Journal of Marine Sciences ›› 2023, Vol. 41 ›› Issue (1): 14-25.DOI: 10.3969-j.issn.1001-909X.2023.01.002
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Carbon cycling in costal ocean and CO2 negative emissions
YU Lei1,2(
), LI Sanzhong1,2, SUO Yanhui1,2,*(), WANG Xiujuan1,2
- 1. Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2. Function Laboratory for Assessment and Prospecting Techniques of Marine Mineral Resources, Laoshan Laboratory, Qingdao 266237, China
-
Received:2022-10-18Revised:2023-01-28Online:2023-03-15Published:2023-04-28
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YU Lei, LI Sanzhong, SUO Yanhui, WANG Xiujuan. Carbon cycling in costal ocean and CO2 negative emissions[J]. Journal of Marine Sciences, 2023, 41(1): 14-25.
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URL: http://hyxyj.sio.org.cn/EN/10.3969-j.issn.1001-909X.2023.01.002
Fig.1 Influencing factors of organic carbon and inorganic carbon fluxes and carbon cycle processes in coastal ocean (Figure was modified from reference[10]. DOC, DIC, POC and hv are dissolved organic carbon, dissolved inorganic carbon, particulate organic carbon and photon energy, respectively.)
Fig.1 Influencing factors of organic carbon and inorganic carbon fluxes and carbon cycle processes in coastal ocean (Figure was modified from reference[10]. DOC, DIC, POC and hv are dissolved organic carbon, dissolved inorganic carbon, particulate organic carbon and photon energy, respectively.)
Fig.2 Statistic data of organic carbon and inorganic carbon fluxes in the three subsystems of tidal wetlands, estuarine and continental shelf in coastal marine system and their transport directions (Figure was modified from reference[10]. OC is organic carbon, IC is inorganic carbon. Red and black values are the carbon fluxes exchanged across and within the boundaries of the coastal ocean, with positive values. Arrows indicate the directions of the carbon matters transport. Blue values represent the balance between gross primary production (GPP) and total system respiration (RAH), i.e., net ecosystem production (NEP), with negative values indicating conversion of OC to IC. Carbon flux error is negligible. The unit is Pg C·a-1.)
Fig.2 Statistic data of organic carbon and inorganic carbon fluxes in the three subsystems of tidal wetlands, estuarine and continental shelf in coastal marine system and their transport directions (Figure was modified from reference[10]. OC is organic carbon, IC is inorganic carbon. Red and black values are the carbon fluxes exchanged across and within the boundaries of the coastal ocean, with positive values. Arrows indicate the directions of the carbon matters transport. Blue values represent the balance between gross primary production (GPP) and total system respiration (RAH), i.e., net ecosystem production (NEP), with negative values indicating conversion of OC to IC. Carbon flux error is negligible. The unit is Pg C·a-1.)
Fig.3 The relationship between annual CO2 flux density and the coastal ocean latitude(a); The relationship between annual CO2 flux density and coastal ocean latitude, compiled from the literatures(b); Seasonal and annual mean ΔpCO2 at 50 km from land(c) (Figure was modified from reference[43].The data of fig.a were from reference[20].)
Fig.3 The relationship between annual CO2 flux density and the coastal ocean latitude(a); The relationship between annual CO2 flux density and coastal ocean latitude, compiled from the literatures(b); Seasonal and annual mean ΔpCO2 at 50 km from land(c) (Figure was modified from reference[43].The data of fig.a were from reference[20].)
Fig.4 pCO2 levels, net ecosystem production (NEP), and organic and inorganic carbon fluxes on pre-industrial and current continental shelves (Figure was modified from reference[10]. The unit for organic carbon, inorganic carbon fluxes and NEP in this figure is Pg C·a-1.)
Fig.4 pCO2 levels, net ecosystem production (NEP), and organic and inorganic carbon fluxes on pre-industrial and current continental shelves (Figure was modified from reference[10]. The unit for organic carbon, inorganic carbon fluxes and NEP in this figure is Pg C·a-1.)
Fig.5 Anthropogenic CO2 emissions(a) and their absorptive amounts in the systems of atmosphere, land and ocean(b) from 1750 to 2011 (Figure was modified from refernce[48].)
Fig.5 Anthropogenic CO2 emissions(a) and their absorptive amounts in the systems of atmosphere, land and ocean(b) from 1750 to 2011 (Figure was modified from refernce[48].)
Fig.6 Ocean carbon negative emission (ONCE) processes mediated by microbial and fluid-rock interactions in anoxic environments (Figure was modified from reference[21]. ONCE including refractory dissolved organic carbon production, alkalinity enhancement, and carbonate minerals precipitation.)
Fig.6 Ocean carbon negative emission (ONCE) processes mediated by microbial and fluid-rock interactions in anoxic environments (Figure was modified from reference[21]. ONCE including refractory dissolved organic carbon production, alkalinity enhancement, and carbonate minerals precipitation.)
Fig.7 Evaluation of CO2storage mechanism and storage safety at different stages after supercritical CO2 injection into sedimentary basins (Figure was modified from reference[1].)
Fig.7 Evaluation of CO2storage mechanism and storage safety at different stages after supercritical CO2 injection into sedimentary basins (Figure was modified from reference[1].)
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