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Foam flow in low-permeability berea sandstone cores: a laboratory investigation

机译:低渗透性Berea砂岩岩心中的泡沫流动:实验室研究

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Foam flow in porous media has been a subject of extensive investigation for the last 37 years because of its application in enhanced oil recovery (EOR) and stimulation operations. In acidizing, foam is used to facilitate the diversion of acid into the low-permeability strata when multiple layers of contrasing permeabilities are present. Very little has been done to investigate the flow behavior of foam in low-permeability rocks (1-10 md), mainly because of equipment limitations caused by the very high pressure gradients encountered whe foam is injected. This paper discusses the results of several single-core,constant-quality, steady-state foam flow experiments, using a 9-md fired Berea Sandstone core and a 3500 psi (24 MPa) rated coreflooding unit. Factors, such as surfactant type, foam quality, liquid and gas velocities, were varied to investigate their effect on foam mobility, mobility reduction factors, and pressure gradients. To simulate the post-foam acid stage used in acidizing, brine was injected following foam injection in each experiment and the residual permeability and foam stability were observed. The foam qualities used varied from 55% to 90%, and the injection rates varied from 5 to 25 ft/day (1.5-7.5 m/day). Significant reductions in mobilities were observed for all the cases during steady-state foam injection. A new parameter called the persistency index is proposed to quantify foam stability during the post-foam acid stage, which may prove to be critical to predicting the foam diversion behavior. Also, more consistent results were obtained when dimensionless parameters such as mobility reduction factors rather than mobilities were compared. Finally, low-permeability results were compared with those for the higher permeability to identify uniqueness of foam generation in low-permeability formations.
机译:在多孔介质中的泡沫流动在过去的37年中一直是广泛研究的课题,因为它在提高采油率(EOR)和增产作业中的应用。在酸化过程中,当存在多个相反渗透率的层时,使用泡沫来促进酸转移至低渗透率层中。研究泡沫在低渗透性岩石(1-10 md)中的流动行为的工作很少,主要是由于注入泡沫时遇到的非常高的压力梯度所引起的设备限制。本文讨论了使用9-md燃烧的Berea砂岩岩心和额定3500 psi(24 MPa)的岩心驱替单元进行的几个单核,恒定质量,稳态泡沫流动实验的结果。改变诸如表面活性剂类型,泡沫质量,液体和气体速度之类的因素以研究它们对泡沫迁移率,迁移率降低因子和压力梯度的影响。为了模拟用于酸化的泡沫后酸阶段,在每个实验中在注入泡沫之后注入盐水,并观察到残留的渗透性和泡沫稳定性。所使用的泡沫质量从55%到90%不等,注射速率从5到25 ft /天(1.5-7.5 m /天)不等。在稳态泡沫注射过程中,所有情况下的运动性均明显降低。提出了一个称为持久性指数的新参数来量化泡沫后酸阶段的泡沫稳定性,这对于预测泡沫的转向行为可能至关重要。同样,当比较无量纲参数(例如迁移率降低因子而不是迁移率)时,可以获得更一致的结果。最后,将低渗透率的结果与较高渗透率的结果进行比较,以确定低渗透率地层中泡沫生成的独特性。

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