Phosphine in the lower atmosphere of qingdao-a coastal site of the yellow sea (China)

  • Jian Bing Li
  • , Gui Ling Zhang*
  • , Jing Zhang
  • , Su Mei Liu
  • , Jing Ling Ren
  • , Zhong Xin Hou
  • *Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

6 Scopus citations

Abstract

Gaseous phosphine (PH3) in the inshore atmosphere was observed from October 2005 to August 2006 at a coastal site of the Yellow Sea in China. The concentration of PH3 ranged from 0.01 to 14.86 ng m-3 with an average of 1.14 ng m-3. The concentration showed a diurnal variation in PH3 with the peak occurring at morning and the lowest point at noon. An obvious seasonal variation of atmospheric PH3 was found, with the PH3 levels in the summer higher than those in the winter. The PH3 levels in the atmosphere were apparently affected by temperature, radiation, sources, and other meteorological factors. The data indicate that PH3 can be transported between the terrestrial and inshore atmosphere of Qingdao and the Yellow Sea or the East China Sea in both directions. The study increases evidence that PH3 participates within the global biogeochemical phosphorus cycle in P transport from land and inshore waters to the sea where commonly P is scarce and where PH3 inflow could be of important.

Original languageEnglish
Pages (from-to)117-131
Number of pages15
JournalWater, Air, and Soil Pollution
Volume204
Issue number1-4
DOIs
StatePublished - Nov 2009
Externally publishedYes

Keywords

  • Diurnal variation
  • Phosphine
  • Phosphorus transportation
  • Seasonal variation
  • Yellow Sea

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