The Impact of Re-Injecting Flowback Fluids on Formation Damage. Case Study: Marcellus Shale

Lifu Zhang, M. Tice, B. Hascakir
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引用次数: 2

Abstract

Reuse of flowback water in hydraulic fracturing is usually used by industry to reduce consumption, transportation and disposal cost of water. But because of complex interactions between injected water and reservoir rocks, induced fractures may be blocked by impurities carried by flowback and mineral precipitation by water-rock interactions, which causes formation damage. Therefore, knowledge of flowback water-rock interactions is important to understand the changes within the formation and effects on hydraulic fracturing performance. This study focuses on investigating flowback water-rock interactions during hydraulic fracturing in Marcellus Shale Formation. Simple deionized water-rock interactions and complicated flowback water-rock interactions were studied under static and dynamic conditions. In static experiments, crushed reservoir rock samples were exposed to water for three weeks at room condition. In the dynamic experiment, continuous water flow interacted with rock samples through the core-flooding experimental system for three hours at reservoir condition. Before and after experiments, rock samples were characterized to determine the change on the rock surfaces. Water samples were analyzed to estimate the particle precipitation tendency and potential to modify flow pathway. Surface elemental concentrations, mineralogy and SEM images of rock samples were characterized. Ion contents, particle size, TDS and Zeta potential in the water samples were analyzed. In both static and dynamic experiments, compared with deionized water-rock interaction, rock samples after being exposed to flowback water show change in the elemental compositions, more fine particles attachment and new minerals detected on rock surface due to effect of flowback water. In produced water, Na, Sr and Cl are extremely high after flowback water-rock interactions because of flowback water contamination. Water parameter analysis indicates after flowback water-rock interactions, suspensions in produced water have highest precipitation tendency because of extremely highest TDS, largest particle size and lowest absolute Zeta potential relative to all water samples. Therefore, according to rock and water characterization, if flowback water without any treatment would be reused in the field hydraulic fracturing operation, created flow pathways and pores are more likely to be blocked and formation damage will be caused. This study provides information on comparison between deionized water-rock interaction and flowback water interaction. The information enhances the understanding of basic water-rock interaction mechanisms and evaluates formation damage caused by reuse of flowback water.
回注返排液对地层损害的影响案例研究:Marcellus页岩
水力压裂返排水的回用通常被工业用于降低水的消耗、运输和处理成本。但由于注入水与储层岩石之间复杂的相互作用,可能会被返排携带的杂质和水岩相互作用产生的矿物沉淀堵塞裂缝,造成地层损害。因此,了解反排水岩相互作用对于了解地层内部变化及其对水力压裂性能的影响非常重要。本研究的重点是研究Marcellus页岩地层水力压裂过程中的反排水岩相互作用。在静态和动态条件下研究了简单去离子化水岩相互作用和复杂反排水岩相互作用。在静态实验中,将破碎的储层岩石样品在室温条件下暴露于水中三周。在动态实验中,在油藏条件下,连续水流通过岩心驱替实验系统与岩样相互作用3小时。实验前后,对岩石样品进行表征,以确定岩石表面的变化。对水样进行了分析,以估计颗粒的沉淀趋势和改变水流路径的潜力。对岩石样品的表面元素浓度、矿物学和SEM图像进行了表征。对水样中的离子含量、粒径、TDS和Zeta电位进行了分析。在静态和动态实验中,与去离子化的水-岩相互作用相比,受返排水的影响,岩石样品的元素组成发生了变化,岩石表面有更多的细颗粒附着,并且在岩石表面检测到新的矿物。在采出水中,由于返排水污染,返排水-岩相互作用后,Na、Sr、Cl含量极高。水参数分析表明,反排水岩相互作用后,采出水中悬浮液的沉淀倾向最高,因为相对于所有水样,TDS极高,粒径最大,Zeta电位最低。因此,根据岩石和水的特征,如果未经处理的返排水在现场水力压裂作业中重复使用,则更容易堵塞流动通道和孔隙,造成地层损害。本研究提供了去离子水-岩相互作用和返排水相互作用的比较资料。这些信息增强了对水岩相互作用基本机制的认识,并可用于评价返排水回用对地层造成的损害。
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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