CH4-CO2-H2O-NaCl 四元系统的 SAFT2 状态方程及其在枯竭气藏二氧化碳封存中的应用

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
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引用次数: 0

摘要

了解 CH4-CO2-H2O-NaCl 四元体系的相平衡和物理化学特征对于评估在枯竭天然气储层中封存二氧化碳的成本和风险以及流体包裹性研究非常重要。本研究利用基于统计关联流体理论(SAFT)的状态方程(EOS),在温度为 298 至 513 K(25-240 °C)、压力高达 600 bar(60 MPa)和氯化钠浓度高达 6 mol/kgH2O 的条件下,研究了该体系的相平衡和热力学性质。模型参数是通过拟合子系统(即 CH4-H2O、CH4-CO2 和 CH4-H2O-NaCl)的可用实验数据和子系统(即纯组分、CO2-H2O 和 CO2-H2O-NaCl)的可用参数获得的。利用本研究开发的 SAFT EOS,我们预测了(CH4 + CO2)气体混合物在纯 H2O 中的溶解度,并将其与现有实验数据和四种常用数值模拟器的预测值进行了比较。结果表明,我们的模型可以为 CH4-CO2-H2O 三元体系提供可靠的预测。随后,我们进一步预测了 NaCl 在 0 至 6 mol/kgH2O 范围内的 CH4-CO2-H2O-NaCl 体系的相平衡和密度。我们还利用 SAFT EOS 预测了 CO2 和 CH4 在 CO2- 提高采油的水-替代气过程中的溶解度,结果表明与通过 Peng-Robinson EOS 预测 CO2 和 CH4 溶解度的模拟结果非常吻合。这些预测的 CH4-CO2-H2O-NaCl 系统中的热力学性质和相行为为在枯竭油气藏中封存二氧化碳的意义提供了定量的启示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SAFT2 equation of state for the CH4–CO2–H2O–NaCl quaternary system with applications to CO2 storage in depleted gas reservoirs

Understanding the phase equilibria and physical-chemical characteristics of the CH4–CO2–H2O–NaCl quaternary system is important for evaluating costs and risks for the storage of CO2 in depleted natural gas reservoirs as well as fluid inclusion studies. In this study, phase equilibria and thermodynamic properties of this system were investigated through the utilization of a statistical association fluid theory-based (SAFT) equation of state (EOS) at temperatures from 298 to 513 K (25–240 °C), pressures up to 600 bar (60 MPa) and concentration of NaCl up to 6 mol/kgH2O. The model parameters were obtained from the fitting of available experimental data of subsystems (i.e., CH4–H2O, CH4–CO2, and CH4–H2O–NaCl) that were judged to be reliable and incorporation of available parameters for the subsystems (i.e., pure component, CO2–H2O, and CO2–H2O–NaCl). Using the SAFT EOS developed in this study, we predicted the solubility of (CH4 + CO2) gas mixtures in pure H2O and compared it with the available experimental data and the predicted values from four popular numerical simulators. The results indicate that our model can provide reliable predictions for the CH4–CO2–H2O ternary system. Subsequently, we further predicted the phase equilibria and density of the CH4–CO2–H2O–NaCl system with NaCl varying from 0 to 6 mol/kgH2O. We also employed the SAFT EOS to predict the solubility of CO2 and CH4 in the water-alternating-gas process for CO2-enhanced oil recovery, demonstrating good agreement with the simulation results obtained through the Peng-Robinson EOS for predicting the CO2 and CH4 solubility. These predicted thermodynamic properties and phase behaviors in the CH4–CO2–H2O–NaCl system provide quantitative insights into the implications of CO2 storage in depleted oil and gas reservoirs.

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来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
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