Abst'/> Uranium in agricultural soils and drinking water wells on the Swiss Plateau
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Uranium in agricultural soils and drinking water wells on the Swiss Plateau

机译:瑞士高原农业土壤和饮用水井中的铀

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AbstractMineral phosphorus fertilizers are regularly applied to agricultural sites, but their uranium (U) content is potentially hazardous to humans and the environment. Fertilizer-derived U can accumulate in the soil, but might also leach to ground-, spring and surface waters. We sampled 19 mineral fertilizers from the canton of Bern and soils of three arable and one forest reference sites at each of four locations with elevated U concentrations (7–28 μg L−1) in nearby drinking water wells. The total U concentrations of the fertilizers were measured. The soils were analysed at three depth intervals down to 1 m for general soil parameters, total Cd, P, U and NaHCO3-extractable U concentrations, and234/238U activity ratios (AR). The U concentrations and AR values of the drinking water samples were also measured. A theoretical assessment showed that fertilizer-derived U may cause high U concentrations in leaching waters (up to approx. 25 μg L−1), but normally contributes only a small amount (approx. 0–3 μg L−1). The arable soils investigated showed no significant U accumulation compared to the forest sites. The close positive correlation of AR with NaHCO3-extractable U (R = 0.7, p < 0.001) indicates that application of fertilizer can increase the extractable U pool. The lack of depth gradients in the soil U concentrations (1.5–2.7 mg kg−1) and AR (0.90–1.06) ratios are inconsistent with the accumulation of U in the surface soil, and might indicate some leaching of fertilizer-derived U. The AR values in the water samples were close to 1, possibly suggesting an influence of fertilizer-derived U. However, based on findings from the literature and considering the heterogeneity of the catchment area, the agricultural practices, and the comparatively long distance to the groundwater, we conclude that fertilizer-derived U makes only a minor contribution to the elevated U concentrations in the water samples.Graphical abstractDisplay OmittedHighlightsMineral P fertilizers contain high U concentrations.Mineral fertilization could cause high U concentrations in waters.The concentration of extractable U is linked to mineral fertilizer application.No accumulation in the surface soil might indicate partial leaching of U.Fertilizer-derived U is probably only of minor importance for water concentrations.Mineral fertilizer application causes an increase of NaHCO3-extractable U in soil, and might significantly contribute to U concentrations in waters at background levels, but is probably only a minor contributor at high U concentrations in the waters of the Swiss Plateau.
机译: 摘要 矿物质磷肥经常用于农业场所,但其铀(U)含量可能对人类和环境构成危害。源自肥料的铀可以在土壤中积累,但也可能会渗入地下水,泉水和地表水中。我们从伯尔尼州采样了19种矿物肥料,并在四个U浓度较高的位置(7–28μgL − 1 )在附近的饮用水井中。测量了肥料中的总U浓度。在三个深度间隔(低至1 m)下分析土壤的一般土壤参数,总Cd,P,U和NaHCO 3 可提取的U浓度以及 234/238 U活性比(AR)。还测量了饮用水样品中的U浓度和AR值。理论评估表明,源自肥料的U可能会在浸出水中引起较高的U浓度(最高约25μgL -1 ),但通常仅造成少量(约0–3μgL -1 )。与森林地点相比,调查的可耕土壤没有显着的U积累。 AR与NaHCO 3 可提取的U的紧密正相关(R = 0.7,p <0.001)表明肥料的施用可以增加可提取的U池。土壤U浓度(1.5–2.7 mg kg − 1 )和AR(0.90–1.06)比率缺乏深度梯度与U的积累不一致在表层土壤中,并且可能表明有肥料浸出的U浸出。水样品中的AR值接近于1,可能暗示了肥料浸出的U的影响。但是,基于文献的发现并考虑了异质性在集水区,农业实践以及距地下水相对较长的距离方面,我们得出结论,源自化肥的铀对水样中铀浓度升高的贡献很小。 图形摘要 省略显示 突出显示 矿物磷肥中U含量高。 矿物施肥可能会导致水中高浓度的铀。 可萃取铀的浓度与矿物肥料的施用有关。 < ce:list-item id =“ u0025”> N o表层土壤中的积累可能表明U的部分浸出。 源自肥料的U可能对水的浓度只具有较小的重要性。 < ce:simple-para id =“ abspara0025” view =“ all”>施用矿物肥料会导致土壤中NaHCO 3 可提取的U的增加,并且可能显着增加有助于在背景水平的水中的U浓度,但是在瑞士高原的水中,在高U浓度下可能只是次要贡献者。

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