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Effect of nutrient uptake by plant roots on the fate of REEs in soil

机译:植物根系吸收养分对土壤稀土元素命运的影响

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摘要

Concentrations of rare earth elements (REEs) and major ions in soil solutions were observed under different growth stages of soybean in order to evaluate the effect of nutrient uptake by plant roots on the mobility of REEs in soil-plant systems. Soybean plants were grown in pots, which were kept in a greenhouse for 84 days. The concentrations of major nutrient cations (K and Ca) in the soil solution decreased with the soybean growth. On the other hand, the concentrations of Al, Y, La, Ce, Nd, Gd, Dy, Er and Yb increased. Although no decrease of pH was observed, it was assumed that the REEs and Al were dissolved from the soil solid phase due to H~+ release from the plant roots for K~+ and Ca~(2+ )uptake. Subsequently, the bioaccumulation of REEs in the soybean roots was observed in the maturing stage of the soybean. These results showed that the soybean roots could enhance the dissolution of REEs from the soil solid phase and they could also accumulate REEs through plant growth.
机译:为了评估植物根系吸收养分对稀土在土壤-植物系统中迁移率的影响,观察了大豆不同生长阶段土壤溶液中稀土元素(REEs)和主要离子的浓度。大豆植物在花盆中生长,并在温室中放置84天。土壤溶液中主要营养阳离子(K和Ca)的浓度随大豆的生长而降低。另一方面,Al,Y,La,Ce,Nd,Gd,Dy,Er和Yb的浓度增加。尽管未观察到pH的降低,但可以认为由于K〜+和Ca〜(2+)的吸收,由于植物根部释放的H〜+,REE和Al从土壤固相中溶解了。随后,在大豆的成熟阶段观察到大豆根中REE的生物积累。这些结果表明,大豆根可以增强土壤固相中稀土元素的溶解,并且还可以通过植物的生长来积累稀土元素。

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