Measurement and modeling of CO2 diffusion coefficient in Saline Aquifer at reservoir conditions

R. Azin, Mohamad Mahmoudy, S. M. J. Raad, S. Osfouri
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引用次数: 39

Abstract

Storage of CO2 in deep saline aquifers is a promising techniques to mitigate global warming and reduce greenhouse gases (GHG). Correct measurement of diffusivity is essential for predicting rate of transfer and cumulative amount of trapped gas. Little information is available on diffusion of GHG in saline aquifers. In this study, diffusivity of CO2 into a saline aquifer taken from oil field was measured and modeled. Equilibrium concentration of CO2 at gas-liquid interface was determined using Henry’s law. Experimental measurements were reported at temperature and pressure ranges of 32–50°C and 5900–6900 kPa, respectively. Results show that diffusivity of CO2 varies between 3.52–5.98×10−9 m2/s for 5900 kPa and 5.33–6.16×10−9 m2/s for 6900 kPa initial pressure. Also, it was found that both pressure and temperature have a positive impact on the measures of diffusion coefficient. Liquid swelling due to gas dissolution and variations in gas compressibility factor as a result of pressure decay was found negligible. Measured diffusivities were used model the physical model and develop concentration profile of dissolved gas in the liquid phase. Results of this study provide unique measures of CO2 diffusion coefficient in saline aquifer at high pressure and temperature conditions, which can be applied in full-field studies of carbon capture and sequestration projects.
水库条件下含盐含水层CO2扩散系数的测量与模拟
在深层咸水层中储存二氧化碳是一种很有前途的缓解全球变暖和减少温室气体(GHG)的技术。正确测量扩散系数对于预测传递速率和累计圈闭气量至关重要。关于温室气体在含盐含水层中的扩散的资料很少。本文对油田含盐含水层中CO2的扩散系数进行了测量和模拟。用亨利定律确定了气液界面处CO2的平衡浓度。实验测量分别在32-50°C和5900-6900 kPa的温度和压力范围内进行。结果表明,当初始压力为5900 kPa时,CO2的扩散系数为3.52-5.98×10−9 m2/s;当初始压力为6900 kPa时,CO2的扩散系数为5.33-6.16×10−9 m2/s。同时发现压力和温度对扩散系数的测量都有正向影响。气体溶解引起的液体膨胀和压力衰减引起的气体压缩系数变化可以忽略不计。利用测量的扩散系数建立物理模型,建立液相中溶解气体的浓度分布图。本研究结果提供了高压和高温条件下咸水含水层CO2扩散系数的独特测量方法,可用于碳捕获与封存项目的现场研究。
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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