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The impact of diagenesis precipitation on fracture permeability in naturally fractured carbonate reservoirs

机译:成岩作用沉淀对天然裂缝碳酸盐储层中骨折渗透性的影响

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Naturally fractured carbonate reservoirs are often described as very heterogeneous systems due to the carbonate depositional environment and to the subsequent diagenesis processes such as mineral precipitation in fractures. Fluid flow behaviour in fractures is highly influenced by the fracture aperture size and its morphology. Mineral precipitation can alter the fracture effectiveness to the fluid flow and cause a partial or entire blockage of fractures. Therefore, accurate characterisation of the fracture morphology can help to enhance the prediction of the fluid flow behaviour in naturally fractured carbonate reservoirs. Mineral precipitation on fracture walls can reduce the fracture aperture significantly. As a result, the fracture permeability affected notably, which reduces the flow potential through fractures as well as changes the flow pattern. The objective of this work is to predict the flow behaviour in fractures under various levels of mineral precipitation to mimic reality. We have approached this objective by using outcrop-based models supported by a set of rock and fluid properties of a nearby fractured formation. Then, the model tested for the gas flow using the derivative plot technique of the synthetic well testing data. The simulation results have shown that mineral cementation can cause a partial blockage in fractures, hence a reduction in their flow capacity, as fractures become a less conductive medium. Nevertheless, the matrix medium can enhance the fluid flow in fractures by providing a bypass path to the fluid to overcome the sealed fractures. In this work, a formula has concluded to estimate the reduction in fracture permeability based on the fraction of the precipitated cement. In the studied formation, the core description has shown that 34% of fractures were blocked, which can lead to a reduction in the permeability by 29-64% and by 37-83% with and without matrix contribution, respectively. Thus, including the fracture morphology in the simulation model enables us to predict the performance of fractured carbonate reservoirs accurately.
机译:由于碳酸盐岩沉积环境和随后的成岩作用(如裂缝中的矿物沉淀),天然裂缝性碳酸盐岩储层通常被描述为非常不均匀的系统。裂缝中的流体流动行为高度受裂缝孔径大小及其形态的影响。矿物沉淀会改变压裂液流动的有效性,并导致裂缝部分或全部堵塞。因此,准确描述裂缝形态有助于加强对天然裂缝性碳酸盐岩储层中流体流动行为的预测。裂缝壁上的矿物沉淀可显著减小裂缝孔径。因此,裂缝渗透率受到显著影响,从而降低了通过裂缝的流动势,并改变了流动模式。这项工作的目的是预测不同矿物沉淀水平下裂缝中的流动行为,以模拟现实。我们通过使用基于露头的模型来实现这一目标,该模型由附近断裂地层的一组岩石和流体特性支持。然后,利用合成试井数据的导数图技术对模型进行了气流测试。模拟结果表明,随着裂缝成为导电性较差的介质,矿物胶结会导致裂缝部分堵塞,从而降低其流动能力。然而,基质介质可以通过为流体提供旁路来克服密封裂缝,从而增强裂缝中的流体流动。在这项工作中,得出了一个公式,用于根据沉淀水泥的比例估算裂缝渗透率的降低。在所研究的地层中,岩芯描述显示,34%的裂缝被堵塞,这可能导致渗透率分别降低29-64%和37-83%,无论是否有基质贡献。因此,在模拟模型中加入裂缝形态,可以准确预测裂缝性碳酸盐岩储层的动态。

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