极地研究 ›› 2004, Vol. 15 ›› Issue (1-English): 47-54.

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The biogeochemistry of carbon cycle in summer of the Prydz Bay, Antarctic ⅳ:Characteristics of DOC distribution

 Hu Chuanyu, Pan Jianming, Liu Xiaoya and Zhang Haisheng   

  1. Second Institute of Oceanography, SOA, Key Lab of Submarine Geosciences of SOA, Hangzhou 310012
  • 出版日期:1954-03-30 发布日期:1954-03-30
  • 通讯作者: Hu Chuanyu

The biogeochemistry of carbon cycle in summer of the Prydz Bay, Antarctic ⅳ:Characteristics of DOC distribution

 Hu Chuanyu, Pan Jianming, Liu Xiaoya and Zhang Haisheng   

  1. Second Institute of Oceanography, SOA, Key Lab of Submarine Geosciences of SOA, Hangzhou 310012
  • Online:1954-03-30 Published:1954-03-30
  • Contact: Hu Chuanyu

摘要:

The distributions and changes of dissolved organic carbon in the Prydz Bay and out open sea were investigated during CHINARE-15 (the 15th Chinese National Antarctic Research Expedition). The results showed that the content of DOC was higher in the Prydz Bay and outer open sea compared to those typical of surface oceanic levels (70- 80 μM), average content of DOC in the surface water was 102.32 μM, the range was 68.23- 125.92 μM. The vertical distribution of DOC in the water column was similar to many ocean sites, that is to say, the content of upper water is higher than deep water, a subsurface maximum persisted between 25- 50 m. The DOC pool in the Prydz Bay were consisted with labile, semi-labile and refractory pools, in which refractory pools was mainly part. The concentration of refractory DOC was 92.34 and 76.89 μM in Prydz Bay and outer open sea, and account 77% and 82% for total DOC, respectively.

关键词: distribution of DOC, Prydz Bay, Antarctic

Abstract:

The distributions and changes of dissolved organic carbon in the Prydz Bay and out open sea were investigated during CHINARE-15 (the 15th Chinese National Antarctic Research Expedition). The results showed that the content of DOC was higher in the Prydz Bay and outer open sea compared to those typical of surface oceanic levels (70- 80 μM), average content of DOC in the surface water was 102.32 μM, the range was 68.23- 125.92 μM. The vertical distribution of DOC in the water column was similar to many ocean sites, that is to say, the content of upper water is higher than deep water, a subsurface maximum persisted between 25- 50 m. The DOC pool in the Prydz Bay were consisted with labile, semi-labile and refractory pools, in which refractory pools was mainly part. The concentration of refractory DOC was 92.34 and 76.89 μM in Prydz Bay and outer open sea, and account 77% and 82% for total DOC, respectively.

Key words: distribution of DOC, Prydz Bay, Antarctic