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首页> 外文期刊>Journal of Colloid and Interface Science >2+, CO3 2?, Mg2+, SO4 2?) for characterizing carbonate wettability]]>
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2+, CO3 2?, Mg2+, SO4 2?) for characterizing carbonate wettability]]>

机译: 2?,mg 2 + ,因此 4 <什么:SIMP PLACE =“POST”> 2?)用于表征碳酸盐润湿性]]]>

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Graphical abstract Display Omitted Abstract This study presents experiment and surface complexation modeling (SCM) of synthetic calcite zeta potential in brine with mixed potential determining ions (PDI) under various CO2 partial pressures. Such SCM, based on systematic zeta potential measurement in mixed brines (Mg2+, SO4 2?, Ca2+ and CO3 2?), is currently not available in the literature and is expected to facilitate understanding of the role of electrostatic forces in calcite wettability alteration. We first use a double layer SCM to model experimental zeta potential measurements and then systematically analyze the contribution of charged surface species. Calcite surface charge is investigated as a function of four PDIs and CO2 partial pressure. We show that our model can accurately predict calcite zeta potential in brine containing a combination of four PDIs and apply it to predict zeta potential in ultra-low and pressurized CO2 environments for potential application in enhanced oil recovery in carbonate reservoirs. Model prediction reveals that calcite surface will be positively charged in all considered brines in pressurized CO2 environment (1atm). The calcite zeta potential is sensitive to CO2 partial pressure in the various brine in the order of Na2CO3 Na2SO4 NaClMgCl2 CaCl2 (Ionic strength=0.1M). ]]>
机译:<![cdata [ 图形摘要 显示省略 抽象 本研究介绍了盐水中的合成方解石Zeta潜力的实验和表面络合建模(SCM)在各种CO 2 部分压力。这种SCM,基于混合盐水的系统Zeta电位测量(Mg 2 + ,因此 4 2> 2?,ca 2 + 和co 3 2?),目前无法在文献中提供,预计会促进理解静电力在方解石润湿性中的作用改造。我们首先使用双层SCM来模拟实验性Zeta电位测量,然后系统地分析带电表面物种的贡献。通过四种PDIS和CO 部分压力,研究了方解石表面电荷。我们表明我们的模型可以准确地预测包含四个PDI组合的盐水中的方解石Zeta电位,并将其应用于超低和加压CO中的Zeta电位 2 碳酸盐储层增强利油潜在应用的环境。模型预测揭示了方解石表面在加压Co 环境(& 1 atm)。方解石Zeta电位对CO 2 在NA 2 CO 3 NA 2 so 4 NaCl MGCL 2 cacl 2 (离子强度 = 0.1 m)。 ]]>

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