首页> 外文期刊>Geoderma: An International Journal of Soil Science >Heavy metal contamination along a soil transect in the vicinity of the iron smelter of Kremikovtzi (Bulgaria).
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Heavy metal contamination along a soil transect in the vicinity of the iron smelter of Kremikovtzi (Bulgaria).

机译:克雷米科夫齐(保加利亚)铁冶炼厂附近土壤样地上的重金属污染。

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Based on previous preliminary survey results, elevated heavy metal concentrations of the agricultural soils of the villages of the Kremikovtzi region east of the Bulgarian capital Sofia were attributed to pollution from dusts emitted by the iron smelter in the centre of the region. Additional sampling in a test area indicated that high metal concentrations in this area could also be of geogenic origin. In order to test this hypothesis, we sampled a sequence of 14 soil profiles at increasing distance from the smelter along a 2 km transect through agricultural land outside the metallurgical complex of Kremikovtzi. The transect extended through two different units of soil types: Chromic Luvisols and Alluvial Fluvisols. Samples of the fine earth fraction (<2 mm grain size) from various depths were analysed for 19 elements by X-ray fluorescence spectroscopy (XRF). Maximum concentrations of the suspected main pollutants were approximately 170 mg/kg As, 185 mg/kg Pb, and 350 mg/kg Zn. Concentration profiles over depth were distinctly different between the two soil units for most elements and in comparison to this difference varied little within each unit. Within the two units there were no trends with distance to the smelter. The concentration profiles did not indicate any substantial contribution from atmospheric deposition. The enrichment of elemental concentrations relative to Zr did not provide sufficiently conclusive evidence to distinguish anthropogenic from geogenic metal sources. While the ratios of zinc, copper and arsenic to zirconium were almost constant, chromium, nickel and molybdenum ratios to zirconium varied between 2- and 5-fold (primarily showing a decrease) with depth in the majority of profiles, indicating gradients in the original deposition of the soil-forming parent material rather than an anthropogenic source. The study illustrates how important it can be in identifying the origin of soil pollution not only to look into areal distribution patterns of suspected contaminants, but also to investigate their depth profiles as well as that of other elements and to account for pedological factors and their variability..
机译:根据先前的初步调查结果,保加利亚首都索非亚以东的克雷米科夫齐地区村庄的农业土壤中重金属的浓度升高,归因于该地区中心的炼铁厂排放的粉尘造成的污染。在测试区域中进行的其他采样表明,该区域中的高金属浓度也可能是地质成因。为了检验这一假设,我们在距克雷米科夫齐(Kremikovtzi)冶金综合体以外的农田沿2 km断面距离冶炼厂的距离增加的地方,采样了14种土壤剖面。横断面延伸通过两种不同的土壤类型单元:铬黄维素和冲积氟维素。通过X射线荧光光谱法(XRF)分析了来自各个深度的细土级分(粒度小于2 mm)样品的19种元素。可疑主要污染物的最大浓度约为170 mg / kg砷,185 mg / kg铅和350 mg / kg锌。对于大多数元素,两个土壤单元之间的深度浓度曲线明显不同,并且与之相比,每个单元内的浓度差异很小。在两个单元内,到冶炼厂的距离没有趋势。浓度分布图没有表明来自大气沉积的任何实质性贡献。相对于Zr的元素浓度富集没有提供足够的确凿证据来区分人为与地质金属来源。虽然锌,铜和砷与锆的比率几乎恒定,但铬,镍和钼与锆的比率在大多数轮廓中随深度变化了2到5倍(主要是减少),这表明原始梯度形成土壤的母体材料的沉积,而不是人为的来源。这项研究表明,不仅要确定可疑污染物的区域分布模式,而且要调查其深度剖面以及其他要素的深度剖面,并考虑到土壤学因素及其变异性,在识别土壤污染的来源方面有多么重要。 ..

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