Permeability shifts in chalk core during produced water reinjection

Maksim Kurbasov, Karen L. Feilberg
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Abstract

Chalk reservoirs, due to their high porosity and very low permeability, represent one of the most interesting cases for engineering studies of carbonates. They exhibit complex fluid-rock interactions because of their reactive surfaces and dense porous medium. The reinjection of produced water is an attractive strategy for managing wastewater flow from oil wells. However, the complex composition of produced water, the reactive nature of carbonate rocks, and their low permeability create challenges related to permeability loss.
This study examines the stages of permeability change during core flooding experiments up to the point of complete clogging. A distinctive feature of this study is the presence of residual oil in the core samples, which simulates real reservoir conditions during produced water reinjection. The presence of residual oil is an additional factor influencing the change in core permeability, but there is no clear consensus in the research community on its impact on permeability during produced water injection.
All experiments were conducted in a core flooding system simulating well conditions in terms of pressure (170 bar) and temperature (70 °C). Produced water samples from the Dan field were used to replicate the chemical and thermodynamic processes occurring in a real well. The experiments identified three stages of permeability change: an initial increase in permeability (+12%), a period of pressure stabilization, and a subsequent decrease in permeability (−8%) due to the formation of inorganic precipitates within the core channels.
The primary objective of the experiments is to investigate the relationship between permeability changes and the stages of reinjection, with a focus on the effects of residual oil. The study focuses on identifying the processes occurring up to the point of complete clogging, considering the impact of residual oil saturation in the chalk core samples. Image analysis using scanning electron microscopy, particle size measurement with a zeta-potential meter, and thermodynamic scale formation modeling with ScaleCERE software were employed to explain these processes.
Three stages of permeability change were identified during the injection of 200 pore volumes of produced water: increased permeability (+12%), pressure stabilization, and decreased permeability (−8%). The positive influence of residual oil saturation on the filtration and storage properties of the reservoir was established, due to the mobilization of chalk core particles. Additionally, the theory of core channel clogging during the reinjection of formation water by the formation of inorganic precipitates within the channels was confirmed.
Understanding the causes of permeability reduction that occurred during the stage of permeability decrease enables the development of water purification methods specifically targeted at the causes of rock clogging. Predicting the process of injecting a mixture of produced and seawater will help in interpreting the data during disposal operations by injecting formation water into an injection well, and it will allow for the selection of effective measures to mitigate the impact on the reservoir.
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白垩岩芯在采出水回注过程中的渗透性变化
白垩储层具有高孔隙度和极低的渗透率,是碳酸盐岩工程研究中最有趣的案例之一。由于白垩岩具有活性表面和致密的多孔介质,它们表现出复杂的流体-岩石相互作用。回注采出水是管理油井废水流的一种有吸引力的策略。然而,采出水的复杂成分、碳酸盐岩的反应性及其低渗透率给渗透率损失带来了挑战。本研究考察了岩心充水实验过程中渗透率变化的各个阶段,直至完全堵塞。本研究的一个显著特点是岩心样本中存在残余油,这模拟了采出水回注过程中的真实储层条件。残余油的存在是影响岩心渗透率变化的另一个因素,但研究界对残余油在采出水注入过程中对渗透率的影响还没有达成明确的共识。丹油田的采出水样本被用来复制真实油井中发生的化学和热力学过程。实验确定了渗透率变化的三个阶段:渗透率最初增加(+12%)、压力稳定期以及随后由于岩心通道内无机沉淀物的形成而导致的渗透率下降(-8%)。考虑到白垩岩芯样本中残余油饱和度的影响,研究重点是确定直至完全堵塞前的过程。为解释这些过程,采用了扫描电子显微镜进行图像分析,使用 zeta 电位计测量颗粒大小,并使用 ScaleCERE 软件进行热力学尺度地层建模。在注入 200 孔隙体积的采出水期间,确定了渗透率变化的三个阶段:渗透率增加(+12%)、压力稳定和渗透率降低(-8%)。由于白垩岩芯颗粒的移动,确定了剩余油饱和度对储层过滤和储存特性的积极影响。此外,岩心通道内无机沉淀物的形成也证实了地层水回注过程中岩心通道堵塞的理论。了解渗透率下降阶段渗透率降低的原因,就能开发出专门针对岩石堵塞原因的净水方法。预测注入采出水和海水混合物的过程将有助于在向注水井注入地层水的处理作业中解释数据,并有助于选择有效措施以减轻对储层的影响。
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