Particle dynamics constrained by 210Po-210Pb-226Ra in the interior of the South China Sea
编号:1440 访问权限:仅限参会人 更新:2026-09-01 00:39:25 浏览:0次 口头报告

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摘要
The sinking of particulate matter largely controls the resident timescales of carbon sequestered in the ocean interior and the level of atmospheric CO2. Owing to a lack of approaches to constrain particle settling, the particle dynamics in the ocean interior remains poorly understood than those in the upper ocean. Here, 210Po, 210Pb, and 226Ra were analyzed to examine the cycling and settling of particulate matter across the water column of the South China Sea. In the euphotic zone, 210Pb is in excess relative to 226Ra (A.R. = 1.46 ± 0.32), indicating the dominance of atmospheric deposition of 210Pb. 210Po is in deficit relative to 210Pb (A.R. = 0.50 ± 0.08), revealing plankton-induced rapid settling of particulate matter. In the intermediate and deep water, the deficit in 210Pb (A.R. > 1.0) indicates that particles continuously remove 210Pb from seawater during settling to depth, supporting the use of 210Pb–226Ra as a tracer for particle sinking in the ocean interior. In contrast, the 210Po-210Pb disequilibrium exhibits spatial heterogeneity. On the northern slope, a 210Po deficit (A.R. < 1.0) is observed, attributed to the cross-shelf/slope transport of particles. In the southwestern basin, the riverine materials resulted in a depletion of 210Po in the Mekong plume region. In the southeastern basin with little influence of shelf and river, a 210Po deficit was only observed down to 1000 m; 210Po reached equilibrium with 210Pb (A.R. ≈ 1.0) in the deep water. In bottom water, the concentrations of particulate matter were 2–3 times those in the overlying water, pointing to the benthic nepheloid layer in the South China Sea and resulting in the enhanced 210Po deficits. Using an inverse model, the settling velocity (SV) varied from 6 to 151 m d-1, averaging 23 ± 14 m d-1. The sinking flux of particles ranged from 0.1 to 11.6 g m-2 d-1, with an average of 2.0 ± 1.1 g m-2 d-1. These results preliminarily elucidated the differential characteristics of particle cycling and settling at various depths in the South China Sea.
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报告人
Weihong Zhu
Xiamen University

稿件作者
Weihong Zhu Xiamen University
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重要日期
  • 会议日期

    01月12日

    2027

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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