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Adsorption- and Diffusion-Controlled Wettability Change in Modified Salinity Water Flooding

机译:改性盐水洪水的吸附和扩散控制的润湿性变化

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摘要

During the modified salinity water (MSW) flooding, the injected water must first reach and interact with the residual oil attached on the pore surfaces through a thin formation water film to mobilize the oil and improve the oil recovery. This can cause a delay in the rock response to the injection of MSW, as observed in many core flooding tests. The physicochemical processes that control this response time occur at two different scales: the alteration of wettability at the film scale and the consequent mobilization of oil at the Darcy scale. We propose a new model that links the diffusion- and adsorption-controlled flow of ions in the thin film to the two-phase flow of oil and water at the Darcy scale through a wettability-modifier parameter. This parameter is defined based on the salinity change in the water film or the adsorption/desorption of ions on the water-film-covered rock and is used as an interpolating parameter for two sets of relative permeability curves for the initial state and the new state of the reservoir. We utilize the model to analyze several core flooding results to first explain the observed oil breakthrough delay and second find out how much of this delay is expected to happen in the reservoir scale. Our results suggest that sizes of residual oil droplets and the effective ionic diffusion in the thin water film, dictated by the electrostatic charge of the oil–brine and rock–brine interfaces, play significant roles in controlling the oil breakthrough time. In addition, our observations suggest that the observed delay is strongly controlled by a rather slow diffusion process in the water film, which is not scalable from the core to field scale.
机译:在改性盐水(MSW)洪水期间,注入的水必须首先通过薄的形成水膜将其附着在孔表面上的残留油相互作用,以便动员油并改善油回收。这可能导致岩石反应对MSW的延迟,如在许多核心泛滥试验中所观察到的那样。控制该响应时间的物理化学过程发生在两种不同的尺度:薄膜规模上的润湿性的改变以及在达西规模处随后的油动员。我们提出了一种新的模型,将薄膜中的薄膜中的扩散和吸附控制的离子流链接到Darcy Super参数在Darcy Scalifer中将薄膜中的薄膜和水的两相流流动。该参数基于水膜中的盐度变化或水膜覆盖的岩石上的离子的吸附/解吸来定义,用作初始状态和新状态的两组相对渗透曲线的内插参数水库。我们利用模型来分析几个核心洪水结果,首先解释观察到的石油突破延误,第二个找出预期在储层规模中发生了多少这一延迟。我们的研究结果表明,通过油盐水和岩石界面的静电电荷决定的薄水薄膜中的剩余油滴和有效离子扩散的大小在控制油突破时间方面起显着作用。此外,我们的观察结果表明,观察到的延迟受水膜中的相当慢的扩散过程强烈控制,这是不可从核心可扩展到现场规模的。

著录项

  • 来源
    《Energy & fuels 》 |2020年第11期| 13767-13781| 共15页
  • 作者单位

    Danish Hydrocarbon Research and Technology Centre Technical University of Denmark;

    Danish Hydrocarbon Research and Technology Centre Technical University of Denmark;

    Danish Hydrocarbon Research and Technology Centre Technical University of Denmark;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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