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ZHU Zhuoyi,WU Ying,ZHANG Jing,WEI Hao. 2005. Spatial and temporal variation of particulate organic carbon in the PN section of East China Sea. Acta Oceanologica Sinica, (5):89-99
Spatial and temporal variation of particulate organic carbon in the PN section of East China Sea
Spatial and temporal variation of particulate organic carbon in the PN section of East China Sea
Received:April 05, 2005  Revised:July 09, 2005
DOI:
Key words:POC  PN  East China Sea  PN section
中文关键词:  POC  PN  East China Sea  PN section
基金项目:
Author NameAffiliationE-mail
ZHU Zhuoyi State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China zhu.Zhuoyi@163.com 
WU Ying State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China  
ZHANG Jing State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266003, China 
 
WEI Hao Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003, China  
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Abstract:
      Variations of the particulate organic carbon and nitrogen (POC/PN) along the PN section in the East China Sea (ECS) were examined based on POC/PN data obtained in September 2002.A comparison with others work indicates that POC is the highest in summer, followed by autumn and spring, and the lowest in winter.Generally, POC concentration decreases seawards, and the in situ productivity in September plays an important role in POC distribution.POC in the PN section is composed of terrestrial, resuspended, in situ produced carbon and carbon originated from the Kuroshio waters.The Changjiang River effects the ECS in the PN section, but the influence is mainly minimiged beyond 123.5° E because ofbarrier effect.The impact of Kuroshio subsurface water (KSSW) over shelf break can also effect POC distribution, with high POC concentration there.
中文摘要:
      Variations of the particulate organic carbon and nitrogen (POC/PN) along the PN section in the East China Sea (ECS) were examined based on POC/PN data obtained in September 2002.A comparison with others work indicates that POC is the highest in summer, followed by autumn and spring, and the lowest in winter.Generally, POC concentration decreases seawards, and the in situ productivity in September plays an important role in POC distribution.POC in the PN section is composed of terrestrial, resuspended, in situ produced carbon and carbon originated from the Kuroshio waters.The Changjiang River effects the ECS in the PN section, but the influence is mainly minimiged beyond 123.5° E because ofbarrier effect.The impact of Kuroshio subsurface water (KSSW) over shelf break can also effect POC distribution, with high POC concentration there.
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