English  |  正體中文  |  简体中文  |  Items with full text/Total items : 26988/38789
Visitors : 2353187      Online Users : 30
RC Version 4.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
Scope Adv. Search
LoginUploadHelpAboutAdminister

Please use this identifier to cite or link to this item: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/50223

Title: Sinking fluxes of 210Pb and 210Po in the deep basin of the northern South China Sea
Authors: Ching-Ling Wei
Chao-Yuan Chia
Wen-Chen Chou
Wen-Huei Lee
Contributors: 國立臺灣海洋大學:海洋環境與生態研究所
Keywords: 210Pb
210Po
POC flux
PIC flux
Sediment trap
South China Sea
Date: 2016-06
Issue Date: 2018-09-25T08:00:21Z
Publisher: Journal of Environmental Radioactivity
Abstract: Abstract: Vertical fluxes of total mass (Fmass), particulate organic carbon (FPOC), particulate inorganic carbon (FPIC), 210Pb (FPb-210), and 210Po (FPo-210) were determined by sediment traps deployed at two depths, 2000 m and 3500 m, at SEATS (South East Asian Time-series Study, 116°00°E, 18°00°N) in the northern South China Sea during June 2008–June 2009. The Fmass ranges from 12.2 to 55.1 mg m−2 d−1 and from 89.3 to 250.8 mg m−2 d−1, at 2000 m and 3500 m, respectively, and shows seasonal and inter-annul variation. The temporal variation of FPOC, FPIC, and FPb-210 were in phase with the Fmass, which was coupled with the seasonal cycles of primary production in the euphotic layer. The FPb-210 ranges from 5 to 48 dpm m−2d−1 and from 38 to 105 dpm m−2d−1, at 2000 m and 3500 m, respectively. Contrasting with 210Pb, the FPo-210 shows poor correlation with Fmass. The FPo-210 ranges from 3 to 146 dpm m−2d−1 and from 50 to 309 dpm m−2d−1, at 2000 m and 3500 m, respectively. Episodic events of the settling of biological particles from the surface layer and the regeneration processes the deep layer control the 210Po removal in the water column of the South China Sea. Strong correlations of the flux and source ratio of 210Pb, (F/P)Pb-210, and the particulate carbon fluxes were found, which give relationships of FPOC (μg cm−2y−1) = 26.8 + 371.0 (F/P)Pb-210 and FPIC (μg cm−2y−1) = −1.4 + 533.1 (F/P)Pb-210.
Relation: 174 pp.45-53
URI: http://ntour.ntou.edu.tw:8080/ir/handle/987654321/50223
Appears in Collections:[海洋環境與生態研究所] 期刊論文

Files in This Item:

File Description SizeFormat
index.html0KbHTML29View/Open


All items in NTOUR are protected by copyright, with all rights reserved.

 


著作權政策宣告: 本網站之內容為國立臺灣海洋大學所收錄之機構典藏,無償提供學術研究與公眾教育等公益性使用,請合理使用本網站之內容,以尊重著作權人之權益。
網站維護: 海大圖資處 圖書系統組
DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - Feedback