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SIMULATION OF DISSOLUTION FRONT PROPAGATION DURING ACID INJECTION INTO POROUS MEDIA: A CFD APPROACH

机译:酸注入多孔介质中的溶解前传播模拟:CFD方法

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Acid is often injected into porous media to dissolve rock material and enhance flow capability of the rock. Most simulation studies on the propagation of the dissolution front are based on constant injection rate (CIR). Therefore, the objective of this work is to develop numerical model to study acid dissolution front under constant injection pressure (CIP) and also incorporate the effect of fluid temperature on acid -rock interaction. Commercial computational Fluid Dynamics (CFD) software (ANSYS Fluent) is used to solve three-dimensional acid-rock interaction model in cylindrical coordinates. In this work, correlated porosity and permeability distributions are generated. Effect of heat transfer between the injected fluid and the formation on fluid properties and surface reaction rate are accounted for in the model. The study confirmed that all types of acid dissolution patterns exist during constant injection pressure. CIP technique requires lower acid volume to achieve breakthrough in the conical and branched dissolution regimes, than that is required for CIR technique. In dominant wormhole pattern, both techniques require nearly the same acid volume to breakthrough. Thermal interaction between the injected fluid and the formation leads to change of surface reaction rate and physical properties of the fluid, such as viscosity, density, and diffusivity. Injection of cold fluid into heated formation leads to a higher wormhole density as found from experimental studies due to retardation of surface reaction rate. The model developed in this work accurately captures different dissolution patterns. The model shows that the acid volume required for wormhole breakthrough depends on the inlet conditions (CIR or CIP) and the thermal interaction between the injected fluid and formation. This modeling study attempts to answer the critical questions pertaining to the effect of temperature and injection conditions on acid-rock interaction.
机译:通常将酸注入多孔介质中以溶解岩石材料并增强岩石的流动能力。大多数关于溶解前沿传播的模拟研究都是基于恒定注入速率(CIR)。因此,这项工作的目的是建立一个数值模型,以研究在恒定注入压力(CIP)下的酸溶解前沿,并且还包括流体温度对酸-岩相互作用的影响。商业计算流体动力学(CFD)软件(ANSYS Fluent)用于求解圆柱坐标系中的三维酸-岩相互作用模型。在这项工作中,生成了相关的孔隙度和渗透率分布。在模型中考虑了注入的流体和地层之间的热传递对流体性质和表面反应速率的影响。研究证实,在恒定的注射压力下,所有类型的酸溶解模式均存在。与CIR技术相比,CIP技术需要更低的酸量以实现圆锥形和支链溶解方式的突破。在主要的虫洞模式下,两种技术都需要几乎相同的酸体积才能突破。注入的流体与地层之间的热相互作用导致表面反应速率和流体的物理性质(例如粘度,密度和扩散率)的变化。从实验研究中发现,由于表面反应速率的延迟,将冷流体注入加热的地层会导致较高的虫洞密度。在这项工作中开发的模型可以准确地捕获不同的溶出模式。该模型表明,虫孔穿透所需的酸量取决于入口条件(CIR或CIP)以及注入的流体与地层之间的热相互作用。这项建模研究试图回答与温度和注入条件对酸-岩相互作用的影响有关的关键问题。

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