地球科学进展 ›› 2015, Vol. 30 ›› Issue (2): 214 -225. doi: 10.11867/j.issn.1001-8166.2015.02.0214

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黑潮与毗邻陆架海域的碳交换
卢汐 1, 2( ), 宋金明 1, *( ), 袁华茂 1, 李宁 1   
  1. 1. 中国科学院海洋研究所海洋生态与环境科学重点实验室,山东青岛 266071
    2. 中国科学院大学地球科学学院,北京 100049
  • 出版日期:2015-03-08
  • 通讯作者: 宋金明 E-mail:luxi_19900209@hotmail.com;jmsong@ms.qdio.ac.cn
  • 基金资助:
    中国科学院战略性先导科技专项“黑潮向近海生源要素的输送”(编号:XDA11020102)和“黄东海典型海域海气界面碳通量”(编号:XDA05030402)资助

Carbon Distribution and Exchange of Kuroshio and Adjacent China Sea Shelf: A Review

Xi Lu 1, 2( ), Jinming Song 1( ), Huamao Yuan 1, Ning Li 1   

  1. 1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Online:2015-03-08 Published:2015-02-20

作为沟通陆架边缘海与开放大洋的北太平洋西边界流,黑潮对毗邻中国陆架海域碳循环有着不可忽视的影响。分析总结了黑潮与毗邻陆架海域海水中溶解有机碳(DOC)、颗粒有机碳(POC)、溶解无机碳(DIC)和颗粒无机碳(PIC)分布与交换的现有研究成果。分析表明,黑潮通过表层水涡旋、入侵以及次表层以下水体上涌等形式携碳进入毗邻陆架海域。在黑潮与毗邻陆架海域,DOC和POC的分布受生物活动、水团混合以及沉积物—水界面相互作用的共同影响,表层与陆架水中含量较高,DIC受海水碳酸盐体系平衡影响,表层含量低于底层,在陆架海域与上升流区有高值,PIC含量较低。在台湾东北海域,DOC,POC和DIC由东海陆架海域向黑潮有净输出,输出量分别为2 431×109,1 051×109和21 733×109 mol C/a,PIC通过陆架源悬浮颗粒物向黑潮主流输送,通量为1 852×109 mol C/a。DOC,POC和PIC由南海经吕宋海峡向黑潮有净输出,输出量分别为2 652×109,1 009×109和230×109 mol C/a,但DIC由黑潮向南海有净输出,通量为13 005×109 mol C/a。台湾海峡碳循环受黑潮输运的影响,但影响机制及过程至今并不清楚。因此,黑潮与毗邻陆架海域的碳交换过程研究还有若干重大科学问题亟待解决,尚需深入系统的研究。

The Kuroshio, as the western boundary current of the North Pacific Ocean, communicates waters between China marginal seas and the open ocean, thus has vital impact on the carbon budgets in adjacent East China Sea Shelf area. The distributions and exchange processes of Dissolved Organic Carbon (DOC), Particulate Organic Carbon (POC), Dissolved Inorganic Carbon (DIC) and Particulate Inorganic Carbon (PIC) between Kuroshio current and adjacent China Sea Shelf were reviewed. The Kuroshio entered the East China Sea Shelf area via eddies, intrusion and upwelling. In the study area, the distributions of DOC and POC were affected by biological activity, mixing of water masses and interaction at the seasediment interface. Both DOC and POC were higher in the coastal area than in the Kuroshio area, and had maximum values on the surface layer. DIC, controlled by the balance of carbonate system in seawater, was higher in coastal area and upwelling area, and had minimum value in the surface water. The concentration of PIC was low. In the exchange area off northeastern Taiwan, DOC, POC and DIC were exported from shelf area to the Kuroshio current. The net export values were 2 431×109, 1 051×109 and 21 733×109 mol C/a, respectively. Offshore transportation of suspended particles from shelf area might export PIC to Kuroshio current (1 852×109 mol C/a). In Luzon Strait, DOC, POC and PIC were exported to the Kuroshio waters from South China Sea shelf area. The net export fluxes were 2 652×109, 1 009×109 and 230×109 mol C/a, respectively. DIC had a year-round net flux export from Kuroshio to South China Sea Shelf (13 005×109 mol C/a). Carbon cycling in Taiwan Strait was influenced by Kuroshio waters, but the way and extent of the influence was inconclusive. Several important questions remain to be answered before more accurate conclusions are made.

中图分类号: 

图1 黑潮流系示意图
Fig. 1 Kuroshio and adjacent marginal seas area
表1 东海陆架表层水及黑潮各水层水文特征
Table 1 Hydrography parameters in East China Sea Shelf and Kuroshio main stream
表2 东海近岸表层水及黑潮不同水层水体中的DOC(单位:μmol/L)
Table 2 DOC concentrations in waters of East China Sea and Kuroshio main stream (unit: μmol/L)
表3 东海近岸表层水及黑潮不同水层水体中的POC(单位:μmol/L)
Table 3 POC concentrations in waters of East China Sea and Kuroshio main stream (unit: μmol/L)
表4 东海近岸表层水及黑潮不同水层水体中的DIC(单位:μmol/kg)
Table 4 DIC concentrations in waters of East China Sea and Kuroshio main stream (unit: μmol/kg )
表5 台湾东北部海域跨陆架碳收支(单位:10 9mol C/a)
Table 5 Cross-shelf carbon fluxes off northeastern Taiwan (unit: 10 9mol C/a)
图2 黑潮与毗邻陆架海域间的碳交换通量(单位:10 9mol C/a) [ 15 , 52 ] SCSSW:南海表层水;SCSIW:南海中层水;KSW:黑潮表层水;KTW:黑潮热带水;KIW:黑潮中层水;KDW:黑潮深层水;ECSSW:东海表层水;ECSSS:东海悬浮沉积物
Fig.2 Carbon fluxes between Kuroshio current and adjacent marginal seas (unit: 10 9mol C/a) [ 15 , 52 ] SCSSW: South China Sea Surface Water; SCSIW: South China Sea Intermediate Water; KSW: Kuroshio Surface Water; KTW: Kuroshio Tropical Water; KIW: Kuroshio Intermediate Water; KDW: Kuroshio Deep Water; ECSSW: East China Sea Surface Water; ECSSS: East China Sea Suspended Sediments
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