Geochemistry of the water profiles at the slope of East China Sea and Okinawa Trough and its implications

FAN Jiahui; DOU Yanguang; ZHAO Jingtao; LI Jun; ZOU Liang; CAI Feng; CHEN Xiaohui; LI Qing

doi:10.16562/j.cnki.0256-1492.2021072201

2021 Vol. 41, No. 6

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Article navigation > Marine Geology & Quaternary Geology > 2021 > 41(6): 102-114

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FAN Jiahui, DOU Yanguang, ZHAO Jingtao, LI Jun, ZOU Liang, CAI Feng, CHEN Xiaohui, LI Qing. Geochemistry of the water profiles at the slope of East China Sea and Okinawa Trough and its implications[J]. Marine Geology & Quaternary Geology, 2021, 41(6): 102-114. doi: 10.16562/j.cnki.0256-1492.2021072201

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FAN Jiahui, DOU Yanguang, ZHAO Jingtao, LI Jun, ZOU Liang, CAI Feng, CHEN Xiaohui, LI Qing. Geochemistry of the water profiles at the slope of East China Sea and Okinawa Trough and its implications[J]. Marine Geology & Quaternary Geology, 2021, 41(6): 102-114. doi: 10.16562/j.cnki.0256-1492.2021072201

Geochemistry of the water profiles at the slope of East China Sea and Okinawa Trough and its implications

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Qingdao Institute of Marine Geology, Qingdao 266237, China
3.
China University of Geosciences (Beijing), Beijing 100083, China
4.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
5.
Laboratory for Marine Mineral Resource, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

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Corresponding author: DOU Yanguang, douyanguang@gmail.com

Received Date: 22 July 2021

Revised Date: 19 August 2021

Publish Date: 28 December 2021

Abstract

Abstract

Two water profiles are selected from the northern part of the Okinawa Trough and the elements, such as carbon, chlorine, and boron isotopes and ion concentrations analyzed for investigation of the control factors of the ion and isotope compositions, water source, and modern water exchange process of the water profiles. It is seen that the properties of surface water, subsurface water, and intermediate water in the water profiles are obviously different. The ion concentrations of K⁺, Ca²⁺, and SO₄²⁻ in the ST2 profile increase with water depth, and the vertical changes of δ¹³C, δ¹¹B, and δ³⁷Cl fluctuate substantially. The vertical changing pattern of ion concentrations, and isotopes along the profile ST19 is opposite to the profile ST2. The surface water (0～100 m) and subsurface water (100～300 m) of the profiles ST2 and ST19 are mainly coming from KSW（Kuroshio Surface Water）and KTW（Kuroshio Tropical Water）, affected by CDW（Changjiang Diluted Water）/shelf water, whereas the composition of the intermediate water (300～1000 m) is similar to that of NPIW（North Pacific Intermediate Water) and SCSIW（South China Sea Intermediate Water）. There are obvious north-south differences in water composition between the two profiles, owing to the differences in locality, CDW/shelf water transmission path, local upwelling caused by regional topography and the proportions of NPIW and SCSIW in the water profiles.
- ion concentration /
- carbon, boron, and chlorine isotopes /
- water source /
- north-south difference /
- East China Sea slope /
- Okinawa Trough

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References

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