CAS Key Lab of Colloid, Interface and Chemical Thermodynamics, Institute of Chemistry, Chinese Academy of Sciences, Beijing 100190, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Molecules. 2020 Mar 8;25(5):1214. doi: 10.3390/molecules25051214.
The hydraulic fracturing technique remains essential to unlock fossil fuel from shale oil reservoirs. However, water imbibed by shale during hydraulic fracturing triggers environmental and technical challenges due to the low flowback water recovery. While it appears that the imbibition of fracturing fluid is a complex function of physico-chemical processes in particular capillary force which is associated with wettability of oil-brine-shale, the controlling factor(s) to govern the wettability is incomplete and the literature data in this context is missing. We thus measured the adsorption/desorption of asphaltenes on silica surface in the presence of brines using quartz crystal microbalance with dissipation (QCM-D). We detected zeta potential of asphaltene-brine and brine-silica systems and calculated the disjoining pressures of the asphaltene-brine-silica system in the case of different salinity. Moreover, we performed a geochemical study to quantify the variation of surface chemical species at asphaltene and silica surfaces with different pH values and used the chemical force microscope (CFM) method to quantify the effect of pH on intermolecular forces. Our results show that lowering salinity or raising pH reduced the adhesion force between asphaltene and silica surface. For example, at a pH value of 6.5, when the concentration of injected water is reduced from 1000 mM to 100 mM and 10 mM, the adhesion force decreased by approximately 58% and 66%, respectively. In addition, for the 100 mM NaCl solution, when the pH value increased from 4.5 to 6.5 and 9, the adhesion force decreased by approximately 56% and 87%, respectively. Decreased adhesion forces between asphaltene and the silica surface could promote the desorption of asphaltene from the silica surface, resulting in a negative zeta potential for both asphaltene-silica and brine-silica interfaces and a shift of wettability towards water-wet characteristic. During such a process, -NH number at asphaltene surfaces decreases and the bonds between -NH and >SiO break down, to further interpret the formation of a thinner asphaltene adlayer on the rock surface. This study proposes a reliable theoretical basis for the application of hydraulic fracturing technology, and a facile and possible manipulation strategy to increase flowback water from unconventional reservoirs.
水力压裂技术对于从页岩油藏中开采化石燃料仍然至关重要。然而,由于回注水回收率低,页岩在水力压裂过程中吸收的水会引发环境和技术挑战。尽管看来,压裂液的吸入是一个复杂的物理化学过程的函数,特别是与油-盐水-页岩润湿性相关的毛细力,但控制润湿性的因素并不完整,而且这方面的文献数据也缺失。因此,我们使用石英晶体微天平(QCM-D)在盐水存在的情况下测量了沥青质在二氧化硅表面上的吸附/解吸。我们检测了沥青质-盐水和盐水-二氧化硅系统的动电电势,并计算了不同盐度下沥青质-盐水-二氧化硅系统的非平衡压力。此外,我们进行了地球化学研究,以量化不同 pH 值下沥青质和二氧化硅表面上表面化学物质的变化,并使用化学力显微镜(CFM)方法量化 pH 值对分子间力的影响。我们的结果表明,降低盐度或提高 pH 值会降低沥青质和二氧化硅表面之间的粘附力。例如,在 pH 值为 6.5 时,当注入水的浓度从 1000 mM 降低到 100 mM 和 10 mM 时,粘附力分别降低了约 58%和 66%。此外,对于 100 mM NaCl 溶液,当 pH 值从 4.5 增加到 6.5 和 9 时,粘附力分别降低了约 56%和 87%。沥青质和二氧化硅表面之间的粘附力降低会促进沥青质从二氧化硅表面解吸,导致沥青质-二氧化硅和盐水-二氧化硅界面的负动电电势以及润湿性向水湿特征转变。在此过程中,沥青质表面上的-NH 数量减少,-NH 和>SiO 之间的键断裂,进一步解释了在岩石表面形成更薄的沥青质吸附层。这项研究为水力压裂技术的应用提供了可靠的理论基础,并提出了一种简单可行的策略来增加非常规储层的回注水。