Origin of Lead in Eight Central European Peat Bogs Determined from Isotope Ratios, Strengths, and Operation Times of Regional Pollution Sources

Martin Novák,* Simon Emmanuel, Melanie A. Vile,§ Yigal Erel, Alain Véron, Tomáš Paes, R. Kelman Wieder, Mirko Vaněek,# Markéta Štěpánová, Eva Břízová, and Jan Hovorka
Department of Geochemistry, Czech Geological Survey, Geologick 6, 152 00 Prague 5, Czech Republic, Institute of Earth Sciences, The Hebrew University, Jerusalem 91904, Israel, Department of Ecology and Evolutionary Biology, 106A Guyot Hall, Princeton University, Princeton, New Jersey, CEREGE, UMR CNRS 6635, Universite Aix-Marseille, Europole Mediterraneen, BP80 Plateau Petit Arbois, 13545 Aix en Provence, France, Department of Biology, Villanova University, Villanova, Pennsylvania 19085, Geofond of the Czech Republic, Kosteln 26, 170 21 Prague 7, Czech Republic, Department of Quaternary Research, Czech Geological Survey, Klrov 3, 118 21 Prague 1, Czech Republic, and Institute for Environmental Studies, Charles University, Bentsk 2, 128 01 Prague 2, Czech Republic
Environ. Sci. Technol., 2003, 37 (3), pp 437–445
DOI: 10.1021/es0200387
Publication Date (Web): December 18, 2002
Copyright © 2003 American Chemical Society
*

 Corresponding author phone:  +420-251816540; fax:  +420-251818748; e-mail:  novak@cgu.cz.

,

 Department of Geochemistry, Czech Geological Survey.

,

 The Hebrew University.

,
§

 Princeton University

,

 Universite Aix-Marseille.

,

 Villanova University.

,
#

 Geofond of the Czech Republic.

,

 Department of Quaternary Research, Czech Geological Survey.

,

 Charles University.

Abstract

Lead originating from coal burning, gasoline burning, and ore smelting was identified in 210Pb-dated profiles through eight peat bogs distributed over an area of 60 000 km2. The Sphagnum-dominated bogs were located mainly in mountainous regions of the Czech Republic bordering with Germany, Austria, and Poland. Basal peat 14C-dated at 11 000 years BP had a relatively high 206Pb/207Pb ratio (1.193). Peat deposited around 1800 AD had a lower 206Pb/207Pb ratio of 1.168−1.178, indicating that environmental lead in Central Europe had been largely affected by human activity (smelting) even before the beginning of the Industrial Revolution. Five of the sites exhibited a nearly constant 206Pb/207Pb ratio (1.175) throughout the 19th century, resembling the “anthropogenic baseline” described in Northern Europe (1.17). At all sites, the206Pb/207Pb ratio of peat decreased at least until 1980; at four sites, a reversal to more radiogenic values (higher 206Pb/207Pb), typical of easing pollution, was observed in the following decade (1980−1990). A time series of annual outputs for 14 different mining districts dispersing lead into the environment has been constructed for the past 200 years. The production of Ag−Pb, coal, and leaded gasoline peaked in 1900, 1980, and 1980, respectively. In contrast to other European countries, no peak in annual Pb accumulation rates was found in 1900, the year of maximum ore smelting. The highest annual Pb accumulation rates in peat were consistent with the highest Pb emission rates from coal-fired power plants and traffic (1980). Although maximum coal and gasoline production coincided in time, their isotope ratios were unique. The mean measured 206Pb/207Pb ratios of local coal, ores, and gasoline were 1.19, 1.16, and 1.11, respectively. A considerable proportion of coal emissions, relative to gasoline emisions, was responsible for the higher 206Pb/207Pb ratios in the recent atmosphere (1.15) compared to Western Europe (1.10). As in West European countries, the gasoline sold in the Czech Republic during the Communist era (1948−1989) contained an admixture of low-radiogenic Precambrian lead from Australia.

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History

  • Published In Issue February 01, 2003
  • Received for review February 20, 2002
    Revised manuscript received October 14, 2002
    Accepted October 28, 2002

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