SOURCES OF LEAD IN SOIL AND DUST AND THE USE OF DUST FALLOUT AS A SAMPLING MEDIUM

Citation
Bl. Gulson et al., SOURCES OF LEAD IN SOIL AND DUST AND THE USE OF DUST FALLOUT AS A SAMPLING MEDIUM, Science of the total environment, 166(1-3), 1995, pp. 245-262
Citations number
33
Categorie Soggetti
Environmental Sciences
ISSN journal
00489697
Volume
166
Issue
1-3
Year of publication
1995
Pages
245 - 262
Database
ISI
SICI code
0048-9697(1995)166:1-3<245:SOLISA>2.0.ZU;2-1
Abstract
Pilot investigations using stable lead isotope and scanning electron m icroscopic analyses have been undertaken in different environments ran ging from mining and smelting to urban in order to better understand t he source of, and relationships between, soil and house dust. House du st is characterised by vacuum cleaner dust and/or surface wipes and co mpared with long-term dust (dust fail) accumulations over a > 3-month interval or with airborne particulates. Finer grain sizes of soils hav e lead concentrations from 2 to 9 times those measured in the bulk fra ctions. In Broken Hill isotopic ratios show that the major source of l ead in soils is from the orebody, with rare examples containing lead f rom paint sources. In inner Sydney, soil lead values vary from 37 to 2 660 ppm Pb in bulk samples and up to 3130 ppm in the finer fractions. The lead may be from diverse sources such as gasoline or paint. Finer fractions of vacuum cleaner dust from both Broken Hill and Sydney may contain up to three times the amount of lead measured in the bulk samp les. In Broken Hill, the percentages by weight of total lead in the -2 50-mu m fraction range from 11 to 51%. Bulk vacuum cleaner dusts from Broken Hill contain up to 4490 ppm Pb. Bulk vacuum cleaner dusts from inner Sydney contain up to 2950 ppm Pb. Isotopic variations in fractio ns of vacuum cleaner dust containing > 1000 ppm Pb from inner Sydney i ndicate that the lead in dust has come from different sources and such differences lessen the usefulness of analyses of bulk vacuum cleaner dust. Our results reinforce the importance of analysing the finer frac tion of soil and house dust, especially those in the -150-mu m (or eve n -100-mu m) fraction for soils and the -100-mu m fraction for vacuum cleaner dust. Dust-fall accumulations have many advantages over more c onventional methods for estimating lead in house dust, such as vacuum cleaner dust or surface wipes. These advantages include: low cost; no power source required; can be set up by a technician; minimal inconven ience to householder (i.e., no power required, no noise, out of the wa y, a few minutes to set up and collect); integrates lead flux over a s pecific period; usually unbiased (in contrast to vacuuming or wipes wh ere the householder may clean prior to a sampling visit); easy to 'con trol' by placement of other dishes in the same house. For Broken Hill, a strong correlation (r = 0.95) was obtained between the isotopic com position of lead in blood and dust-fall accumulation.