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TRACE ELEMENTS IN ESTONIAN PEAT

机译:爱沙尼亚泥炭中的微量元素

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Estonian peat is commonly used in home country and exported all over the world, therefore we need to know the chemical composition of peat and the concentration of trace elements in it. 684 peat samples from 64 mires were analysed, concentration of 16 trace elements and general characteristics (peat type, degree of humification, pH and ash content) were determined. Samples were taken from the whole section after every 0.5 m, in places 0.25 m. Atomic absorption method was used to determine the concentration of Cd, Cr, Cu, Mn, Ni, Pb and Zn (AASflame), Cd (AAS-ETA), and Hg (cold vapour method). Concentration of As, Co, Mo, Sr, Th, U and V was determined by X-ray fluorescence method. By genesis peatlands are divided into 25 peat districts. The setting of peat layer, its genesis and concentration of trace elements in the peat is presented by the above peat districts. The concentration of trace elements in peat is small: As-2.40,Cd-0.120,Co-0.50,Cr-3.1,Cu-4.4,Hg-0.050,Mn-35.1,Mo-1.2,Ni-3.7, Pb - 3.3, Sr-21.9, Zn-10.0, Th-0.47,U-1.27, V-3.8mg/kg and S -0.25%. Main binding mechanisms are: mechanical, biological, physical-chemical, physical, chemical. The high concentrations of trace elements are mostly related to the mires feeding from springs. The trace elements can reach the human organism in different ways: via the food chain, by inhaling, by drinking water. Results of statistical processing show that Co has the highest positive correlations with different elements and ash content. The high correlation coefficients have also As, Ni, Mo, ash content and pH. The influence of peat layer decreases in the following order: transitional mire - raised bog - fen. The smallest values of most trace elements were recorded in mires feeding from precipitation and the highest - in mires feeding from groundwater. The influence of peat type on the concentration of trace elements decreases from surface layer towards the base. The mineral component of peat was analysed as well. The scientific research shows that the concentration of trace elements is often higher in the bottom part of peat layer. The peat presently produced in Estonia is ecologically clean.
机译:爱沙尼亚泥炭通常在本国使用,并出口到世界各地,因此我们需要了解泥炭的化学组成和其中的微量元素浓度。分析了来自64个泥潭的684个泥炭样品,确定了16种微量元素的浓度和一般特征(豌豆类型,腐殖度,pH和灰分)。每隔0.5 m在0.25 m的地方从整个断面中取样。原子吸收法用于测定Cd,Cr,Cu,Mn,Ni,Pb和Zn(AASflame),Cd(AAS-ETA)和Hg(冷蒸气法)的浓度。通过X射线荧光法测定As,Co,Mo,Sr,Th,U和V的浓度。泥炭地按创世纪划分为25个泥炭区。上述泥炭区介绍了泥炭层的形成,泥炭的成因和微量元素的浓度。泥炭中微量元素的浓度很小:As-2.40,Cd-0.120,Co-0.50,Cr-3.1,Cu-4.4,Hg-0.050,Mn-35.1,Mo-1.2,Ni-3.7,Pb-3.3, Sr-21.9,Zn-10.0,Th-0.47,U-1.27,V-3.8mg / kg和S -0.25%。主要的结合机理是:机械的,生物的,物理化学的,物理的,化学的。痕量元素的高浓度主要与春季的泥潭有关。微量元素可以通过不同的方式到达人体:通过食物链,通过吸入,通过饮用水。统计处理结果表明,Co与不同元素和灰分含量的正相关性最高。高相关系数还具有As,Ni,Mo,灰分和pH。泥炭层的影响按以下顺序减小:过渡泥潭-凸起沼泽-芬。多数微量元素的最小值记录在来自降水的泥潭中,最高值记录在从地下水中的泥潭中。泥炭类型对微量元素浓度的影响从表层向底部逐渐减小。还分析了泥炭的矿物成分。科学研究表明,泥炭层底部的微量元素浓度通常较高。目前在爱沙尼亚生产的泥炭在生态上是清洁的。

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