Measurement of CO2 Diffusivity for Carbon Sequestration: A Microfluidic Approach for Reservoir-Specific Analysis

Predicting carbon dioxide (CO2) security and capacity in sequestration requires knowledge of CO2 diffusion into reservoir fluids. In this paper we demonstrate a microfluidic based approach to measuring the mutual diffusion coefficient of carbon dioxide in water and brine. The approach enables formation of fresh CO2?liquid interfaces; the resulting diffusion is quantified by imaging fluorescence quenching of a pH-dependent dye, and subsequent analyses. This method was applied to study the effects of site-specific variables?CO2 pressure and salinity levels?on the diffusion coefficient. In contrast to established, macro-scale pressure?volume?temperature cell methods that require large sample volumes and testing periods of hours/days, this approach requires only microliters of sample, provides results within minutes, and isolates diffusive mass transport from convective effects. The measured diffusion coefficient of CO2 in water was constant (1.86 [±0.26] ? 10?9 m2/s) over the range of pressures (5?50 bar) tested at 26 °C, in agreement with existing models. The effects of salinity were measured with solutions of 0?5 M NaCl, where the diffusion coefficient varied up to 3 times. These experimental data support existing theory and demonstrate the applicability of this method for reservoir-specific testing. Predicting carbon dioxide (CO2) security and capacity in sequestration requires knowledge of CO2 diffusion into reservoir fluids. In this paper we demonstrate a microfluidic based approach to measuring the mutual diffusion coefficient of carbon dioxide in water and brine. The approach enables formation of fresh CO2?liquid interfaces; the resulting diffusion is quantified by imaging fluorescence quenching of a pH-dependent dye, and subsequent analyses. This method was applied to study the effects of site-specific variables?CO2 pressure and salinity levels?on the diffusion coefficient. In contrast to established, macro-scale pressure?volume?temperature cell methods that require large sample volumes and testing periods of hours/days, this approach requires only microliters of sample, provides results within minutes, and isolates diffusive mass transport from convective effects. The measured diffusion coefficient of CO2 in water was constant (1.86 [±0.26] ? 10?9 m2/s) over the range of pressures (5?50 bar) tested at 26 °C, in agreement with existing models. The effects of salinity were measured with solutions of 0?5 M NaCl, where the diffusion coefficient varied up to 3 times. These experimental data support existing theory and demonstrate the applicability of this method for reservoir-specific testing.