Karoussi O, Hamouda A A
Department of Petroleum Engineering, University of Stavanger, 4036 Stavanger, Norway.
J Colloid Interface Sci. 2008 Jan 1;317(1):26-34. doi: 10.1016/j.jcis.2007.09.045. Epub 2007 Sep 21.
Effect of Mg2+ and SO24 on wettability alteration of modified calcite surface to oil-wet by stearic acid (SA) is addressed both in macroscopic and nanoscale using contact angle and atomic force microscopy technique (AFM), respectively. No apparent difference is shown by AFM images, compared to a clear trend that is obtained form contact angle measurements, where Mg2+ ions have shown to alter the modified calcite surface to more water-wet than that in presence of SO24 ions. The adhesion forces, due to the presence of SA, are shown to be less pronounced in presence of Mg2+ ion than that in case of SO24. This confirms the macroscale measurements of contact angle by nanoscale level. The phenomenon of the alteration to more water-wet calcite surface is related to the distribution coefficient of SA in n-decane/water system, which decreased in presence of Mg2+ and SO24 ions, indicating less adsorption of SA on calcite surface.
分别使用接触角和原子力显微镜技术(AFM),从宏观和纳米尺度研究了Mg2+和SO42-对硬脂酸(SA)改性方解石表面油湿润湿性改变的影响。与接触角测量得到的明显趋势相比,AFM图像没有显示出明显差异,其中Mg2+离子已显示出比存在SO42-离子时能使改性方解石表面更亲水性。由于SA的存在,Mg2+离子存在时的粘附力比SO42-离子时不那么明显。这从纳米尺度证实了接触角的宏观测量。方解石表面更亲水性改变的现象与SA在正癸烷/水体系中的分配系数有关,在Mg2+和SO42-离子存在下该系数降低,表明SA在方解石表面的吸附减少。