Wettability Alteration of Kerogen by Interacting with Hydraulic Fracturing Fluid

X. Yi, K. Lee
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Abstract

The recent increase in unconventional oil and gas exploration and production has promoted active research on hydraulic fracturing, but the impact of interactions between fracturing fluid and kerogen on the alteration of kerogen wettability has not been well understood. The objective of this study is to experimentally estimate the changing wettability of kerogen with various thermal maturity levels by the interactions with hydraulic fracturing fluid. To achieve the objective, kerogen was isolated from a bulk rock of organic-rich shale with different types and maturities. Kerogen isolates was kept in a mix with synthetic hydraulic fracturing fluid under the temperature of 80 °C for 14 days. Relative changes of sulfate ions were analyzed by using Ion Chromatography (IC). In the measurement of kerogen wettability, sessile drop method was applied to measure the direct contact angle by utilizing the Drop Shape Analyzer (DSA). During the reaction with hydraulic fracturing fluid, kerogen isolates were analyzed by conducting functional group analysis, which provided the supplemental information on the wettability of kerogen. Functional groups of kerogen were analyzed by using the Attenuated Total Reflectance Fourier-Transform Infrared spectroscopy (ATR-FTIR). The reaction of fracturing fluid and kerogen isolates from various organic-rich shales were conducted, and it is experimentally demonstrated that the interactions between kerogen and fracturing fluid would cause substantial wettability alterations in organic pores and fractures that depend on the types and maturities of kerogen. The DSA results indicated that the air/water-contact angle decreases after the reaction, regardless of the types and maturities of kerogen, while the higher level of maturity of kerogen led to a greater change of air/water-contact angle. The results of ATR-FTIR showed that the hydrophobic functional groups were lost in the mature kerogen isolates, and they were potentially lost in the relatively lower level of maturity-kerogen isolates due to the oxidation, indicating that the kerogen showed increasing hydrophilicity, which provided a strong support to the DSA results. This study experimentally determined the wettability alteration of kerogen by interacting with organic additives in hydraulic fracturing fluid. The results of this investigation will provide a significant step forward in evaluating the multiphase fluid transport in organic-rich shales with the wettability alteration and resulting hydrocarbon production.
水力压裂液对干酪根润湿性的影响
近年来,非常规油气勘探和生产的增加促进了水力压裂研究的活跃,但压裂液与干酪根相互作用对干酪根润湿性变化的影响尚未得到很好的认识。本研究的目的是通过实验估计不同热成熟度水平下干酪根与水力压裂液相互作用的润湿性变化。为了实现这一目标,从不同类型和成熟度的富有机质页岩中分离出干酪根。分离干酪根与合成水力压裂液在80℃的温度下混合保存14天。用离子色谱法分析了硫酸盐离子的相对变化。在干酪根润湿性的测量中,采用液滴法,利用液滴形状分析仪(drop Shape Analyzer, DSA)测量直接接触角。在与水力压裂液反应过程中,通过官能团分析对干酪根分离物进行了分析,为干酪根润湿性提供了补充信息。利用衰减全反射傅里叶变换红外光谱(ATR-FTIR)对干酪根的官能团进行了分析。研究了不同富有机质页岩中压裂液与干酪根分离物的反应,实验表明,干酪根与压裂液的相互作用会导致有机质孔隙和裂缝的润湿性发生显著变化,这种变化取决于干酪根的类型和成熟度。DSA结果表明,无论干酪根类型和成熟度如何,反应后空气/水接触角减小,且干酪根成熟度越高,空气/水接触角变化越大。ATR-FTIR结果显示,成熟干酪根分离物中疏水官能团丢失,而在相对较低水平成熟干酪根分离物中,由于氧化作用,疏水官能团可能丢失,表明干酪根的亲水性增强,这为DSA结果提供了有力的支持。实验研究了水力压裂液中有机添加剂对干酪根润湿性的影响。该研究结果将为评价富有机质页岩的多相流体输运与润湿性变化及其油气产量提供重要的依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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