Major ions and radionuclides in aerosol particles from the South Pole during ISCAT-2000

被引:38
作者
Arimoto, R
Hogan, A
Grube, P
Davis, D
Webb, J
Schloesslin, C
Sage, S
Raccah, F
机构
[1] New Mexico State Univ, Carlsbad Environm Monitoring & Res Ctr, Carlsbad, NM 88220 USA
[2] Cerfified Consulting Meteorol, Piermont, NH 03779 USA
[3] Lyndon State Coll, Dept Meteorol, Lyndonville, VT 05851 USA
[4] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
[5] Environm Measurements Lab, Dept Homeland Secur, New York, NY 10014 USA
基金
美国国家科学基金会;
关键词
sulfur cycle; major ions; trace elements; radionuclides; aerosols; Antarctica; geochemistry;
D O I
10.1016/j.atmosenv.2004.01.049
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
As part of ISCAT 2000, bulk, high-volume, aerosol samples were collected at the South Pole (SP) nominally over 24-h intervals, and they were analyzed for major ions.. several trace elements, and three naturally occurring radionuclides. The mean concentrations of Na (<17 ng m(-3)), sulfate (98 ng m(-3)), and methanesulfonate (MSA, 4.4 mg m(-3)) all were lower in ISCAT 2000 compared with ISCAT 1998, suggesting weaker marine influences during the latter study. In contrast, the Pb-210 activity (0.20 mBq m(-3)) was more than two-times higher in ISCAT 2000 than in 1998, and nitrate concentrations (150 ng m(-3)) were approximately four-times higher, suggesting stronger continental influences in the second study. These differences between experiments are consistent with an analysis of meteorological transport and exchange. 7 Be activities were generally comparable for ISCAT-1998 and 2000, suggesting that there were, on average. similar upper tropospheric/lower stratospheric influences on surface air during the two experiments: long-term records of Be-7, however, show pronounced annual and lower-frequency cycles. The concentration ratios of MSA to nss-sulfate (R) were similar in the two campaigns, and a regression analysis suggests that a non-biogenic source or sources account for up to similar to30% of the nonsea-salt sulfate. Various possible explanations for the low values of R (= 0.08) relative to other Antarctic sites are discussed, including differences in R due to where the oxidation of DMS takes place (that is, in the marine boundary layer or in the buffer layer/free troposphere), chemical fractionation during transport, and the transport of sulfur compounds from lower latitudes and possibly from Mt. Erebus. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:5473 / 5484
页数:12
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