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Effect of brine salinity on the geological sequestration of CO2 in a deep saline carbonate formation

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  • Ram Kumar
  • Scott Campbell
  • Eric Sonnenthal
  • Jeffrey Cunningham

Abstract

When supercritical CO2 is injected into a deep saline aquifer, the salinity of the brine can influence both the solubility of the injected CO2 in the brine and the subsequent aqueous geochemical reactions that occur. The objective of this study is to assess the effect of brine salinity on CO2 storage in deep saline carbonate formations. Specifically, the study aims to quantitatively assess the effect of brine salinity on (a) the amount of CO2 that can be sequestered in the aqueous phase, (b) the storage efficiency of the repository, (c) the change in pH of the residual brine after dissolution of CO2, and (d) changes in the mineralogy and porosity of the rock matrix that result from mineral dissolution and precipitation reactions induced by CO2 injection. Injection of CO2 into a model layered carbonate formation was simulated using the reactive‐transport code TOUGHREACT 3.3. The simulations consisted of 50 years of injection into a partially completed injection well, followed by 50 years of equilibration (no injection). Salinity of the brine was varied between 1% and 15% to determine the effects of salinity. Because the solubility of CO2 decreases as the salinity of the brine increases, an increase in brine salinity from 1% to 15% resulted in a 19% decrease in storage efficiency and a 25% decrease in the mass of CO2 dissolved in the aqueous phase. However, despite the strong effect of brine salinity on CO2 dissolution, there was almost no effect of salinity on the pH change in the residual brine: the chemical activity coefficient of the dissolved CO2 increases with brine salinity, counteracting the effects of decreased solubility. Consequently, brine salinity had little effect on mineral dissolution or precipitation, or on changes in formation porosity. The study therefore helps to choose sequestration sites depending upon the salinity of the brine: lower salinity results in more solubility trapping and better storage efficiency without noticeable differences in pH drop or mineral dissolution. © 2020 Society of Chemical Industry and John Wiley & Sons, Ltd.

Suggested Citation

  • Ram Kumar & Scott Campbell & Eric Sonnenthal & Jeffrey Cunningham, 2020. "Effect of brine salinity on the geological sequestration of CO2 in a deep saline carbonate formation," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 10(2), pages 296-312, April.
    • Handle: RePEc:wly:greenh:v:10:y:2020:i:2:p:296-312
    DOI: 10.1002/ghg.1960
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    References listed on IDEAS

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    1. Liwei Zhang & Robert M. Dilmore & Grant S. Bromhal, 2016. "Effect of outer boundary condition, reservoir size, and CO 2 effective permeability on pressure and CO 2 saturation predictions under carbon sequestration conditions," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 6(4), pages 546-560, August.
    2. Emad A. Al†Khdheeawi & Stephanie Vialle & Ahmed Barifcani & Mohammad Sarmadivaleh & Yihuai Zhang & Stefan Iglauer, 2018. "Impact of salinity on CO2 containment security in highly heterogeneous reservoirs," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 8(1), pages 93-105, February.
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    Cited by:

    1. Alsedik Abousif & David Wronkiewicz & Abdelmoniem Masoud, 2024. "Geochemical assessment of mineral sequestration of carbon dioxide in the midcontinent rift," Greenhouse Gases: Science and Technology, Blackwell Publishing, vol. 14(2), pages 295-318, April.

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