首页> 外文期刊>Journal of Radioanalytical and Nuclear Chemistry >The sorption of Eu(III) on calcareous soil: effects of pH, ionic strength, temperature, foreign ions and humic acid
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The sorption of Eu(III) on calcareous soil: effects of pH, ionic strength, temperature, foreign ions and humic acid

机译:钙质土壤对Eu(III)的吸附:pH,离子强度,温度,外来离子和腐殖酸的影响

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摘要

The sorption of Eu(III) on calcareous soil as a function of pH, humic acid (HA), temperature and foreign ions was investigated under ambient conditions. Eu(III) sorption on soil was strongly pH dependent in the observed pH range. The effect of ionic strength was significant at pH 8. The type of salt cation used had no visible influence on Eu(III) uptake on soil, however at low pH values, the influence of anions was following the order: Cl− ≈ NO3 − > ClO4 −. In the presence of HA, the sorption edge obviously shifted about two pH units to the lower pH, whilst in range of pH 6–7, the sorption of Eu(III) decreased with increasing pH because a considerable amount of Eu(III) was present as humate complexes in aqueous phase, then increased again at pH > 11. The results indicated that the sorption of Eu(III) on soil mainly formed outer-sphere complexes and/or ion exchange below pH ~7; whereas inner-sphere complexes and precipitation of Eu(OH)3(s) may play main role above pH ~8.
机译:在环境条件下研究了Eu(III)在石灰性土壤上的吸附随pH,腐殖酸(HA),温度和外来离子的变化。在观察到的pH范围内,Eu(III)在土壤上的吸附强烈依赖于pH。在pH值为8时,离子强度的影响显着。所用盐阳离子的类型对土壤中Eu(III)的吸收没有明显影响,但是在低pH值下,阴离子的影响顺序如下:Cl - ≈NO 3 - 4 -。在存在HA的情况下,吸附边缘明显移至较低pH约两个pH单位,而在pH 6–7范围内,Eu(III)的吸附随pH的升高而降低,因为大量的Eu(III)被吸附。在水相中以腐殖酸盐配合物形式存在,然后在pH> 11时再次增加。结果表明,Eu(III)在土壤上的吸附主要是在pH〜7以下形成外球络合物和/或离子交换。在pH〜8以上,内球络合物和Eu(OH) 3 的沉淀可能起主要作用。

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