Determination of sub-parts-per-trillion levels of rare earth elements in natural waters by inductively coupled plasma time-of-flight mass spectrometry after flow injection on-line sorption preconcentration in a knotted reactor

Citation
K. Benkhedda et al., Determination of sub-parts-per-trillion levels of rare earth elements in natural waters by inductively coupled plasma time-of-flight mass spectrometry after flow injection on-line sorption preconcentration in a knotted reactor, J ANAL ATOM, 16(9), 2001, pp. 995-1001
Citations number
30
Categorie Soggetti
Spectroscopy /Instrumentation/Analytical Sciences
Journal title
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
ISSN journal
02679477 → ACNP
Volume
16
Issue
9
Year of publication
2001
Pages
995 - 1001
Database
ISI
SICI code
0267-9477(200109)16:9<995:DOSLOR>2.0.ZU;2-8
Abstract
A flow injection (FI) on-line sorption system, for the preconcentration and separation in a knotted reactor (KR), is coupled with inductively coupled plasma time-of-flight mass spectrometry (ICP-TOFMS) for the fast, selective and sensitive determination or ultra-trace concentrations of rare earth el ements (REEs) in environmental waters. The on-line preconcentration and sep aration of the REEs is achieved by sorption of the REE complexes formed in the pH range 3.7-4.6 on the inner walls of a (300 cm x 0.5 mm) PTFE KR prec oated with the chelating reagent 1-phenyl-3-methyl-4-benzoylpyrazol-5-one ( PMBP) at a pH of 9.6. The analytes are eluted and transported to the ICP-TO FMS system with 2% (v/v) HNO3 containing 0.5 mug l(-1) of Rh and In as inte rnal standards, using ultrasonic nebulisation. The REEs are effectively pre concentrated and separated from the major matrix constituents-alkali and al kaline earth elements. Of particular significance is their separation from barium, which produces considerable isobaric interferences on some of the a nalytes. Using a preconcentration time of 30 s and a sample flow rate of 4. 4 ml min(-1), enhancement factors of 15 to 22 for the different REES are ac hieved. The detection limits (3 sigma) range from 3 to 40 pg l(-1). The pre cision for 9 replicate determinations of 0.1 mug l(-1) of each analyte is b etter than 5% (RSD). The accuracy of the method is demonstrated by the anal ysis of environmental waters and by recovery measurements on spiked samples .