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Studies on the potential of inorganic carbon removal and carbon sequestration in seawater through Ca2+ addition |
LI Shuo-chen1,3, LI Xue-gang1,2,3,4, HE Zhi-peng5, SONG Jin-ming1,2,3,4, LIU Shan-shan1,2,4, WANG Zhi-bo1,3 |
1. Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; 2. Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; 3. University of Chinese Academy of Sciences, Beijing 100049, China; 4. Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China; 5. Shandong Fishery Development and Resource Conservation Station, Jinan 250011, China |
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Abstract This study explored the potential of introducing Ca2+ into seawater to remove dissolved inorganic carbon and enhance the oceanic carbon sink. Laboratory simulations under various initial conditions were conducted, by altering the initial pH of seawater, Mg/Ca ratio, and introducing seeding nuclei, monitor the changes in seawater pH, DIC, and TA regularly. Results indicated that the introduction of Ca2+ effectively reduced the magnesium-to-calcium ratio(5.2) in natural ocean and increased the oversaturation of calcium carbonate, thereby facilitating the removal of inorganic carbon from the marine system. Furthermore, the efficacy of inorganic carbon removal with calcium-containing compounds was positively correlated with the initial pH of seawater. However, solely elevating seawater pH was insufficient to induce calcium carbonate formation; additional Ca2+ introduction was necessary to enhance calcium carbonate oversaturation for significant inorganic carbon removal. Additionally, the study revealed that inducing non-homogeneous precipitation through the addition of specific nuclei further promotes calcium carbonate generation, thereby improving inorganic carbon removal from seawater.The research findings indicated that under the conditions of adding 45mmol/L of Ca2+ and montmorillonite nuclei, with an initial pH of 8.5, the maximum amount of calcium carbonate generated can reach 959 μmol/L. The removal of inorganic carbon from seawater, leading to the short-term absorption of atmospheric CO2and increased oceanic carbon sink, offers a novel perspective and theoretical foundation for exploring ocean carbon enhancement technologies.
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Received: 21 February 2024
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