Abstract
The paper proposes a simple, accurate, precise, and rapid method for determining the high atomic number (Z) major-element, tantalum (Z = 73), in the rare mineral, columbite [(Fe,Mn) (Nb,Ta)2O6] — tantalite [(Fe,Mn) (Ta,Nb)2O6], by wavelength-dispersive x-ray fluorescence spectrometry (WDXRFS). The other major-element in columbite-tantalite is the lower atomic number niobium (Z = 41). The method uses the characteristic radiation, TaKα, and an LiF 420 analysing crystal, to overcome the problems associated with the serious x-ray spectral-line interference of the secondorder NbKα and NbKβ with the first-order TaLα1 and TaLβ1 respectively.
Samples of columbite-tantalite ground to minus 300 mesh are blended with cellulose in the proportion of 1:1, and pressed powder-pellets are made from 1-g aliquots, with boric acid as a backing. The analytical standards consist of chemically analysed columbite-tantalite containing 5 to 80% by weight of Ta2O5. The instrumental parameters include a rhodium x-ray tube (operating voltage = 100 kV; current = 10 mA), air path, fine collimator (150 μm), and scintillation counter. The counting involves fixed time with three readings of 20s each on the peak and three readings of 20s each on one background.
The accuracy achieved is excellent (within 1.6 to 2.2%), as is the precision (within 0.4 to 2.4%). The time taken for determining Ta2O5 in a batch of twentyfour samples of columbite-tantalite, for a replication of four analyses per sample, by one operator using a manual WDXRF spectrometer, is only five hours.
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Reference
Lister, B. (1986). Re-evaluation of Reference Materials, IGS 21-39. Geostandards News-Letter, v.10, No.2, pp.177–181.
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Viswanathan, S., Chaki, A. & Singh, Y. Wavelength-dispersive x-ray fluorescence spectrometric determination of tantalum in columbite-tantalite using TaKα and an LiF 420 analysing crystal. J Geol Soc India 76, 171–174 (2010). https://doi.org/10.1007/s12594-010-0091-z
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DOI: https://doi.org/10.1007/s12594-010-0091-z