Title of article :
Aerosol composition and its sources at the King Sejong Station, Antarctic peninsula
Author/Authors :
Vinit K. Mishra، نويسنده , , Ki-Hyun Kim، نويسنده , , Sungmin Hong، نويسنده , , Khanghyun Lee، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2004
Pages :
16
From page :
4069
To page :
4084
Abstract :
The annual cycles of major metals and ions in suspended particulate matters (SPM) have been investigated at a costal site of the Antarctic Peninsula in order to elucidate temporal variations as well as major source processes responsible for their formation. The measurements had been performed from January 2000 to December 2001 at the Korean Antarctic research station, ‘King Sejong’ (62°13′ S, 58°47′ W). The observed time series of important aerosol components showed clear seasonal variation patterns, while the mean elemental concentrations (e.g., 1875 (Al), 10.3 (Ba), 0.3 (Bi), 1.3 (Cd), 1.7 pg m−3 (Co)) were generally compatible with those reported previously. The presence of high EF values with respect to both mean crustal and seawater composition (such as Bi, Cd, Cr, Cu, Ni, V, and Zn), however, suggests a possibly important role of anthropogenic processes in this remote site. In contrast, the concentrations of ionic species were not clearly distinguishable from those of other Antarctic sites; but the consideration of ionic mass balance between cations and anions pointed out the uniqueness of their source/sink processes in the study area. The major source processes of those aerosol components were also investigated using a series of statistical analyses. The overall results of our study indicated the dominance of several processes (or sources) such as sea-salt emission, secondary aerosol formation, and anthropogenic pollution from both local and distant sources.
Keywords :
aerosol , seasonal variations , enrichment factor , Source/sink , King Sejong station
Journal title :
Atmospheric Environment
Serial Year :
2004
Journal title :
Atmospheric Environment
Record number :
758270
Link To Document :
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