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Wettability of supercritical carbon dioxide/water/quartz systems: Simultaneous measurement of contact angle and interfacial tension at reservoir conditions

机译:超临界二氧化碳/水/石英系统的润湿性:在储层条件下同时测量接触角和界面张力

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Injection of carbon dioxide in deep saline aquifers is considered as a method of carbon sequestration. The efficiency of this process is dependent on the fluid-fluid and rock-fluid interactions inside the porous media. For instance, the final storage capacity and total amount of capillary-trapped CO_2 inside an aquifer are affected by the interfacial tension between the fluids and the contact angle between the fluids and the rock mineral surface. A thorough study of these parameters and their variations with temperature and pressure will provide a better understanding of the carbon sequestration process and thus improve predictions of the sequestration efficiency. In this study, the controversial concept of wettability alteration of quartz surfaces in the presence of supercritical carbon dioxide (sc-CO_2) was investigated. A novel apparatus for measuring interfacial tension and contact angle at high temperatures and pressures based on Axisymmetric Drop Shape Analysis with no-Apex (ADSA-NA) method was developed and validated with a simple system. Densities, interfacial tensions, and dynamic contact angles of CO_2/water/quartz systems were determined for a wide range of pressures and temperatures relevant to geological sequestration of CO_2 in the subcritical and supercritical states. Image analysis was performed with ADSA-NA method that allows the determination of both interfacial tensions and contact angles with high accuracy. The results show that supercritical CO_2 alters the wettability of quartz surface toward less water-wet conditions compared to subcritical CO_2. Also we observed an increase in the water advancing contact angles with increasing temperature indicating less water-wet quartz surfaces at higher temperatures.
机译:在深盐水层中注入二氧化碳被认为是固碳的一种方法。该过程的效率取决于多孔介质内部的流体-流体和岩石-流体相互作用。例如,含水层内部的最终存储容量和毛细管捕集的CO_2总量受流体之间的界面张力以及流体与岩石矿物表面之间的接触角的影响。对这些参数及其随温度和压力的变化进行透彻的研究将提供对碳固存过程的更好理解,从而改善对固存效率的预测。在这项研究中,研究了在超临界二氧化碳(sc-CO_2)存在下石英表面润湿性变化的争议概念。开发了一种基于无顶点轴对称液滴形状分析(ADSA-NA)方法的高温和高压下测量界面张力和接触角的新型设备,并通过一个简单的系统对其进行了验证。确定了与亚临界和超临界状态下的CO_2地质隔离有关的宽范围的压力和温度,确定了CO_2 /水/石英系统的密度,界面张力和动态接触角。使用ADSA-NA方法进行图像分析,该方法可以高精度确定界面张力和接触角。结果表明,与亚临界CO_2相比,超临界CO_2使石英表面的润湿性向更少的水湿条件变化。我们还观察到水前进接触角随温度升高而增加,这表明在较高温度下较少的水湿石英表面。

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