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1000 Titel
  • An assessment of ocean alkalinity enhancement using aqueous hydroxides: kinetics, efficiency, and precipitation thresholds
1000 Autor/in
  1. Ringham, Mallory C. |
  2. Hirtle, Nathan |
  3. Shaw, Cody |
  4. Lu, Xi |
  5. Herndon, Julian |
  6. Carter, Brendan R. |
  7. Eisaman, Matthew D. |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-08-09
1000 Erschienen in
1000 Quellenangabe
  • 21(15):3551-3570
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/bg-21-3551-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Ocean alkalinity enhancement (OAE) is a promising approach to marine carbon dioxide removal (mCDR) that leverages the large surface area and carbon storage capacity of the oceans to sequester atmospheric CO2 as dissolved bicarbonate (HCO3-). One OAE method involves the conversion of salt in seawater into aqueous alkalinity (NaOH), which is returned to the ocean. The resulting increase in seawater pH and alkalinity causes a shift in dissolved inorganic carbon (DIC) speciation toward carbonate and a decrease in the surface ocean pCO2. The shift in the pCO2 results in enhanced uptake of atmospheric CO2 by the seawater due to gas exchange. In this study, we systematically test the efficiency of CO2 uptake in seawater treated with NaOH at aquarium (15 L) and tank (6000 L) scales to establish operational boundaries for safety and efficiency in advance of scaling up to field experiments. CO2 equilibration occurred on the order of weeks to months, depending on circulation, air forcing, and air bubbling conditions within the test tanks. An increase of ∼0.7–0.9 mol DIC per mol added alkalinity (in the form of NaOH) was observed through analysis of seawater bottle samples and pH sensor data, consistent with the value expected given the values of the carbonate system equilibrium calculations for the range of salinities and temperatures tested. Mineral precipitation occurred when the bulk seawater pH exceeded 10.0 and Ωaragonite exceeded 30.0. This precipitation was dominated by Mg(OH)2 over hours to 1 d before shifting to CaCO3,aragonite precipitation. These data, combined with models of the dilution and advection of alkaline plumes, will allow the estimation of the amount of carbon dioxide removal expected from OAE pilot studies. Future experiments should better approximate field conditions including sediment interactions, biological activity, ocean circulation, air–sea gas exchange rates, and mixing zone dynamics. </jats:p>
1000 Liste der Beteiligten
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1000 Förderer
  1. Grantham Foundation for the Protection of the Environment |
  2. Brookhaven National Laboratory |
  3. Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington |
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    1000 Förderer Grantham Foundation for the Protection of the Environment |
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  2. 1000 joinedFunding-child
    1000 Förderer Brookhaven National Laboratory |
    1000 Förderprogramm -
    1000 Fördernummer -
  3. 1000 joinedFunding-child
    1000 Förderer Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington |
    1000 Förderprogramm -
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1000 Objektart article
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1000 Erstellt am 2024-10-02T18:40:30.236+0200
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1000 Zuletzt bearbeitet 2025-08-06T15:56:10.248+0200
1000 Objekt bearb. Wed Aug 06 15:56:10 CEST 2025
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