234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea

MA Hao ZENG Zhi YU Wen HE Jianhua CHEN Liqi CHENG Jianping YIN Mingduan ZENG Shi

MAHao, ZENGZhi, YUWen, HEJianhua, CHENLiqi, CHENGJianping, YINMingduan, ZENGShi. 234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea[J]. 海洋学报英文版, 2011, (3): 55-62. doi: 10.1007/s13131-011-0119-2
引用本文: MAHao, ZENGZhi, YUWen, HEJianhua, CHENLiqi, CHENGJianping, YINMingduan, ZENGShi. 234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea[J]. 海洋学报英文版, 2011, (3): 55-62. doi: 10.1007/s13131-011-0119-2
MA Hao, ZENG Zhi, YU Wen, HE Jianhua, CHEN Liqi, CHENG Jianping, YIN Mingduan, ZENG Shi. 234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea[J]. Acta Oceanologica Sinica, 2011, (3): 55-62. doi: 10.1007/s13131-011-0119-2
Citation: MA Hao, ZENG Zhi, YU Wen, HE Jianhua, CHEN Liqi, CHENG Jianping, YIN Mingduan, ZENG Shi. 234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea[J]. Acta Oceanologica Sinica, 2011, (3): 55-62. doi: 10.1007/s13131-011-0119-2

234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea

doi: 10.1007/s13131-011-0119-2
基金项目: The National Natural Science Foundation of China under grant Nos 40531007, 40676062 and 10705019; the scientific research foundation of the Ministry of Science and Technology of China through commonweal grant No. 2007050228 and International Cooperation Program No. 2009DFA22920; Open Fund of the Key Laboratory of Global Change and MarineAtmospheric Chemistry, State Oceanic Administration under grant Nos 0807 and 0902; Tsinghua University Initiative Scientific Research Program.

234Th/238U disequilibrium and particulate organic carbon export in the northwestern South China Sea

  • 摘要: 234Th was utilized as a tracer of particulate organic carbon (POC) export in the northwestern South China Sea (SCS) on the basis of the data collected at four stations during a spring cruise. Depth profiles of dissolved and particulate 234Th activities were measured in the upper 60 m, showing a significant deficit relative to 238U over the investigated stations. A stratified structure of 234Th-238 U disequilibrium was in general observed in the upper 60 m water column, indicating that the euphotic zone of the northwestern SCS in this reason can be divided into two layers, an upper and lower layer, with different export rates. POC export fluxes were estimated from a one-dimensional steady state model of 234Th fluxes in combination with the measurement of POC/234Th ratios on suspended particles. The POC export in this region ranged from 8.2 to 20.0 mmol/(m2·d), with an average of 16.0 mmol/(m2·d), and was slightly higher than those previously reported in the southern SCS.
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出版历程
  • 收稿日期:  2010-07-16
  • 修回日期:  2010-12-29

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