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YANG Weifeng,CHEN Min,HUANG Yipu,LIU Guangshan,JIA Chengxia.Excess polonium-210 in the coastal atmosphere originating from marine biogenic material[J].Acta Oceanologica Sinica,2006,(6):78-87
Excess polonium-210 in the coastal atmosphere originating from marine biogenic material
Excess polonium-210 in the coastal atmosphere originating from marine biogenic material
投稿时间:2006-01-20  修订日期:2006-07-21
DOI:
中文关键词:  excess polonium-210  depositional flux  coastal atmosphere  precipitation
英文关键词:excess polonium-210  depositional flux  coastal atmosphere  precipitation
基金项目:
作者单位E-mail
YANG Weifeng Department of Oceanography, Xiamen University, Xiamen 361005, China  
CHEN Min Department of Oceanography, Xiamen University, Xiamen 361005, China
State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361005, China 
mchen@xmu.edu.cn 
HUANG Yipu Department of Oceanography, Xiamen University, Xiamen 361005, China
State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361005, China 
 
LIU Guangshan Department of Oceanography, Xiamen University, Xiamen 361005, China
State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361005, China 
 
JIA Chengxia Department of Oceanography, Xiamen University, Xiamen 361005, China  
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中文摘要:
      The depositional fluxes of atmospheric polonium-210 were measured at one site in Xiamen from August 2001 to March 2002.With predominant marine air mass, the depositional fluxes of atmospheric polonium-210 ranged from 0.01 to 0.09 Bq/(m2·d), with an average of 0.04 Bq/(m2·d).The seasonal pattern showed elevated polonium-210 fluxes in summer and autumn rather than in winter.Atmospheric depositional fluxes of polonium-210 showed a good correlation with beryllium-7 (r2=0.85) and lead-210 fluxes (r2=0.71), indicating their similar removal mechanism from atmosphere.The relationship between the polonium-210 depositional fluxes and the precipitation amount demonstrated that the precipitation dominates the polonium-210 removal from the atmosphere.The observed high activity ratios of polonium-210 to lead-210 indicated the occurrence of excess polonium-210 in coastal atmosphere, which may originate from marine surface waters either by indirect (foam), or more likely, direct (air-sea exchange) input of marine biogenic material into the atmosphere.This source is even more important than the in situ decay of lead-210.
英文摘要:
      The depositional fluxes of atmospheric polonium-210 were measured at one site in Xiamen from August 2001 to March 2002.With predominant marine air mass, the depositional fluxes of atmospheric polonium-210 ranged from 0.01 to 0.09 Bq/(m2·d), with an average of 0.04 Bq/(m2·d).The seasonal pattern showed elevated polonium-210 fluxes in summer and autumn rather than in winter.Atmospheric depositional fluxes of polonium-210 showed a good correlation with beryllium-7 (r2=0.85) and lead-210 fluxes (r2=0.71), indicating their similar removal mechanism from atmosphere.The relationship between the polonium-210 depositional fluxes and the precipitation amount demonstrated that the precipitation dominates the polonium-210 removal from the atmosphere.The observed high activity ratios of polonium-210 to lead-210 indicated the occurrence of excess polonium-210 in coastal atmosphere, which may originate from marine surface waters either by indirect (foam), or more likely, direct (air-sea exchange) input of marine biogenic material into the atmosphere.This source is even more important than the in situ decay of lead-210.
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