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Beyond Dual-Porosity Modeling for the Simulation of Complex Flow Mechanisms in Shale Reservoirs

机译:超出双孔隙率建模,用于仿真页岩储层复杂流动机制

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The state of the art of modeling fluid flow in shale reservoirs is dominated by dual porosity models which divide the reservoirs into matrix blocks that significantly contribute to fluid storage and fracture networks which principally control flow capacity. However, recent extensive microscopic studies reveal that there exist massive micro- and nano- pore systems in shale matrices. Because of this, the actual flow mechanisms in shale reservoirs are considerably more complex than can be simulated by the conventional dual porosity models and Darcy’s Law. Therefore, a model capturing multiple pore scales and flow can provide a better understanding of complex flow mechanisms occurring in these reservoirs. Through the use of a unique simulator this paper presents a micro-scale multiple-porosity model for fluid flow in shale reservoirs by capturing the dynamics occurring in three separate porosity systems: organic matter (mainly kerogen), inorganic matter, natural fractures. Inorganic and organic portions of shale matrix are treated as sub-blocks with different attributes, such as wettability and pore structures. In the organic matter or kerogen, gas desorption and diffusion are the dominant physics. Since the flow regimes are sensitive to pore size, the effects of nanopores and vugs in kerogen are incorporated into the simulator. The separate inorganic sub-blocks mainly contribute to the ability to better model dynamic water behavior. The multiple porosity model is built upon a unique tool for simulating general multiple porosity systems in which several porosity systems may be tied to each other through arbitrary transfer functions and connectivities. This new model allows us to better understand complex flow mechanisms and in turn is extended into the reservoir scale considering hydraulic fractures through upscaling techniques. Sensitivity studies on the contributions of the different flow mechanisms and kerogen properties give some insight as to their importance. Results also include a comparison of the conventional dual porosity treatment and show that significant differences in fluid distributions and dynamics are obtained with the improved multiple porosity simulation. Finally a case for reservoir-scale model covering organic matter, inorganic matter, natural fractures and hydraulic fractures is presented and will allow operators to better predict ultimate recovery from shale reservoirs.
机译:在页岩储层中建模的流体流动的技术是由双孔隙率模型的主导,其将储存器分成基质块,这显着促进了主要控制流量的流体储存和裂缝网络。然而,近期广泛的显微镜研究表明,页岩基质中存在巨大的微孔和纳米孔系统。因此,页岩储存器中的实际流量机制比传统的双孔隙率模型和达西法律模拟更复杂。因此,捕获多个孔径和流量的模型可以更好地理解这些储存器中发生的复杂流动机制。通过使用独特的模拟器本文通过捕获三个单独的孔隙率系统中发生的动态来提出页岩储层中的流体流量的微级多孔孔隙率模型:有机物(主要是角质原),无机物质,天然骨折。岩浆基质的无机和有机部分被视为具有不同属性的子块,例如润湿性和孔结构。在有机物或角质原中,气体解吸和扩散是显性物理学。由于流量制度对孔径敏感,因此纳米孔和Vug在基因中的效果掺入模拟器中。单独的无机子块主要有助于更好地模范动态水行为的能力。多孔隙度模型基于用于模拟一般多孔系统的独特工具,其中多个孔隙率系统可以通过任意传递函数和连接彼此依次捆绑。这种新模型使我们能够更好地理解复杂的流量机制,并且通过升高技术考虑液压骨折的储层规模延伸到储层规模中。对不同流动机制和基因特性贡献的敏感性研究表述了对其重要性的欣赏。结果还包括常规双孔隙率处理的比较,并表明利用改进的多孔孔隙模拟获得了流体分布和动力学的显着差异。最后提出了覆盖有机质,无机物质,自然骨折和液压骨折的储层规模模型的案例,并使运营商能够更好地预测来自页岩储层的最终恢复。

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