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Regional Differentiation by Lead Isotope Ratios in Different Soil Fractions
Corresponding Author(s) : Jianping Zhang
Asian Journal of Chemistry,
Vol. 25 No. 5 (2013): Vol 25 Issue 5
Abstract
The isotopic ratios of lead vary with geographic locations. In this study, lead isotopic ratios of soil from different regions in Fujian Province are determined by inductively coupled plasma mass spectrometry, the differences of lead isotopic ratios (206Pb/207Pb, 206Pb/208Pb) in the total digests of soil fractions and in that of the residual fractions were compared. The results show that lead isotopic ratios of residual fraction are more efficient than that of total digests of soil fractions in identifying sources of soil.
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References
N.C. Munksgaard, G.J. Batterham and D.L. Parry, Marine Pollut. Bull., 36, 527 (1998).
V.J. Stukas and C.S. Wong, Science, 211, 1424 (1981).
D. Amarasiriwardena and R.M. Barnes, Fresenius J. Anal. Chem., 362, 493 (1998).
Z.Y. Huang, M.F. Yang, Z.X. Zhuang, X.R. Wang and S. Frank, Chin. J. Anal. Chem., 31, 1036 (2003).
Z.Q. Cheng and K.A. Foland, Appl. Geochem., 20, 353 (2005).
A. Tessier, P.G.C. Campbell and M. Blsson, Anal. Chem., 51, 844 (1979).
M. Viczian, A. Lasztity and R.M. Barnes, J. Anal. At. Spectrom., 5, 293 (1990).
C. Latkoczy, T. Prohaska, G. Stingeder and M.T. Nicola, J. Anal. At. Spectrom., 13, 561 (1998).