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Effect of individual ions on rock-brine-oil interactions: A microcalorimetric approach
Understanding the mechanisms behind the additional oil recovery by low salinity water flooding (LSWF) in carbonates has been difficult because of the complexity of the crude oil + brine + rock system. This study is an attempt to isolate fluid–fluid and rock-fluid interactions through Isothermal Titr...
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Published in: | Fuel (Guildford) 2021-04, Vol.290, p.119955, Article 119955 |
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creator | Cobos, Jacquelin E. Søgaard, Erik G. |
description | Understanding the mechanisms behind the additional oil recovery by low salinity water flooding (LSWF) in carbonates has been difficult because of the complexity of the crude oil + brine + rock system. This study is an attempt to isolate fluid–fluid and rock-fluid interactions through Isothermal Titration Calorimetry (ITC) to get a deeper understanding of the oil recovery process. The results from the fluid–fluid interactions pointed out that the observed endothermic response is determined by the formation of micro-dispersions, in which Mg2+ is more active than Ca2+. The incorporation of Ca2+, Mg2+, SO42- and HCO3- onto the chalk lattice effectively does not need energy from the surroundings to proceed. On the other hand, the incorporation of Mg2+ or Ca2+ into the calcite structure in the presence of SO42- is less energetically favorable due to pair creation. |
doi_str_mv | 10.1016/j.fuel.2020.119955 |
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subjects | Brines Calcite Calcium Calcium ions Calorimetry Carbonates Chalk Crude oil Flooding Fluid–fluid interactions Low salinity Magnesium Mixture of ions Oil Oil recovery Rock-fluid Rocks Single ions Titration Titration calorimetry |
title | Effect of individual ions on rock-brine-oil interactions: A microcalorimetric approach |
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