Processing math: 100%

  • Measuring Interfacial Tension between Brine and Carbon Dioxide in Geological CO2 Sequestration Conditions using Pendant Bubble Methods
  • Park, Gyuryeong;An, Hyejin;Kim, Seon-ok;Wang, Sookyun;
  • Department of Energy Resources Engineering, Pukyong National University;Department of Energy Resources Engineering, Pukyong National University;Department of Energy Resources Engineering, Pukyong National University;Department of Energy Resources Engineering, Pukyong National University;
  • 수적(垂滴)법을 이용한 이산화탄소 지중저장 조건에서의 염수-이산화탄소 간 계면장력 측정
  • 박규령;안혜진;김선옥;왕수균;
  • 부경대학교 에너지자원공학과;부경대학교 에너지자원공학과;부경대학교 에너지자원공학과;부경대학교 에너지자원공학과;
Abstract
This experimental study was aimed to estimate interfacial tension of brine-CO2 by using a pendant bubble method and image analysis. Measurements were performed for wide ranges of temperatures, pressures, and salinities covering reservoir conditions in Pohang basin, a possible candidate for CO2 storage operation in Korea. The profiles of CO2 bubbles in brine obtained from image analysis with the densities of brine and CO2 from previous studies were applied to Laplace-Young equation for calculating interfacial twnsion in brine-CO2 system. The experimental results reveals that the interfacial tension is significantly affected by reservoir conditions such as pressure, temperature and water salinity. For conditions of constant temperature and water salinity, the interfacial tension decreases as pressure increases for low pressures (P < Pc), and approaches to a constant value for high pressures. For conditions of constant pressure and water salinity, the interfacial tension increases as temperature increases for T < Tc, with an asymptotic trend towards a constant value for high temperatures. For conditions of constant pressure and temperature, the interfacial tension increases with increasing water salinity. The trends in changes of interfacial tension can be explained by the effects of the reservoir conditions on the density difference of brine and CO2, and the solubility of CO2 in brine. The information on interfacial tensions obtained from this research can be applied in predicting the migration and distribution of injecting and residual fluids in brine-CO2-rock systems in deep geological environments during geological CO2 sequestrations.

Keywords: CO2;Brine;Interfacial tension;Pendant bubble method;Geological CO2 sequestration;

References
  • 1. Aggelopoulos, C.A., Robin, M., Perfetti, E., and Vizika, O., 2010, CO2/CaCl2 solution interfacial tensions under CO2 geological storage conditions: influence of cation valence on interfacial tension, Adv. Water Resour., 33, 691-697.
  •  
  • 2. Aggelopoulos, C.A., Robin, M., and Vizika, O., 2011, Interfacial tension between CO2 and brine (NaCl + CaCl2) at elevated pressures and temperatures: The additive effect of different salts, Adv. Water Resour., 34, 505-511.
  •  
  • 3. Andreas, J.M., Hauser, E.A., and Tucker, W.B., 1938, Boundary tension by pendant drops, J. Phys. Chem., 42, 1001-1019.
  •  
  • 4. Akiba, H. and Ohmura, R., 2016, Surface tension between CO2 gas and tetra-n-butylammonium bromide aqueous solution, J. Chem. Thermodyn., 92, 72-75.
  •  
  • 5. Arashiro, E.A. and Demarquette, N.R., 1999, Use of the pendant drop method to measure interfacial tension between molten polymers, Mat. Res., 2(1), 23-32.
  •  
  • 6. Bachu and Bennion, 2009, Dependence of CO2-brine interfacial tension on aquifer pressure, temperature and water salinity, Energy Procedia, 1(1), 3157-3164.
  •  
  • 7. Chalbaud, C., Robin, M., Lombard, J.-M., Bertin, H., and Egerman, P., 2010, Brine/CO2 interfacial properties and effects on CO2 storage in deep saline aquifers, Oil Gas Sci. Technol., 65(4), 541-555.
  •  
  • 8. Chiquet, P., Broseta, D., and Thibeau, S., 2007, Wettability alteration of caprock minerals by carbon dioxide, Geofluids, 7, 112-122.
  •  
  • 9. Duana, Z. and Sun, R., 2003, An improved model calculating CO2 solubility in pure water and aqueous NaCl solutions from 273 to 533 K and from 0 to 2000 bar, Chem. Geol., 193, 257-271.
  •  
  • 10. Esponoza, D.N. and Santamarina, J.C., 2010, Water-CO2-mineral systems: Interfacial tension, contact angle, and diffusion-Implications to CO2 geological storage, Water Resour. Res., 46, W07537, doi:10.1029/2009WR008634.
  •  
  • 11. Grigull, U. and Schmidt, E., 1979, Properties of Water and Steam in Si-Units. Second Revised and Updated Printing, Springer-Verlag, Berlin, 190 p.
  •  
  • 12. IPCC (Intergovernmental Panel on Climate Change), 2005, Carbon dioxide capture and storage, Cambridge University Press, Cambridge, 431p.
  •  
  • 13. Li, X., Boek, E., Maitland, G.C., and Trusler, J.P.M., 2012, Interfacial tension of (Brines + CO2): (0.864 NaCl + 0.136 KCl) at temperatures between (298 and 448) K, pressures between (2 and 50) MPa, and total molalities of (1 to 5) molkg1. J. Chem. Eng. Data, 57(4), 1078-1088.
  •  
  • 14. Macleod, D.B., 1923, On a relation between surface tension and density, T. Faraday Soc., 19, 38-41.
  •  
  • 15. Misak, M.D., 1968, Equations for determining 1/H versus S values in computer calculations of interfacial tension by the pendent drop method, J. Colloid Interface Sci., 27(1), 141-142.
  •  
  • 16. Shah, V., Broseta, D., Mouronval, G., and Montel, F., 2008, Water/acid gas interfacial tensions and their impact on acid gas geological storage, Int. J. Greenh. Gas Con., 2, 594-604.
  •  
  • 17. Song, Y., Kim, H.C., and Lee, T.J., 2010, Geothermal development in Korea: Country Update 2005-2009, World Geothermal Congress 2010, Bali, Indonesia, April 25-29, 241 p.
  •  
  • 18. Wiebe, R., 1941, The binary system carbon dioxide-water under pressure, Chem. Rev. 29, 475-489.
  •  
  • 19. Yang, D., Tontiwachwuthikul, P., and Gu Y., 2005, Interfacial interactions between reservoir brine and CO2 at high pressure and elevated temperature, Energ. Fuel., 19, 216-223.
  •  

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