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Sorption of Th(IV) on Na-rectorite: Effect of HA, ionic strength, foreign ions and temperature

机译:Th(IV)在钠锂蒙脱石上的吸附:HA,离子强度,外来离子和温度的影响

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摘要

The sorption of Th(IV) on Na-rectorite as a function of pH, ionic strength, temperature, soil humic acid (HA) and foreign ions was studied by using a batch technique under ambient conditions, The results indicated that the sorption of Th(IV) on Na-rectorite is strongly depended on pH, ionic strength and temperature. The presence of HA enhanced Th(IV) sorption at low pH and had no obvious effect on Th(IV) sorption at high pH. The sorption of Th(IV) decreased with increasing temperature, indicating that the sorption process of Th(IV) on rectorite was exothermic. Sodium-rectorite and HA were characterized by acid-base titration to obtain the pK(a), and the constant capacitance model (CCM) modeled the sorption data very well with the aid of FITEQL 3.2. HA/Th(IV) addition sequences affected Th(IV) sorption in the ternary systems. The sorption of Th(IV) on Na-rectorite may be dominated by surface complexation, while cation exchange also contributes partly to the sorption. (c) 2007 Elsevier Ltd. All rights reserved.
机译:采用分批技术研究了在锂蒙脱石上Th(IV)的吸附与pH,离子强度,温度,土壤腐殖酸(HA)和外来离子的关系,结果表明Th(IV)的吸附(四)钠锂蒙脱石在很大程度上取决于pH值,离子强度和温度。 HA的存在增强了低pH下Th(IV)的吸附,而对高pH下Th(IV)的吸附没有明显影响。 Th(IV)的吸附量随温度升高而降低,这表明累托石对Th(IV)的吸附过程是放热的。用酸碱滴定法表征锂蒙脱石和HA以获得pK(a),恒电容模型(CCM)借助FITEQL 3.2很好地模拟了吸附数据。 HA / Th(IV)添加顺序影响三元系统中Th(IV)的吸附。钠锂蒙脱石对Th(IV)的吸附可能受表面络合作用的支配,而阳离子交换也部分地促进了吸附。 (c)2007 Elsevier Ltd.保留所有权利。

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