Department of Environment and Natural Resources, Agricultural University of Tirana, Koder-Kamez 1029, Tirana, Albania.
Institute of Soil Science and Soil Conservation, Research Centre for Biosystems, Land Use and Nutrition (iFZ), Justus Liebig University Giessen, Heinrich-Buff-Ring 26-32, 35392, Giessen, Germany.
Environ Monit Assess. 2022 Jan 22;194(2):115. doi: 10.1007/s10661-022-09749-4.
This research aimed to determine the background and precautionary values of Cd, Cr, Cu, Ni, Pb, Zn, Co, As, and Hg and provide the spatial distribution of these metals in Albania's soils using statistical and geostatistical methods. Since the distribution of the data was commonly not Gaussian, they were transformed into their natural logarithm for deriving background concentrations and precautionary values. Background concentrations were defined as antilog of the median. Precautionary concentration values for soil protection were defined as antilog of 90th percentile of the ln-transformed data. Background concentrations in forest soils were larger compared to those in soils under other land use types. The largest background concentrations for Cd, Cr, Ni, Cu, Co, and Zn were found in forest soils formed on magmatic rocks, while largest concentrations of Pb and Hg were found in soils formed on flysch and molasse. The background values and precautionary concentration values (in brackets) (mg kg) for agricultural soils across flysch/molasses and quaternary deposits were as follows: Cd 0.24 (0.82), Cr 131.63 (527.42), Cu 41.26 (72.75), Ni 287.15 (632.70), Pb 19.11 (284.86), Zn 81.80 (113.90). The largest background values for Cd and Zn were found in Phaeozems, for Cr, Pb, and Co in Luvisols and Cambisols, and for Cu, Hg, and Ni in Fluvisols. The proposed background concentrations and precautionary values complete the picture of metal contents in European soils, can be used as reference concentrations for the Albanian environmental legislation, and allow the identification of potential contamination hot spots.
本研究旨在利用统计和地质统计方法,确定阿尔巴尼亚土壤中 Cd、Cr、Cu、Ni、Pb、Zn、Co、As 和 Hg 的背景和预防值,并提供这些金属在土壤中的空间分布情况。由于数据的分布通常不是正态的,因此将其转换为自然对数以得出背景浓度和预防值。背景浓度定义为中值的反对数。土壤保护的预防浓度值定义为 ln 转换数据第 90 百分位数的反对数。与其他土地利用类型下的土壤相比,森林土壤中的背景浓度更大。Cd、Cr、Ni、Cu、Co 和 Zn 的最大背景浓度出现在火成岩形成的森林土壤中,而 Pb 和 Hg 的最大浓度出现在 flysch 和 molasse 形成的土壤中。跨越 flysch/molasse 和第四纪沉积物的农业土壤的背景值和预防浓度值(括号内)(mg/kg)如下:Cd 0.24(0.82),Cr 131.63(527.42),Cu 41.26(72.75),Ni 287.15(632.70),Pb 19.11(284.86),Zn 81.80(113.90)。Phaeozems 中 Cd 和 Zn 的背景值最大,Luvisols 和 Cambisols 中 Cr、Pb 和 Co 的背景值最大,Fluvisols 中 Cu、Hg 和 Ni 的背景值最大。提出的背景浓度和预防值完善了欧洲土壤中金属含量的图景,可以作为阿尔巴尼亚环境立法的参考浓度,并有助于识别潜在的污染热点。