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Volume 44 Issue 11
Nov.  2022
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Article Contents
Huang Ya’nan. Source and sedimentary process of 239+240Pu in the eastern China seas[J]. Haiyang Xuebao,2022, 44(11):77–87 doi: 10.12284/hyxb2022123
Citation: Huang Ya’nan. Source and sedimentary process of 239+240Pu in the eastern China seas[J]. Haiyang Xuebao,2022, 44(11):77–87 doi: 10.12284/hyxb2022123

Source and sedimentary process of 239+240Pu in the eastern China seas

doi: 10.12284/hyxb2022123
  • Received Date: 2021-11-19
  • Rev Recd Date: 2022-05-01
  • Available Online: 2022-06-23
  • Publish Date: 2022-11-03
  • This study compiled the data of 239+240Pu specific activity, 240Pu/239Pu atom ratio and 239+240Pu flux or inventory in the East China Sea and adjacent waters. Based on the 239+240Pu concentration in atmospheric fallout, 239+240Pu in seawater, 239+240Pu in organisms, 239+240Pu in sediment trap and 239+240Pu in sediment, the geochemical behavior of 239+240Pu were explained in the East China Sea and adjacent waters. The results showed that global fallout and Pacific proving grounds close-in fallout were the two major sources of 239+240Pu. Under the influence of water masses such as the Changjing River diluted water, Zhejiang-Fujian Coastal Current, Taiwan Warm Current, Kuroshio Current and upwelling current, mixing effect and removal effect, the concentration of 239+240Pu in coastal waters of the East China Sea showed a trend of removal over time, the burial depth of 239+240Pu in the near shore sediments was deeper than that in the far sea area. In the northeast of Taiwan Island of China, the 239+240Pu specific activity and 239+240Pu inventory in Okinawa Trough increased significantly under the influence of Kuroshio current intrusion and upwelling current. At the same time, this study found that the relationship between 239+240Pu specific activity and 240Pu/239Pu atom ratio in surface sediments of the East China Sea, and confirmed the existence of a tributary of the Kuroshio bottom in northeastern Taiwan, and indicated the location where the Taiwan Warm Current and a tributary of the Kuroshio bottom may intersect.
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