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作 者:Dong Liu Rongda Yu Peng Yuan
机构地区:[1]CAS Key Laboratory of Mineralogy and Metallogeny/Guangdong Provincial Key Laboratory of Mineral Physics and Materials,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,CAS Center for Excellence in Deep Earth Science,Guangzhou 510640,China [2]University of Chinese Academy of Sciences,Beijing 100049,China [3]Guangdong Provincial Key Laboratory of Integrated Agro-environmental Pollution Control and Management,Institute of Eco-environmental and Soil Sciences,Guangdong Academy of Sciences,Guangzhou 510650,China [4]School of Environmental Science and Engineering,Guangdong University of Technology,Guangzhou 510006,China
出 处:《Ocean-Land-Atmosphere Research》2024年第1期319-321,共3页海洋-陆地-大气研究(英文)
基 金:supported by the National Natural Science Foundation of China(grant nos.42188102,42172047,and 41772041);the Guangdong Basic and Applied Basic Research Foundation(2022A1515010824);the Science and Technology Planning Project of Guangdong Province,China(2023B1212060048 and 2023B1212060044);the State Key Laboratory of Marine Geology,Tongji University(no.MGK202203).This is contribution No.IS-3436 from GIGCAS.
摘 要:To keep global warming below 1.5℃ and address the threats posed by global climate change,various geoengineering strate-gies based on increasing negative carbon emissions in oceans have been proposed,as the ocean is considered to be the largest reservoir of carbon[1,2].The dissolution of silicate minerals,such as olivine,is a promising engineering strategy that not only depletes carbon dioxide(CO_(2))but also reduces ocean acidification.
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