DIRECT DETERMINATION OF ATMOSPHERIC LEAD BY ZEEMAN SOLID SAMPLING GRAPHITE-FURNACE ATOMIC-ABSORPTION SPECTROMETRY (GFAAS)

被引:15
作者
LOW, PS
HSU, GJ
机构
[1] FORSCHUNGSZENTRUM JULICH, NUCL RES CTR, INST APPL PHYS CHEM, W-5170 JULICH 1, GERMANY
[2] GRUN ANALYSENGERATE GMBH WETZLAR, W-6330 WETZLAR, GERMANY
来源
FRESENIUS JOURNAL OF ANALYTICAL CHEMISTRY | 1990年 / 337卷 / 03期
关键词
D O I
10.1007/BF00321978
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Atmospheric lead was collected by membrane filters using two low volume air samplers at Jülich, Stolberg, and Wetzlar, Federal Republic of Germany. Sampling times varied from 2 to 8 h. After sampling, each filter was subsampled in two cross-sections using a clean stainless steel punch (diameter 5 mm). The lead content of each subsample disc was determined directly by Zeeman GFAAS, calibrated with aqueous standard solutions and supported by solid reference materials. The distribution of lead between the subsamples was generally homogeneous, with standard deviations ranging from 11 to 37%, but typically <15% for samples with 8 h sampling time. The analysis of each filter usually took about 30 min. The differences in air quality between the three sampling locations, as measured by the lead concentrations, are discussed. In general, Stolberg appears to have the highest lead concentrations. The mass particle-size distribution of lead in the aerosol samples collected by membrane filters using a cascade impactor at Stolberg was also investigated with the same analytical technique. Using graphite platform boats as direct samplers, it is possible for the dry deposition flux of lead to be estimated. This provides a quick means of assessing the levels of lead pollution in the atmospheric environment. With lead concentrations measured in parallel, the dry deposition velocities of lead can be estimated under various meteorological conditions. Application of similar sampling and analytical techniques to other atmospheric trace metals may be possible. © 1990 Springer-Verlag.
引用
收藏
页码:299 / 305
页数:7
相关论文
共 23 条
[1]   ATMOSPHERIC TRACE-ELEMENTS AT ENEWETAK ATOLL .2. TRANSPORT TO THE OCEAN BY WET AND DRY DEPOSITION [J].
ARIMOTO, R ;
DUCE, RA ;
RAY, BJ ;
UNNI, CK .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1985, 90 (ND1) :2391-2408
[2]   TRACE-ELEMENTS IN THE ATMOSPHERE OF AMERICAN-SAMOA - CONCENTRATIONS AND DEPOSITION TO THE TROPICAL SOUTH-PACIFIC [J].
ARIMOTO, R ;
DUCE, RA ;
RAY, BJ ;
HEWITT, AD ;
WILLIAMS, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D7) :8465-8479
[3]  
BLOOM H, 1983, SEARCH, V14, P315
[4]  
BRYCESMITH D, 1980, LEAD HLTH
[6]   THE INFLUENCE OF SURFACE-STRUCTURE ON PREDICTED PARTICLE DRY DEPOSITION TO NATURAL GRASS CANOPIES [J].
DAVIDSON, CI ;
MILLER, JM ;
PLESKOW, MA .
WATER AIR AND SOIL POLLUTION, 1982, 18 (1-3) :25-43
[7]   LEAD AND CHILD-DEVELOPMENT [J].
DAVIS, JM ;
SVENDSGAARD, DJ .
NATURE, 1987, 329 (6137) :297-300
[8]   DRY DEPOSITION ON A SNOW SURFACE [J].
DOVLAND, H ;
ELIASSEN, A .
ATMOSPHERIC ENVIRONMENT, 1976, 10 (09) :783-785
[9]  
GARLAND JA, 1982, DEPOSITION ATMOSPHER, P9