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Han Wuying,Lin Hongying,Cai Yanya. 1996. Study on the carbon flux in the South China Sea. Acta Oceanologica Sinica, (1):85-92
Study on the carbon flux in the South China Sea
Study on the carbon flux in the South China Sea
Received:March 05, 1995  Revised:October 04, 1995
DOI:
Key words:South China Sea.carbon  flux  model
中文关键词:  South China Sea.carbon  flux  model
基金项目:The project was supported by National Natural Science Foundation of China under contract Nos.E85057,49176274,49256003,49456001.
Author NameAffiliation
Han Wuying South China Sea Institute of Oceanology, Academy of Sciences of China, Guangzhou 510301, China 
Lin Hongying South China Sea Institute of Oceanology, Academy of Sciences of China, Guangzhou 510301, China 
Cai Yanya South China Sea Institute of Oceanology, Academy of Sciences of China, Guangzhou 510301, China 
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Abstract:
      According to depth, the South China Sea can be divided into three boxes by pycnocline and sill.When sea water rises to Box Ⅰ, dissolved inorganic carbon in water can be changed into particulate organic carbon by the organisms assimilation.One part of the particulate carbon will be changed into dissolved inorganic carbon, other will fall down to Box Ⅱ.The similar process eeds in Box Ⅱ and Box Ⅲ and the unresolved particulate carbon in Box Ⅲ will setth into sediments, finally.
中文摘要:
      According to depth, the South China Sea can be divided into three boxes by pycnocline and sill.When sea water rises to Box Ⅰ, dissolved inorganic carbon in water can be changed into particulate organic carbon by the organisms assimilation.One part of the particulate carbon will be changed into dissolved inorganic carbon, other will fall down to Box Ⅱ.The similar process eeds in Box Ⅱ and Box Ⅲ and the unresolved particulate carbon in Box Ⅲ will setth into sediments, finally.
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