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Hierarchical Organization of Flow Network in Fractured Carbonate Reservoirs: Identification and Characterization of Key Parameters

机译:裂缝碳酸盐储层流量网络的分层组织:关键参数的识别与表征

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From field data, outcrop observations, and ground-water flow studies, this paper illustrates that if the assessment of the fracture network organization is effectively an important stage of the reservoir characterization, it cannot be dissociated from the evaluation of the scale relationships, the relation with stratigraphy, and the distribution of fracture hydraulic properties. In Lacq Field, a giant gas field in a fractured carbonate reservoir, the flow network is assessed through the use of dynamic data. Vertical distribution of producing zones shows a very clear control of effective open fractures by stratigraphy, and therefore carbonate lithology. In the same time, producing zones are not located in the areas in which fracture density is the highest. Same results are obtained from the observations of in-situ fracture networks and water incomes in a tunnel and a subsurface quarry. It clearly demonstrates that fracture density is the not the driving parameter for flows, and could be anti-correlated with fracture effective aperture. The computation of equivalent permeability on fracture models shows that fracture aperture distribution (and therefore hydraulic properties distribution) is a more prevalent parameter for uncertainty assessment than fracture distribution. Lastly, the spacing between open producing fractures along vertical or horizontal profiles show either exponential or power-law experimental distributions, regarding the spatial correlation between geological features. This proves the hierarchical organization of the flows, together with the needs for an evolution of the simplistic representation of a constant matrix block size within each cell of the dual porosity reservoir model. These studies enable to up-date the typology of fractured reservoirs we previously published.
机译:本文从现场数据,露天观察和地下水流程研究表明,如果骨折网络组织的评估有效地是储层特征的重要阶段,则不能解离规模关系的评估,这一关系具有地层,以及断裂液压性能的分布。在LACQ领域,通过使用动态数据来评估裂缝碳酸盐储层中的巨型气体场。生产区的垂直分布显示了通过地层的有效开放性裂缝的非常清晰控制,因此碳酸盐岩性。同时,生产区域不位于断裂密度最高的区域中。从隧道和地下采石场的原位骨折网络和水收入的观察结果获得了相同的结果。它清楚地表明断裂密度是流动的驱动参数,并且可以与断裂有效孔的反相关。裂缝模型等同渗透性的计算表明,断裂孔径分布(以及因此液压性质分布)是比骨折分布的不确定性评估更普遍的参数。最后,沿着垂直或水平剖面的开放式裂缝之间的间距显示了关于地质特征之间的空间相关性的指数或动力法实验分布。这证明了流量的分层组织,以及对双孔隙储层模型的每个小区内的恒定矩阵块尺寸的简单表示的演化的需要。这些研究使我们以前发表过的破碎储层的类型。

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