Uncovering the Mechanisms of Low-Salinity Water Injection EOR Processes: A Molecular Simulation Viewpoint

E. F. Martins, G. A. D. Silva, M. A. Salvador, Alvaro David Torrez Baptista, J. M. D. Almeida, C. R. Miranda
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引用次数: 1

Abstract

In this work, we present a multiscale approach based on first-principles calculations and classical molecular dynamics methods, to investigate the enhanced oil recovery via low-salinity water injection (EOR-LSWI). Salting-in effect, wettability, pH alteration, electrical double layer and the main geochemical reactions involved in the multicomponent ionic exchanges mechanism were analyzed in order to understand their contribution, also to provide an overall phenomenological perspective of the involved phenomena with a proposed feedback control system. The first-principles calculations were based on density functional theory, carry out in the Quantum-ESPRESSO package, to determine the adsorption energies of hydrocarbons (propionic and pentanoic acids and phenol) on calcite (CaCO3) {10.4} surface. In addition, we have obtained the free energy variations for the minerals dissolution processes. The solvent effect was taken into account for the geochemical reactions through a continuum dielectric. The interface between calcite and API brine was investigated through steered classical molecular dynamics, as implemented in the LAMMPs code to evaluate the brine ions adsorption/desorption on calcite surface and characterize the electrostatic environment in the vicinity of the calcite-brine-oil interfaces. Our results showed that the adsorption energies for the deprotonated molecules were lower than the ones for the neutral cases, highlighting the pH effect in the desorption processes. The pH also played a role in the calcite dissolution, since the free energy variation (ΔG) of the dissolution process mediated by H3O+ was lower than the ΔG for the neutral pH process. We found the lowest dissolution ΔG for the MgSO4 mineral (bulk), indicating that Mg2+ and SO42- ions would be abundant in the solution. In contrast, the other minerals exhibit a positive ΔG. Ions adsorption/desorption on calcite are isoergic and suggest an equilibrium between Ca2+ and CO32- ions. In contrast, the Na+ and Cl- ions adsorption were not found to be a spontaneous process. Moreover, the potential of mean force profile for Ca2+ and CO32- ions showed a layered structuring, which indicates that the ion hydration energy is related to the adsorption/desorption process. Such results may contribute to cause-effect understanding of correlations among the mechanisms in EOR-LSWI and help to propose an optimal brine composition to maximize the oil recovery.
从分子模拟的角度揭示低矿化度注水提高采收率机理
在这项工作中,我们提出了一种基于第一性原理计算和经典分子动力学方法的多尺度方法,来研究低矿化度注水(EOR-LSWI)提高采收率的方法。分析了盐化效应、润湿性、pH变化、电双层以及多组分离子交换机制中涉及的主要地球化学反应,以了解它们的贡献,并提出了一种反馈控制系统,从整体现象学角度对涉及的现象进行了分析。第一性原理计算基于密度泛函理论,在Quantum-ESPRESSO包中进行,以确定碳氢化合物(丙酸、戊酸和苯酚)在方解石(CaCO3){10.4}表面的吸附能。此外,我们还得到了矿物溶解过程的自由能变化。通过连续介质进行地球化学反应时考虑了溶剂效应。通过LAMMPs程序中的定向经典分子动力学研究方解石和API卤水界面,以评估方解石表面卤水离子的吸附/解吸,并表征方解石-卤水-油界面附近的静电环境。结果表明,脱质子分子的吸附能低于中性分子的吸附能,说明脱质子过程中pH值的影响。pH对方解石的溶解也有影响,因为h30 +介导的溶解过程的自由能变化(ΔG)小于中性pH过程的ΔG。我们发现MgSO4矿物(散装)的溶解度最低ΔG,表明溶液中Mg2+和SO42-离子丰富。相比之下,其他矿物表现出积极的ΔG。离子在方解石上的吸附/解吸是等能的,表明Ca2+和CO32-离子之间存在平衡。相反,Na+和Cl-离子的吸附不是自发过程。Ca2+和CO32-离子的平均力谱电位呈层状结构,表明离子水合能与吸附/脱附过程有关。这些结果可能有助于理解EOR-LSWI机制之间的因果关系,并有助于提出最佳的盐水成分,以最大限度地提高石油采收率。
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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