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首页> 外文期刊>The Korean journal of chemical engineering >Adsorption Behavior of Aqueous Europium on Kaolinite under Various Disposal Conditions
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Adsorption Behavior of Aqueous Europium on Kaolinite under Various Disposal Conditions

机译:不同处理条件下Euro在高岭石上的吸附行为

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This work investigated the adsorption behavior of europium on kaolinite under various disposal conditions. Batch-wise adsorption and precipitation experiments and equilibrium model calculations were performed over a pH range of 4-10 and CO_2 concentration range of 0%, 0.03%, and 10%. Experimental precipitation behaviors are in agreement with the results of equilibrium model calculations using the geochemical code MINTEQA2. Aqueous species of Eu~(3+) exists mainly at pH 5 or below and solid phases of Eu(OH)_3(s), Eu(OH)CO_3(s), and Eu_2(CO_3)_3·3H_2O(s) are formed at higher pH ranges. Adsorption behavior of Eu on kaolinite in the low pH range can be explained by interlayer ion-exchange reaction. The significant increase in adsorbed amount at pH 5-6 is due to the surface complexation at the edge site of kaolinite. In the high pH range, precipitation of Eu contributes mainly to the adsorption quantity. The rapid decrease in adsorbed amount above pH 7 under 10% CO_2 condition occurs by the formation of anionic europium species of Eu(CO_3)_2~-. The adsorption of Eu on kaolinite could be well interpreted by the Freundlich adsorption isotherm. The data except for the highest equilibrium concentration ranges were also explained by Langmuir isotherm and the maximum adsorbed quantity of Eu on kaolinite, b, is 1.2 mg/g.
机译:这项工作研究了various在各种处理条件下对高岭石的吸附行为。在4-10的pH范围和0%,0.03%和10%的CO_2浓度范围内进行了分批吸附和沉淀实验以及平衡模型计算。实验降水行为与使用地球化学代码MINTEQA2进行的平衡模型计算结果一致。 Eu〜(3+)的水相主要存在于pH 5或以下,Eu(OH)_3(s),Eu(OH)CO_3(s)和Eu_2(CO_3)_3·3H_2O(s)的固相为在较高的pH范围内形成。在低pH范围内Eu在高岭石上的吸附行为可以通过层间离子交换反应来解释。 pH 5-6下吸附量的显着增加是由于高岭石边缘部位的表面络合。在高pH范围内,Eu的沉淀主要是对吸附量的贡献。在10%CO_2条件下,pH 7以上时,吸附量的迅速减少是由于Eu(CO_3)_2〜-阴离子euro的形成。 Freundlich吸附等温线可以很好地解释Eu在高岭石上的吸附。 Langmuir等温线也解释了除最高平衡浓度范围外的数据,Eu在高岭石上的最大吸附量b为1.2 mg / g。

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