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Mercury and methylmercury in soil and vegetation of various polluted areas in Slovenia

机译:斯洛文尼亚各污染区土壤和植被中的汞和甲基汞

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摘要

Mercury (Hg) concentrations in soils oscillate locally and depend on the vicinity of contamination sources, geological bedrock composition, soil chemistry, meteorological conditions, vegetation cover and various anthropogenic factors. Besides, Hg concentrations in vegetation depend also on the limited selective uptake, plant metabolism and elimination. Since geologically and pedologically Slovenia represents very heterogeneous area, a systematic grid study was performed in the 1980s and 1990s in order to establish Hg concentrations in soils (LOBNIK et al., 1992; PIRC, 1993; SAJN et al., 1998; SAJN, 1999) - see Fig. 1. Specific concerns were devoted to the urban and industrially polluted areas (SAJN et al., 1998) - see Fig.2a - Ljubljana and to the geological anomaly in the Tdrija area, where rich geological Hg deposits are situated and Hg-ore was exploited for more than 500 years (HESS, 1993; GOSAR & SAJN, 2001) - see Eig.2b However, the need for further measurements and speciation of Hg in soils and vegetation was identified in order to clarify the spatial and temporal distribution of Hg and its transfer to watersheds and biota.
机译:土壤中的汞(Hg)浓度局部波动,并取决于附近的污染源,地质基岩成分,土壤化学,气象条件,植被覆盖和各种人为因素。此外,植被中的汞浓度还取决于有限的选择性吸收,植物代谢和清除。由于斯洛文尼亚在地质和人文学上代表着非常不同的地区,因此在1980年代和1990年代进行了系统的网格研究,以确定土壤中的汞浓度(LOBNIK等,1992; PIRC,1993; SAJN等,1998; SAJN, 1999年)-见图1。特别关注的是城市和工业污染地区(SAJN等,1998年)-见图2a-卢布尔雅那和特德里亚地区的地质异常,那里有丰富的地质汞矿床汞矿石的开采和开采已经有500多年的历史(HESS,1993; GOSAR和SAJN,2001)-参见图2b。但是,为了进一步明确土壤和植被中的汞,已确定需要进行进一步的测量和形态分析。汞的时空分布及其向流域和生物区系的转移。

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