Distribution, behavior, and erosion of uranium in vineyard soils

被引:3
|
作者
Campos, Daniel A. [1 ]
Blanche, Sophia [1 ,2 ]
Jungkunst, Hermann F. [2 ]
Philippe, Allan [1 ]
机构
[1] Univ Koblenz Landau, Inst Environm Sci, iES Landau, Grp Environm & Soil Chem, Fortstr 7, D-76829 Landau In Der Pfalz, Germany
[2] Univ Koblenz Landau, Inst Environm Sci, iES Landau, Grp Geoecol & Phys Geog, Fortstr 7, D-76829 Landau In Der Pfalz, Germany
关键词
Mobility; Phosphate fertilizers; Viticulture; Colloidal transport; Soil structure; Prediction; ORGANIC-MATTER; TRANSPORT; COLLOIDS; ACCUMULATION; SORPTION; FLOW; RADIONUCLIDES; NANOPARTICLES; INFILTRATION; CONTAMINANTS;
D O I
10.1007/s11356-021-14381-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Phosphate fertilization contributes to an input of uranium (U) in agricultural soils. Although its accumulation and fate in agricultural soils have been previously studied, its colloidal transport and accumulation along slopes through erosion have been studied to a lesser extent in viticulture soils. To bridge this gap, the contents and potential mobility of U were investigated in vineyard model soils in the Rhineland-Palatinate region, Germany. In addition to elevated U contents, U was expected to associate with colloids and subject to erosion, thus accumulating on slope foots and in soils with fine structure, and reflecting a greater variability. Moreover, another expectation was the favorable erosion/mobility of U in areas with greater carbonate content. This was tested in three regional locations, at different slope positions and through soil horizon depths, with a total of 57 soil samples. The results show that U concentrations (0.48-1.26 ppm) were slightly higher than proximal non-agricultural soils (0.50 ppm), quite homogenous along slope positions, and slightly higher in topsoils. Assuming a homogeneous fertilization, the vertical translocation of U in soil was most probably higher than along the slope by erosion. In addition, carbonate content and soil texture correlated with U concentrations, whereas other parameters such as organic carbon and iron contents did not. The central role of carbonate and soil texture for the prediction of U content was confirmed using decision trees and elastic net, although their limited prediction power suggests that a larger sample size with a larger range of U content is required to improve the accuracy. Overall, we did not observe neither U nor colloids accumulating on slope foots, thus suggesting that soils are aggregate-stable. Lastly, we suggested considering further soil parameters (e.g., Ca2+, phosphorus, alkali metals) in future works to improve our modelling approach. Overall, our results suggest U is fortunately immobile in the studied locations.
引用
收藏
页码:53181 / 53192
页数:12
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