于3%,表明该模型的实用性。 (C)2018 Elsevier Ltd.保留所有权利。

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