岩心驱油与数学建模相结合的调盐水驱机理研究

M. Taheri, M. Bonto, A. Eftekhari, H. Nick
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引用次数: 3

摘要

我们的目标是找到一种替代方法来匹配二次和三次模式下的改良含盐量水驱试验的历史。我们不只是匹配采收率和压降历史,而是更优先考虑匹配不同的离子浓度和石油突破时间。在此基础上,提出了碳酸盐岩改矿化度水驱的主要机理。研究工作分三步进行:1)研究大量碳酸盐油藏改盐水驱实验数据集。2)利用优化的内部表面络合模型量化电位决定离子(pdi)在碳酸盐表面的吸附3)结合现代基于搜索的优化算法,使用不同的水驱分析溶液(有和没有离子吸附)调整相对渗透率参数,使其与实验数据历史匹配。该优化算法对油品的突破时间和pdi给予了较高的权重系数。相对渗透率的参数太多(Brooks-Corey型有6个参数),可以匹配任何类型的采收率曲线。然而,我们发现,匹配突破时间,特别是在三级改性矿化度水驱中,只能考虑由于pdi在碳酸盐表面吸附而引起的润湿性变化。这一观察结果,结合我们精确模拟pdi在碳酸盐表面吸附的能力,帮助我们确定了导致碳酸盐润湿性变化的重要pdi。例如,我们观察到,考虑钙离子在白垩表面吸附引起的润湿性变化的模型与Stevns Klint露头白垩的第三纪海水驱完全匹配。第二个重要的观察结果是,开始注入改盐盐水和原油突破时间之间的滞后并不总是由于离子的吸附,有时可以用注入盐水盐度较低导致的润湿性变化来解释。必须指出,这种新方法仍然是半经验的,需要与更基本的研究相结合,以确定实际机制。
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Towards Identifying the Mechanisms of the Modified-Salinity Waterflooding by a Novel Combination of Core flooding and Mathematical Modeling
Our objective is to find an alternative approach to the history matching of the modified salinity water flooding tests in secondary and tertiary mode. Instead of matching only the recovery factor and pressure drop history, we give a higher priority to matching the different ion concentrations and oil breakthrough times. Based on these analyses, we suggest the predominant mechanisms for the modified-salinity water flooding in carbonates. The work is done in three steps: 1) Studying a large data-set of modified-salinity water flooding experiments in carbonates. 2) Quantifying the adsorption of potential determining ions (PDIs) on the carbonate surface using an optimized in-house surface-complexation model 3) Adjusting the relative permeability parameters to history-match the experimental data using different analytical solution of water-flooding (with and without ionic adsorption) combined with modern search-based optimization algorithms. The optimization algorithm gives a high weight factor to the breakthrough time of oil and PDIs. Having too many parameters in the relative permeability (6 parameters for Brooks-Corey type) make it possible to match any type of recovery curves. However, we found out that matching the breakthrough times, especially in the tertiary modified salinity waterflooding, can only be achieved by considering the wettability change due to the adsorption of PDIs on the carbonate surface. This observation, combined with our ability to accurately model the adsorption of PDIs on the carbonate surface, helped us to identify the important PDIs that cause the wettability change in carbonates. For instance, we observe that a model that considers the wettability change due to the adsorption of calcium ions on the chalks surface matches perfectly to the tertiary flooding of the Stevns Klint outcrop chalk with seawater. The second important observation is that the lag between the start of the injection of the modified-salinity brine and the oil breakthrough time is not always due to the adsorption of ions and sometimes can be explained by the wettability change due to the lower salinity of the injected brine. It must be noted that this new approach is still semi-empirical, and needs to be combined with more fundamental studies to identify the actual mechanisms.
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