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Volume 43 Issue 11
Dec.  2021
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Article Contents
Liu Chuyue,Zhong Qiangqiang,Huang Dekun, et al. Distribution characteristics of 7Be, 210Po and 210Pb in the surface snow of the Arctic Ocean[J]. Haiyang Xuebao,2021, 43(11):70–76 doi: 10.12284/hyxb2021138
Citation: Liu Chuyue,Zhong Qiangqiang,Huang Dekun, et al. Distribution characteristics of 7Be, 210Po and 210Pb in the surface snow of the Arctic Ocean[J]. Haiyang Xuebao,2021, 43(11):70–76 doi: 10.12284/hyxb2021138

Distribution characteristics of 7Be, 210Po and 210Pb in the surface snow of the Arctic Ocean

doi: 10.12284/hyxb2021138
  • Received Date: 2021-04-27
  • Rev Recd Date: 2021-05-31
  • Available Online: 2021-06-21
  • Publish Date: 2021-12-31
  • The radionuclides 7Be, 210Po and 210Pb transported by the atmosphere can be used as important tracers for studying the material deposition flux of the Arctic Ocean’s atmosphere, modern ocean sedimentation and the transport of materials into the sea ice. They have been widely used in the study of air mass movement, soil erosion, and particle circulation processes in water systems. This paper reports the activities of 7Be, 210Po and 210Pb in the surface snow of the high-latitude ice floes of the Arctic Ocean in 2018. The activity concentrations of 7Be, 210Po and 210Pb are 33.6−632.68 mBq/L, 36.2−87.5 mBq/L, and 30.9−194.49 mBq/L, respectively. The activity concentrations of 7Be and 210Pb in the surface snow of the Arctic Ocean are lower than those in the mid-latitude continental areas. The results show that the activity concentrations of 7Be in snow increased with the increase of latitude. The activity ratio of 210Po/210Pb ranged from 0.70 to 1.48 (with an average of 0.93), 210Po is almost in equilibrium with 210Pb. It indicates that the age of the surface snow is “older”.
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