Dybczyński Rajmund S, Kulisa Krzysztof, Pyszynska Marta, Bojanowska-Czajka Anna
Laboratory of Nuclear Analytical Methods, Institute of Nuclear Chemistry and Technology, 03-195 Warszawa, Poland.
Laboratory of Nuclear Analytical Methods, Institute of Nuclear Chemistry and Technology, 03-195 Warszawa, Poland.
J Chromatogr A. 2015 Mar 20;1386:74-80. doi: 10.1016/j.chroma.2015.01.091. Epub 2015 Feb 7.
Separation of Y from other rare earth elements (REE) is difficult because of similarity of its ionic radius to ionic radii of Tb, Dy and Ho. In the new RP-HPLC system with C18 column, tetra-n-butyl ammonium hydroxide (TBAOH) as an ion interaction reagent (IIR), nitrilotriacetic acid (NTA) as a complexing agent at pH=2.8-3.5, and post column derivatization with Arsenazo III, yttrium is eluted in the region of light REE, between Nd and Sm and is base line separated from Nd and Sm and even from promethium. Simple model employing literature data on complex formation of REE with NTA and based on anion exchange mechanism was developed to foresee the order of elution of individual REE. The model correctly predicted that lanthanides up to Tb will be eluted in the order of increasing Atomic Number (At.No.) but all heavier REE will show smaller retention factors than Tb. Concurrent UV/VIS detection at 658nm and the use of radioactive tracers together with γ-ray spectrometric measurements made possible to establish an unique elution order of elution of REE: La, Ce, Pr, Nd, Pm, Y, Sm, Er, Ho, Tm, Yb, Eu, Lu, Dy+Gd, Tb, Sc. The real place of Y however, in this elution series differs from that predicted by the model (Y between Sm and Eu). The method described in this work enables selective separation of Y from La, Ce, Pr, Nd, Pm, Sm and all heavier REE treated as a group.
钇与其他稀土元素(REE)的分离很困难,因为其离子半径与铽、镝和钬的离子半径相似。在采用C18柱的新型反相高效液相色谱(RP-HPLC)系统中,以氢氧化四丁基铵(TBAOH)作为离子相互作用试剂(IIR),氮川三乙酸(NTA)作为络合剂,pH值为2.8 - 3.5,并使用偶氮胂III进行柱后衍生,钇在轻稀土区域,介于钕和钐之间被洗脱,并与钕和钐甚至与钷实现基线分离。利用文献中关于稀土元素与NTA形成络合物的数据并基于阴离子交换机制,开发了一个简单模型来预测各稀土元素的洗脱顺序。该模型正确预测了直到铽的镧系元素将按原子序数递增的顺序被洗脱,但所有比铽重的稀土元素的保留因子都将比铽小。在658nm处同时进行紫外/可见检测,并使用放射性示踪剂以及γ射线光谱测量,得以确定稀土元素独特的洗脱顺序:镧、铈、镨、钕、钷、钇、钐、铒、钬、铥、镱、铕、镥、镝 + 钆、铽、钪。然而,钇在这个洗脱序列中的实际位置与模型预测的不同(钇在钐和铕之间)。本文所述方法能够从镧、铈、镨、钕、钷、钐以及所有被视为一组的比钐重的稀土元素中选择性分离出钇。