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Improvements on Modelling Wettability Alteration by Engineered WaterInjection:Geochemical Pore-Scale Approach

机译:经工程润滑油模拟润湿性改变的改进:地球化学孔隙尺度方法

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Several laboratory experiments demonstrated that different water compositions cause rocks to change fromoil-to water-wet state.Although it is a consensus that wettability alteration is the main recovery mechanism,modeling the underlying mechanism is still a major challenge.Our main goal is to improve and validatea physically based model to predict contact angles from zeta-potential measurements.We propose a newmass-action formulation for surface complexation model(SCM)that includes the energy interaction effectbetween two close surfaces(PS).Currently,most SCMs consider rock and oil as isolated surfaces(IS).Thus,we hypothesize that,as rock and oil surface approach each other,PS model produce a better descriptionof electrostatic distribution.Additionally,we develop a method of determining SCM equilibrium constantsto fit several zeta-potential measurements for different ion concentrations(Na+,Ca2+,Mg2+,SO42-andH+).Finally,we estimate contact angles using disjoining pressure calculations and compare them withones reported in the literature.From a SCM set of reactions available in the literature,we validate thedeveloped IS model against PHREEQC(a reference simulator for geochemical reactions).For the PS case,the system of equations'solution is very close to IS approach when the interaction between surfaces arenegligible(wide spacing between surfaces).Regarding zeta-potential prediction for calcite-brine system,we argue that Na+ might not be an indifferent ion as suggested previously.Our simulation results indicatethat,besides the renowned potential-determining ions,sodium adsorption on calcite can play an importantrole in electrostatic interactions,switching surface charge polarity.Thus,we only achieve a successfulfit of zeta-potential measurements when Na+ is considered in the SCM reactions.Finally,contact angleestimation using the PS model and disjoining pressure theory provide good predictions of seven differentcases reported in the literature.We validate our method on a total of 66 and 163 contact angle and zeta-potential measurements,respectively.The present work is a novel approach to represent how electrostaticinteractions among rock,brine and oil modify the rock surface charge and the rock wetting state.
机译:若干实验室实验表明,不同的水组合物导致岩石变为从水湿的状态变化。虽然它是一种共识,即润湿性改变是主要的恢复机制,建模潜在机制仍然是一个重大挑战。我们的主要目标是改善基于辅助的模型以预测来自Zeta-电位测量的接触角。我们提出了一种用于表面络合模型(SCM)的新母动作制剂,其包括两个接近表面(PS)的能量相互作用反应.C,大多数SCM考虑岩石和油作为孤立的表面(是).thus,我们假设,随着岩石和油表面彼此接近,PS模型产生更好的静电分布的描述。加法,我们开发了一种确定SCM平衡康斯特托适合不同Zeta电位测量的方法离子浓度(Na +,Ca2 +,Mg2 +,SO42-ANDH +)。最后,我们使用Disjoining压力计算来估计接触角ND比较他们在文献中报告的阳台。从文献中提供的SCM一组反应,我们验证了对Phreeqc的模型(用于地球化学反应的参考模拟器)。对于PS案例,方程式的系统非常接近当曲面中的相互作用(表面之间的宽间距)进行接近。抛弃Zeta - 盐水系统的潜在预测,我们认为Na +可能不是先前所提出的漠不关心的离子。我们的仿真结果表明,除了着名的潜力 - 确定离子,在方解石上吸附可以在静电相互作用中发挥重要侵蚀性,切换表面电荷极性。如果在SCM反应中考虑Na +时,我们只能达到Zeta-电位测量的成功措施。最后,使用PS模型接触触角敏感度和Disjoining的压力理论提供了在文献中报告的七种差异化的良好预测。我们验证了我们的方法o n共66和163个接触角和ζ电位测量。目前的作品是一种新的方法,代表岩石,盐水和油改性岩石表面电荷和岩石润湿状态的静电互补性。

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