Spatio-temporal behaviour and mass balance of fluorine in forest soils near an aluminium smelting plant:: short- and long-term aspects

被引:21
作者
Egli, M [1 ]
Dürrenberger, S [1 ]
Fitze, P [1 ]
机构
[1] Univ Zurich, Dept Geog, CH-8057 Zurich, Switzerland
关键词
fluorine; element fluxes; forest ecosystem; soil monitoring; vegetation; clay minerals;
D O I
10.1016/j.envpol.2003.10.005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
With the help of a large number of monitoring sites, the behaviour of F in forested ecosystems of a formerly polluted area (Mohlin and Rheinfelden, Switzerland) could be studied over 30 years. An aluminium smelting plant originated the pollution of this area in the past: however, after the installation of a filtration plant in 1958 the F emissions were reduced and since 1991 almost absent the primary production of aluminium was stopped. The present-day area with elevated F contents (water-soluble F with > 20 mg/kg) is restricted to a radius of about 1000 in from the plant. In 1969 this area had a radius of about 3 and 5 km. Between 1969 and 2000 a significant decrease in the soluble F content in the soil was observed together with a substantial decrease of F in the vegetation. The net losses of water-soluble F in the soil were in the range of 35 up to more than 70% of the original concentration and the F losses in the vegetation between 60 up to more than 80%. After the reduction of high F deposition rates the accumulated SOM was decomposed within the observation period 1969-1993. The combined decrease in F and humus led to chain reactions with losses of major elements and a dealumination of clay minerals, i.e. removal of interlayered At of 2:1 minerals and consequent formation of smectites. (C) 2003 Elsevier Ltd. All rights reserved.
引用
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页码:195 / 207
页数:13
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