碱度
化学
海水
固碳
地球大气中的二氧化碳
无机碳总量
海洋酸化
二氧化碳
环境化学
碳纤维
固碳
碳酸盐
碳酸氢盐
环境科学
碳循环
二氧化碳去除
总有机碳
具有碳捕获和储存功能的生物能源
大气碳循环
海洋学
蓝炭
光合作用
溶解有机碳
碳捕获和储存(时间表)
自然(考古学)
海洋化学
作者
C. Lee,Adam V. Subhas,J. Kim,Kitack Lee
标识
DOI:10.1021/acs.chemrev.5c00433
摘要
The ocean, Earth's largest carbon reservoir, exerts a central role over atmospheric CO2 through its capacity to store carbon primarily as bicarbonate ions. Direct observations indicate that the global ocean has a net carbon uptake of 2.6-3.0 petagrams of carbon annually, representing nearly 30% of anthropogenic CO2 emissions. This review examines two principal domains of oceanic carbon cycling. The first concerns the natural uptake and storage of anthropogenic CO2, with emphasis on the response of the marine carbonate system and the spatial distribution of absorbed carbon. The second addresses emerging marine CO2 removal strategies, especially ocean alkalinity enhancement and macroalgae-based approaches. Ocean alkalinity enhancement aims to increase seawater buffering capacity to facilitate greater CO2 uptake, whereas macroalgae-based strategies rely on photosynthetic fixation and the subsequent storage of organic and inorganic carbon in various reservoirs. Effective implementation of these approaches necessitates rigorous monitoring, reporting, and verification frameworks to ensure their quantifiable efficacy and environmental integrity.
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