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首页> 外文期刊>Journal of Hydrology >A new friction factor correlation for laminar, single-phase flows through rock fractures
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A new friction factor correlation for laminar, single-phase flows through rock fractures

机译:层状单相流经岩石裂缝的新型摩擦系数相关性

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Single-phase flow through fractured media occurs in various situations, such as transport of dissolved contaminants through geological strata, sequestration of carbon dioxide in depleted gas reservoirs, and in primary oil recovery. In the present study, fluid flows through a rock fracture were simulated. The fracture geometry was obtained from the CT scans of a rock fracture produced by the Brazilian method in a sandstone sample. A post-processing code using a CAD package was developed and used to generate the three-dimensional fracture from the CT scan data. Several sections along the fracture were considered and the Gambit (TM) code was used to generate unstructured grids for flow simulations. FLUENT (TM) was used to analyze the flow conditions through the fracture section for different flow rates. Because of the small aperture of the fractures, the gravitational effects could be neglected. It was confirmed that the pressure drop was dominated by the smallest aperture passages of the fracture. The accuracy of parallel plate models for estimating the pressure drops through fractures was studied. It was shown that the parallel plate flow model with the use of an appropriate effective fracture aperture and inclusion of the tortuosity factor could provide reasonable estimates for pressure drops in the fracture. On the basis of the CFD simulation data, a new expression for the friction factor for flows through fractures was developed. The new model predictions were compared with the simulation results and favorable agreement was found. It was shown that when the length of the fracture and the mean and standard deviation of the fracture are known, the pressure loss as a function of the flow rate could be estimated. These findings may prove useful for design of lab experiments, computational studied of flows through real rock fractures, or inclusions in simulators for large-scale flows in highly fractured rocks. (c) 2006 Elsevier B.V. All rights reserved.
机译:通过裂隙介质的单相流发生在各种情况下,例如通过地质地层输送溶解的污染物,在贫气气藏中封存二氧化碳以及在一次采油中。在本研究中,模拟了流过岩石裂缝的流体。从巴西方法在砂岩样品中产生的岩石裂缝的CT扫描获得了裂缝的几何形状。开发了使用CAD软件包的后处理代码,并将其用于从CT扫描数据生成三维断裂。考虑了沿裂缝的几个部分,并使用Gambit(TM)代码生成了用于流动模拟的非结构化网格。 FLUENT(TM)用于分析通过不同流量的裂缝段的流动条件。由于裂缝的孔径较小,因此可以忽略重力作用。可以确定的是,压降由裂缝的最小孔径通道决定。研究了通过平行板模型估算裂缝压降的准确性。结果表明,采用适当的有效裂缝孔径并包含曲折系数的平行板流模型可以为裂缝中的压降提供合理的估计。在CFD模拟数据的基础上,开发了裂缝流动摩擦系数的新表达式。将新模型的预测结果与仿真结果进行了比较,发现了良好的一致性。结果表明,当已知裂缝的长度以及裂缝的均值和标准偏差时,可以估算出压力损失与流量的关系。这些发现可能被证明对实验室实验的设计,对真实岩石裂缝流动的计算研究或对高度裂隙岩石中大规模流动的模拟器包含物有用。 (c)2006 Elsevier B.V.保留所有权利。

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