Lead isotopic signatures of wine and vineyard soils - tracers of lead origin

被引:52
|
作者
Mihaljevic, M
Ettler, V
Sebek, O
Strnad, L
Chrastny, V
机构
[1] Charles Univ, Inst Geochem Mineral & Mineral Resources, Prague 12843 2, Czech Republic
[2] Charles Univ, Labs Geol Inst, Prague 12843 2, Czech Republic
[3] Univ S Bohemia, Dept Chem, Ceske Budejovice 37005, Czech Republic
关键词
wine; vineyard soil; lead isotope; pollution; ICP-MS;
D O I
10.1016/j.gexplo.2005.08.025
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Pb contents and Pb-206/Pb-207 and Pb-208/(206)pb isotopic ratios were studied in the soils and wines (2004 harvest) of three vineyard areas of the Czech Republic. The areas differ in their geological basements and anthropogenic loading. The isotopic compositions of wine in areas with intensive industry (Most, North Bohemia Pb-206/Pb-207(wine) =1.178 +/- 0.004) and the agricultural areas of Central Bohemia (Roudnice nad Labem Pb-206/Pb-207(wine) = 1.176 +/- 0.007) are similar to the Pb isotopic composition of airborne particulate material typical of polluted and industrial environments (Pb-206/Pb-207 = 1.17-1.19). The isotopic composition of wine from Prague (Pb-206/Pb-207(wine) = 1.174 +/- 0.003) is different from that of the soil, which was severely contaminated in the past by vehicular Pb (Pb-206/Pb-207(soil) = 1.147-1.168). This fact shows that interception of airborne Pb by plants is greater than its uptake by the root system. (c) 2005 Elsevier B.V All rights reserved.
引用
收藏
页码:130 / 133
页数:4
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