盐水化学对岩石-盐水界面低盐度聚合物粘弹性及地球化学相互作用的影响

IF 5.2 2区 化学 Q2 CHEMISTRY, PHYSICAL Journal of Molecular Liquids Pub Date : 2025-05-15 Epub Date: 2025-03-11 DOI:10.1016/j.molliq.2025.127372
Intisar K. Al-Busaidi , Rashid S. Al-Maamari , Mahvash Karimi , Dawoud Al Mahrouqi , Hassina Al Hinai
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引用次数: 0

摘要

近年来,大量研究评估了低矿化度聚合物(LSP)驱在砂岩油藏中的效果;然而,文献综述表明,卤水化学对聚合物粘弹性的影响,以及后续对LSP驱油性能的影响需要澄清。为了实现这一目标,需要考虑不同卤水化学下聚合物与岩石表面的地球化学相互作用及其对聚合物吸附和粘度损失的影响。因此,本研究旨在研究盐水化学对聚合物粘弹性的影响,以及与博伊西砂岩岩心的离子交换反应。采用了一种多维实验方法,包括对不同卤水化学性质的HPAM聚合物溶液进行频率扫描测量。此外,还对含Boise岩石的平衡盐水进行了IC和ICP分析。此外,进行了单相驱替实验,研究了聚合物的吸附和粘度损失,并使用IC和TOC对出水进行了分析。结果表明,低二价阳离子(Ca2+或Mg2+)浓度(2 mM)的聚合物溶液具有较长的弛豫时间(高达12 s−1),表明具有较高的弹性。然而,当阳离子浓度从4 mM增加到14 mM时,聚合物结构稳定,并且额外的Ca2+或Mg2+引起的弛豫时间变化较小(从1.33 s−1减少到0.56 s−1),因此粘弹性变化较小。此外,盐度对HPAM聚合物粘弹性的影响强于特定的盐水组成,盐浓度的电荷筛选效应是弛豫时间减少的主要驱动因素。同样,除了Ca2+和Mg2+不存在外,地层盐水的离子组成对Boise岩石在有或没有聚合物时的地球化学反应影响最小。此外,在驱油实验中发现,聚合物在盐水中的存在会影响离子交换反应、平衡过程,并延长稳定时间,这强调了在流体-岩石相互作用中考虑聚合物行为的重要性。此外,通过控制聚合物-岩石相互作用,补偿盐水的盐度(而非聚合物浓度)主要影响了吸附行为和注入能力。高矿化度聚合物(HSP) (5459 ppm)和高矿化度聚合物(LSP) (545.9 ppm)均表现出相似的20%的粘度降解,其中由于聚合物在HSP中的吸附和LSP中矿化度的变化,粘度恢复延迟,最终降解是由水化学中二价阳离子浓度的增加驱动的。这些发现强调了基于盐水化学优化聚合物配方的重要性,管理注入水的盐度和二价阳离子的存在,了解地球化学相互作用和流动动力学,以提高LSP的性能,减轻盐水-岩石相互作用造成的结垢和粘度损失等不利影响。
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Impact of brine chemistry on viscoelastic properties and geochemical interactions of low salinity polymer at rock-brine interfaces
Recently, numerous studies have evaluated the efficacy of low salinity polymer (LSP) flooding in sandstone oil reservoirs; however, literature review revealed that the effects of brine chemistry on polymer viscoelasticity, and the subsequent impact on LSP flooding performance need to be clarified. To achieve that, the geochemical interactions of polymer with the rock surface at different brine chemistries and their effects on polymer adsorption and viscosity loss need to be considered. Therefore, the present study aims to investigate the impact of brine chemistry on polymer viscoelasticity, and ion exchange reactions with Boise sandstone cores. A multidimensional experimental approach, including frequency sweep measurements of HPAM polymer solutions at various brine chemistries was employed. Additionally, IC and ICP analyses were conducted for equilibrated brine with Boise rock. Moreover, single-phase displacement experiments were performed to study polymer adsorption and viscosity loss, with effluent analysis carried out using IC and TOC. The results revealed that polymer solutions with low divalent cation (Ca2+ or Mg2+) concentrations (2 mM) exhibited longer relaxation times (up to 12 s−1), indicating higher elasticity. However, as the cation concentration increased from 4 mM to 14 mM, the polymer structure stabilized, and additional Ca2+ or Mg2+ caused a smaller change in relaxation time (decreasing from 1.33 s−1 to 0.56 s−1), and consequently, in viscoelasticity. Additionally, salinity had a stronger effect on HPAM polymer viscoelasticity than specific brine composition, with the charge-screening effect from salt concentration being the primary driver of relaxation time reduction. Similarly, the ionic composition of formation brine had minimal impact on the geochemical reactions of Boise rock with or without polymer, except when Ca2+ and Mg2+ were absent. Moreover, the presence of polymer in the brine was found to affect ion exchange reactions, equilibration processes, and extend the stabilization time during flooding experiments, emphasizing the importance of considering polymer behavior in fluid-rock interactions. Furthermore, the salinity of the makeup brine, rather than polymer concentration, primarily influenced adsorption behavior and injectivity by controlling polymer-rock interactions. Both high salinity polymer (HSP) (5459 ppm) and LSP (545.9 ppm) showed a similar 20 % of viscosity degradation, with delays in viscosity recovery due to polymer adsorption in HSP and salinity changes in LSP, and final degradation driven by increased divalent cation concentration in the water chemistry. These findings emphasize the importance of optimizing polymer formulations based on brine chemistry, managing the salinity of injection water and the presence of divalent cations, and understanding geochemical interactions and flow dynamics to enhance LSP performance and mitigate adverse effects such as scaling and viscosity loss due to brine-rock interactions.
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来源期刊
Journal of Molecular Liquids
Journal of Molecular Liquids 化学-物理:原子、分子和化学物理
CiteScore
10.30
自引率
16.70%
发文量
2597
审稿时长
78 days
期刊介绍: The journal includes papers in the following areas: – Simple organic liquids and mixtures – Ionic liquids – Surfactant solutions (including micelles and vesicles) and liquid interfaces – Colloidal solutions and nanoparticles – Thermotropic and lyotropic liquid crystals – Ferrofluids – Water, aqueous solutions and other hydrogen-bonded liquids – Lubricants, polymer solutions and melts – Molten metals and salts – Phase transitions and critical phenomena in liquids and confined fluids – Self assembly in complex liquids.– Biomolecules in solution The emphasis is on the molecular (or microscopic) understanding of particular liquids or liquid systems, especially concerning structure, dynamics and intermolecular forces. The experimental techniques used may include: – Conventional spectroscopy (mid-IR and far-IR, Raman, NMR, etc.) – Non-linear optics and time resolved spectroscopy (psec, fsec, asec, ISRS, etc.) – Light scattering (Rayleigh, Brillouin, PCS, etc.) – Dielectric relaxation – X-ray and neutron scattering and diffraction. Experimental studies, computer simulations (MD or MC) and analytical theory will be considered for publication; papers just reporting experimental results that do not contribute to the understanding of the fundamentals of molecular and ionic liquids will not be accepted. Only papers of a non-routine nature and advancing the field will be considered for publication.
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