西太平洋深水盆地海水及孔隙水的微量元素地球化学特征

邓义楠; 任江波; 郭庆军; 王海峰; 于哲; 刘晨晖

doi:10.3799/dqkx.2017.562

Volume 44 Issue 9

Sep. 2019

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Article Navigation > Earth Science > 2019 > 44(9): 3101-3114

Deng Yinan, Ren Jiangbo, Guo Qingjun, Wang Haifeng, Yu Zhe, Liu Chenhui, 2019. Trace Elements Geochemistry Characteristics of Seawater and Porewater in Deep-Water Basin, Western Pacific. Earth Science, 44(9): 3101-3114. doi: 10.3799/dqkx.2017.562

Citation:

Deng Yinan, Ren Jiangbo, Guo Qingjun, Wang Haifeng, Yu Zhe, Liu Chenhui, 2019. Trace Elements Geochemistry Characteristics of Seawater and Porewater in Deep-Water Basin, Western Pacific. Earth Science, 44(9): 3101-3114. doi: 10.3799/dqkx.2017.562

Citation:

Deng Yinan, Ren Jiangbo, Guo Qingjun, Wang Haifeng, Yu Zhe, Liu Chenhui, 2019. Trace Elements Geochemistry Characteristics of Seawater and Porewater in Deep-Water Basin, Western Pacific. Earth Science, 44(9): 3101-3114. doi: 10.3799/dqkx.2017.562

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Trace Elements Geochemistry Characteristics of Seawater and Porewater in Deep-Water Basin, Western Pacific

doi: 10.3799/dqkx.2017.562

Deng Yinan^{1,2
,},
Ren Jiangbo^1,2,
Guo Qingjun^{3
,
,},
Wang Haifeng^1,2,
Yu Zhe^1,2,
Liu Chenhui⁴

1.
Key Laboratory of Marine Mineral Resources of Ministry of Natural Resources, Guangzhou 510075, China
2.
Guangzhou Marine Geological Survey, Guangzhou 510075, China
3.
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
4.
State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210008, China

Received Date: 2017-02-09
Publish Date: 2019-09-15

Abstract

Abstract

The geochemical characteristics of seawater and porewater in the deep-water basin of western Pacific and its impact on the formation of polymetallic nodules in the sea are still lacking. Seawater and porewater samples were systematically collected in western Pacific. We analyzed the hydro-chemical characteristics in seawater and trace elements in seawater and porewater. The results indicate that DO and pH values show a decrease followed by a rise with depth, whereas SiO₃^2-, NO₃^- and PO₄^3- values exhibit the reverse change trend. The variations of trace elements in seawater show a same trend with nutrient values. Trace metals in porewater are enriched in seawater-sediment interface, and then this concentration increases by degradation of authigenic material located in 3-5 cm in surface sediment. We suggest that relatively high concentration of trace metals in bottom seawater was derived from biological process, and it led to enrichment of polymetallic nodule on extensive oxic surface sediment. Compared to other areas, metal elements (Sc, Cr, Ni, Pb, especially Cu and Co) which were dissolved from detrital component, might play a key role in nodule growth in western Pacific.
- trace element,
- geochemistry,
- seawater,
- porewater,
- migration of trace elements,
- polymetallic nodule,
- western Pacific

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References(72)

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Trace Elements Geochemistry Characteristics of Seawater and Porewater in Deep-Water Basin, Western Pacific

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