Determination of trace zirconium and hafnium in basaltic rocks by inductively coupled plasma atomic emission spectrometry after chemical separation: an evaluation of two methods based on extraction chromatography

Authors
Citation
Xj. Yang et C. Pin, Determination of trace zirconium and hafnium in basaltic rocks by inductively coupled plasma atomic emission spectrometry after chemical separation: an evaluation of two methods based on extraction chromatography, ANALYST, 125(3), 2000, pp. 453-457
Citations number
31
Categorie Soggetti
Chemistry & Analysis","Spectroscopy /Instrumentation/Analytical Sciences
Journal title
ANALYST
ISSN journal
00032654 → ACNP
Volume
125
Issue
3
Year of publication
2000
Pages
453 - 457
Database
ISI
SICI code
0003-2654(2000)125:3<453:DOTZAH>2.0.ZU;2-0
Abstract
The determination of Zr and Hf in basaltic rocks by inductively coupled pla sma atomic emission spectrometry after extraction chromatographic separatio n is reported. Two different approaches were employed using tricaprylylmeth ylammonium chloride (Aliquat 336) and N-benzoyl-N-phenylhydroxylamine (BPHA ) as stationary phases supported on inert porous polymeric substrates. The major advantages of the separation schemes are simplicity and the easy sepa ration of Zr and Hf from Ti, a major element in rocks. The BPHA approach is superior to the Aliquat 336 approach with regard to sample preparation and separation conditions. The method yields detection limits of 0.02 and 0.07 mu g g(-1) for Zr and Hf, respectively. The analytical results for interna tional reference rock materials (BIR-1, W-2, BHVO-1) showed excellent agree ment with literature values obtained by spark source mass spectrometry and inductively coupled plasma mass spectrometry. The relative standard deviati ons were in the range 2-4% for the samples analysed.