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A Comprehensive Geochemical-Based Approach at Modeling and Interpreting Brine Dilution in Carbonate Reservoirs

机译:碳酸盐储层盐水稀释的综合地球化学方法

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It has been amply proven through laboratory studies, affirmed by a few field trials, that dilution of brine injected has a potent impact on improving oil recovery in carbonate reservoirs. However, debate still exists as to the mechanisms responsible for such impact. The widely acknowledged underlying mechanism is the wettability alteration, achieved through a combination of lower ionic strength, multi-ion exchange, surface charge and mineral alteration. Therefore, the motive behind this study is to develop a model that can further support and interpret the brine dilution approach in the framework of carbonate reservoirs. In this paper, we formulated a theory for the observed behavior that coupled equations of multi- component transport and geochemical reactions. The geochemical system considered a choice of significant ions and minerals, relevant to the published experiments. Mechanisms included in the model were dispersion/diffusion, instantaneous equilibrium reactions in terms of intra-aqueous and sorption reactions, and non-equilibrium rate controlled kinetic reactions-mineral alteration. The equivalent modification in wettability was represented by interpolating through a set of flow functions, particularly the relative permeability characteristics. The model was employed to interpret recently published experimental data on carbonate core plugs (Austad et al. (2011); Yousef et al. (2011); Yi and Sarma (2012); Chandrasekhar and Mohanty (2013)) where systematic dilutions of injectate against the initial formation brine were analyzed. Considering known values of injection rate, thermodynamic equilibrium constants, and reaction rate constants, the model was able to capture the trend of the experimental oil recovery and effluent ion concentrations. Thus, the model could help interpret the observed behavior as a sequel to an interplay between surface charge and mineral alteration. The trend typically reflected a speedy transient period at early times, trailed by relaxed transient period and finally reaching a steady state solution. The model was used to closely examine the dominant chemical mechanism responsible for improved oil mobilization relating to brine dilution during smart waterflooding. A thorough understanding of the mechanisms at play during any recovery process is crucial for its successful implementation as well as reliable production modeling, forecasting and optimization.
机译:通过实验室研究已被验证,通过一些现场试验肯定,稀释对碳酸盐储层中的油回收有效地影响盐水稀释。但是,辩论仍然存在对负责此类影响的机制。广泛承认的潜在机制是润湿性改变,通过较低离子强度,多离子交换,表面电荷和矿物改变来实现。因此,这项研究背后的动机是开发一种可以进一步支持和解释碳酸盐储层框架中的盐水稀释方法的模型。在本文中,我们制定了观察到的特征的理论,其偶联多组分传输和地球化学反应的方程。地球化学系统认为是与已发表的实验相关的重要离子和矿物质的选择。该模型中包含的机制是分散/扩散,在水中和吸附反应方面的瞬时平衡反应,以及非平衡速率控制的动力学反应 - 矿物质改变。通过通过内插通过一组流动功能,特别是相对渗透性特性来表示润湿性的等效修改。该模型用于在碳酸核插塞上解释最近公布的实验数据(Austad等(2011); YiSef等人; yi和Sarma(2012); Chandrasekhar和Mohanty(2013)),系统稀释的注射针对初始形成盐水进行了分析。考虑到注射速率,热力学平衡常数和反应速率常数的已知值,该模型能够捕获实验性油回收和流出离子浓度的趋势。因此,该模型可以帮助将观察到的行为解释为表面电荷和矿物改变之间的相互作用的续集。该趋势通常在早期的瞬态时期反映出早期的瞬态时段,由松弛的瞬态周期落后,最后达到稳态解决方案。该模型用于密切研究负责改善智能水上稀释的油动稀释的主要化学机制。在任何恢复过程中对游戏机制的彻底了解对其成功实施以及可靠的生产建模,预测和优化至关重要。

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