On the Prediction of Gas Solubility in Brine Solutions for Applications of CO2 Capture and Sequestration

Ram R. Ratnakar, A. Venkatraman, A. Kalra, B. Dindoruk
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引用次数: 4

Abstract

Geological storage of CO2 in deep saline aquifers has become a well-accepted method for CO2 sequestration. CO2-solubility in these brine solutions is one of the most important factors in determining the amount of CO2 sequestered in these aquifers. Since the type of salt can significantly alter the CO2-solubility in brine solutions, the impact of water chemistry on CO2 solubility is investigated in this work and results are compared against experimental observations. The current work for predicting solubility of a gas in brine solution containing various salts is based on the extension of well-known Setschenow relation that has been commonly used for salts with monovalent ions. In this research, we extend the Setschenow approach by expressing the solubility in terms of ionic strengths and molar concentrations of each salt. The method also characterizes each component (e.g., gas, anions and cations) against the experimental measurements. A simple methodology, developed with a theoretical framework, is presented to predict the impact of different types of salts on solubility of CO2. This approach can be extended to any type of gases or other solutes (e.g. CH4, H2S etc.) in brine solutions. In particular, The gas solubility in brines is expressed in terms of molar components and ionic strength of each salt. The expression contains unique/characteristic parameters for each component (gas, anions and cations). These parameters for anions and cations of typical formation water (present in oil/gas reservoirs) and CO2/novel solvents are obtained from literature or using regression on experimental data.Results of CO2-solubility were compared with published data in literature, demonstrating that the methodology (presented in the work) can predict the effect of water-chemistry on solubility predictions.The proposed method was tested for a novel solvent (dimethyl ether) and comparison with experimental solubility data show an excellent match between the predictions and measurements.
CO2捕集与封存应用中气体在盐水溶液中的溶解度预测
在深层含盐含水层中地质封存二氧化碳已成为一种被广泛接受的二氧化碳封存方法。二氧化碳在这些盐水溶液中的溶解度是决定这些含水层中封存的二氧化碳量的最重要因素之一。由于盐的类型可以显著改变CO2在盐水溶液中的溶解度,因此本工作研究了水化学对CO2溶解度的影响,并将结果与实验观察结果进行了比较。目前预测气体在含各种盐的盐水溶液中的溶解度的工作是基于众所周知的Setschenow关系的扩展,该关系通常用于具有一价离子的盐。在本研究中,我们扩展了Setschenow方法,用离子强度和每种盐的摩尔浓度来表示溶解度。该方法还根据实验测量来表征每种组分(例如,气体、阴离子和阳离子)。一个简单的方法,发展与理论框架,提出了预测不同类型的盐对CO2溶解度的影响。这种方法可以扩展到卤水溶液中的任何类型的气体或其他溶质(例如CH4, H2S等)。特别是,气体在盐水中的溶解度是用每种盐的摩尔组分和离子强度来表示的。该表达式包含每个组分(气体、阴离子和阳离子)的唯一/特征参数。这些典型地层水(存在于油气储层中)和CO2/新型溶剂的阴离子和阳离子参数是通过文献或对实验数据进行回归得到的。将co2溶解度的结果与文献中已发表的数据进行了比较,表明该方法(在工作中提出)可以预测水化学对溶解度预测的影响。在一种新型溶剂(二甲醚)中对该方法进行了测试,并与实验溶解度数据进行了比较,结果表明预测结果与测量结果吻合良好。
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