Rare-earth ores (monazite, ion-adsorption type and xenotime) were analyzed using a coupled analytical method, isotachophoresis-particle induced X-ray emission (ITP-PIXE). The detection limit for each minor rare-earth element in the ores was ca. 0.01 mass% of the total rare-earth elements (TREE), when 200 µg of monazite was analyzed. Since yttrium was the major component in ion-adsorption type and xenotime ores, the use of a leading electrolyte containing a-hydroxyisobutyric acid and tartaric acid as complexing agents was effective for the separation of yttrium ion from lanthanide ions.
KeywordsRare-earth element, isotachophoresis, particle induced X-ray emission (PIXE), isotachophoresis-PIXE The analysis of rare-earth ores, which include fourteen lanthanide elements and yttrium with very different abundances, is one of the difficult problems for any analytical method. Especially when the minor components in the ores are analyzed, an accurate analysis may be disturbed by inherent disadvantages of the employed method, for example, spectrum interference in atomic emission spectroscopy, isotope interference in mass spectroscopy and a matrix effect in X-ray analysis.In such instances chromatographic analysis may be useful. However, since the separation column used for analytical chromatography is easily overloaded, a large amount of sample can not be applied. Therefore, the detection method should be sufficiently sensitive to analyze minor components in the applied sample. As long as conventional detection methods are used, however, the necessary sensitivity is not always available. A coupled analytical method for rare-earth ores, HPLC-ICP-AES, as reported by Yoshida and Haraguchi', is one possible solution, where ICP-AES plays the role of an HPLC detector with high sensitivity and discriminating ability.On the basis of the same strategy, we have developed isotachophoresis-particle induced X-ray emission (ITP-P1XE). Ionic components in a sample solution are first preconcentrated and separated by ITP, and zones of the separated components are fractionated utilizing the counterflow of a leading electrolyte. Dropwise fractions are then analyzed off-line by PIXE. By using this coupled method, a crude rare-earth chloride from monazite ore2 and a model solution of high-level waste from the nuclear fuel cycle3,4 were analyzed with high accuracy.The leading electrolyte used contained a-hydroxyisobutyric acid (HIB) as the complex-forming agent. The separation of fourteen lanthanide ions using the electrolyte is one of the typical applications of ITP.5,6 However, since Y and Dy could not be separated by using the electrolyte, ITP was not useful for analyzing rareearth ores containing both Y and Dy. In order to improve this defect we have recently developed a new leading electrolyte by adding tartaric acid to the previous leading electrolyte as a helping complexing agent.' This paper aims to confirm the utility of the abovementioned electrolyte system in the analysis of rare-earth ores containing Y as one of the major component...