The content of Cd and Pb in undeveloped and shallow soils and plant material in the area of national park Tara

Angelina Novaković, Stjepan Miletić, J. Beloica, Snežana Belanović-Simić, D. Obratov-Petković
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Abstract

Ultramafic (serpenites) are a group of igneous or metamorphic rocks, which are characterized by high concentrations of Mg, Fe, Ni, Cr, and Co, along with low concentrations of Ca, P, and K, contain less than 45% silicon (SiO2). Tara Mountain is natural good of western Serbia where areas under serpentinites occupy 28%. Researchers agree that the flora of serpentine areas is unique and botanically very important. The specificity of the flora and the development of vegetation on serpentinites are characterized by special mechanisms of plant species adaptation to increased concentrations of some heavy metals in the soil with low content of essential elements (nutrients). This paper examines the influence of serpentinite geological substrate on the occurrence of certain plant species in the initial stages of plant community development. The soil was mainly sampled in rock crevices in the early phases of soil development (Lithosols) where the influence and origin of the metals from the rock can be considered the most obvious. Content of cadmium (Cd) and lead (Pb) in geological substratum, soil and plants biomass is analysed in order to differentiate levels and extents of natural and anthropogenic pollution and also deposition data from the EMEP program (European Monitoring and Evaluation Programme). Results show that the content of lead and cadmium in the soil and plant samples are higher than the content in the corresponding rock sample, except for two soil samples, in which the content of Cd is lower. Thissuggest that the origin of the increased Pb and Cd content might be from anthropogenic sources. Deposition (data from EMEP program) of Cd and Pb, which was analysed for the period from 1990-2018, indicate significant cumulative effect. The values of cumulative deposition in research area have a value of 91,51 kg/km2 lead, while the value of cadmium is 1665 g/km2 , which classifies NP Tara in above-average polluted area in R. Serbia.
塔拉国家公园地区未开发浅土层和植物材料中Cd、Pb的含量
超镁铁质(蛇纹岩)是一组火成岩或变质岩,其特征是含有高浓度的Mg、Fe、Ni、Cr和Co,以及低浓度的Ca、P和K,硅(SiO2)含量低于45%。塔拉山是塞尔维亚西部的天然好地,蛇纹岩下面积占28%。研究人员一致认为,蛇形岩地区的植物群是独特的,在植物学上非常重要。蛇纹岩上植物区系的特殊性和植被的发育与植物物种适应某些重金属浓度增加的特殊机制有关,而土壤中必需元素(养分)含量低。本文研究了蛇纹岩地质基质在植物群落发展初期对某些植物物种发生的影响。在土壤发育的早期阶段(岩石层),土壤主要在岩石裂缝中取样,岩石中金属的影响和来源可以被认为是最明显的。分析了地质基质、土壤和植物生物量中镉(Cd)和铅(Pb)的含量,以区分自然和人为污染的水平和程度,并分析了EMEP计划(欧洲监测和评估计划)的沉积数据。结果表明,土壤和植物样品中的铅和镉含量均高于相应岩石样品中的含量,但两种土壤样品中的Cd含量较低。提示铅、镉含量增加的来源可能是人为因素。对1990年至2018年期间Cd和Pb的沉积(来自EMEP程序的数据)进行了分析,显示出显著的累积效应。研究区铅累积沉降值为91,51 kg/km2,镉累积沉降值为1665 g/km2,将NP Tara划分为塞尔维亚平均以上污染区。
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