4.7 Article

Fertilizer P-derived uranium continues to accumulate at Rothamsted long-term experiments

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SCIENCE OF THE TOTAL ENVIRONMENT
卷 820, 期 -, 页码 -

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DOI: 10.1016/j.scitotenv.2022.153118

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Fertilizer-derived uranium; Rothamsted; Soil; Agriculture; Phosphorus

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The application of phosphorus fertilizers leads to the accumulation of uranium in agricultural soils, which is a persistent and global problem. However, the proportion of fertilizer-derived uranium in the soil has not significantly increased over the past 130 years.
The application of phosphorus (P) fertilizers inevitably contributes to the accumulation of trace elements, such as ura-nium (U), in agricultural soils. The fertilizer-derived U accumulation was first reported in Rothamsted Research in 1979. In the present study, we expand this early key research by evaluating the fertilizer-derived U accumulation in topsoil (0-23 cm) from 1876 to the 2010s. We found that total U accumulation rates ranged from 2.8 to 6.1 mu g U kg(-1) yr(-1) at the Broadbalk and Park Grass, respectively, being similar to those observed 40 years ago. This highlights that U accumulation is still an ongoing process in Rothamsted. Fortunately, the proportion of fertilizer-derived U did not significantly increase in the ammonium acetate extractable ('proxy' of plant-available) fraction over 130 years. In addition, we compiled an overview of the global rate of mineral P fertilizer-derived U accumulation in agricultural sys-tems using existing literature (36 experimental trials, from 11 countries). The resulting dataset predicts an estimated mean U accumulation of 0.85 mu g U kg(-1) soil for an annual application of 1 kg P ha(-1) in the topsoil of agricultural sys-tems (0.26 mu g U kg(-1) per kg P ha(-1) for arable land and 1.34 mu g U kg(-1) per kg P ha(-1) for grassland). The annual U accumulation per applied kg P ha(-1) being 0.08 (Broadbalk) and 0.17 mu g U (Park Grass) corresponds to around one-third and one-eighth of the worldwide mean U accumulation for their respective agricultural systems, suggesting 'relatively' low U contents of the applied P fertilizers. Our study underscores that fertilizer-derived U accumulation is a persistent problem on the global scale, even if at different rates, and therewith suggests an evaluation of current regulatory limits and acceptable U input levels from P fertilization.

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