首页> 外文期刊>Environmental Protection and Natural Resources >Accumulation of metallic elements into the superficial peat layer of mires and wet mineral soils of Estonian forest land / Akumulacja metali w powierzchniowej warstwie gleb torfowych i wilgotnych glebach mineralnych ekosystemów le?nych Estonii
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Accumulation of metallic elements into the superficial peat layer of mires and wet mineral soils of Estonian forest land / Akumulacja metali w powierzchniowej warstwie gleb torfowych i wilgotnych glebach mineralnych ekosystemów le?nych Estonii

机译:爱沙尼亚林地的沼泽和湿润的矿物土壤表层泥炭层中金属元素的积累/爱沙尼亚森林生态系统的泥炭土和湿润矿物土壤表层中金属的积累

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This article studied the extent of accumulation of aqua regia extractable metallic elements (Al, Mg, Pb, Zn, Hg, Cd) into peaty (histic) epipedon (EP) of fen soils, transitional bog soils, peaty gley soils and peaty podzols. The accumulation coefficients (Kac) of the elements in EP were estimated in relation of forest floor (FF, as an input) as a comparison to deeper levels (SS, as a past background). The study revealed that the extent of accumulation and its order depend on soil (peat) type or pedo-ecological conditions of peatification. In the forming of EP from FF, the concentrations of Al and Pb were increased on an average 2.5-5.0 times, but that of Hg increased significantly only in peaty soils (on an average 1.5-1.6 times). The contents of Zn were significantly decreased (Kac 0.1-0.5) in all soil groups. The comparison of EP peats concentrations with SS data demonstrated a considerable accumulation of Pb, Cd, Zn and Hg into thin (~20 cm) superficial peat layer.
机译:本文研究了王水可提取金属元素(Al,Mg,Pb,Zn,Hg,Cd)累积到土,过渡性沼泽土壤,豌豆格利土壤和豌豆足动物的豌豆(历史)表皮(EP)中的积累程度。估计EP中元素的积累系数(Kac)是与林地(FF,作为输入)的关系,作为与更深层次(SS,作为过去的背景)的比较。研究表明,积累的程度及其顺序取决于土壤(豆类)的类型或泥炭化的土壤生态条件。在由FF形成的EP中,Al和Pb的浓度平均增加2.5-5.0倍,而Hg的浓度仅在豆质土壤中显着增加(平均1.5-1.6倍)。在所有土壤组中,锌的含量均显着下降(Kac 0.1-0.5)。 EP泥炭浓度与SS数据的比较表明,Pb,Cd,Zn和Hg大量积累到薄的(约20 cm)浅层泥炭层中。

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