Trace element determination in alpine snow and ice by double focusing inductively coupled plasma mass spectrometry with microconcentric nebulization

Citation
C. Barbante et al., Trace element determination in alpine snow and ice by double focusing inductively coupled plasma mass spectrometry with microconcentric nebulization, J ANAL ATOM, 14(9), 1999, pp. 1433-1438
Citations number
22
Categorie Soggetti
Spectroscopy /Instrumentation/Analytical Sciences
Journal title
JOURNAL OF ANALYTICAL ATOMIC SPECTROMETRY
ISSN journal
02679477 → ACNP
Volume
14
Issue
9
Year of publication
1999
Pages
1433 - 1438
Database
ISI
SICI code
0267-9477(199909)14:9<1433:TEDIAS>2.0.ZU;2-9
Abstract
Double focusing inductively coupled plasma mass spectrometry (ICP-MS) has b een applied to the direct, simultaneous determination of Ti, V, Cr, Mn, Fe, Co, Cu, Zn, Mo, Ag, Cd, Sb, Ba, Au, Pb, Bi and U in recent Alpine snow and old ice at the ng g(-1) and pg g(-1) level. Small amounts of sample (about 1 ml) were analysed using a microconcentric nebulizer. To avoid possible s pectral interferences, measurements were carried out both in medium (m/Delt a m approximate to 3400) and low (m/Delta m approximate to 300) resolution modes. Clean procedures were adopted both in the field and in the laborator y in order to reduce the possibility of sample contamination to a minimum. Concentration ranges of Alpine surface snow were (in pg g(-1)): Ti (8-106x1 0(3)), V (3-4601), Cr (3-2985), Mn (1-173x10(3)), Fe (67-1058x10(3)), Co (2 -973), Cu (8-29.1x10(3)), Zn (2-6311), Mo (11-721), Ag (0.5-107), Cd (16-21 8), Sb (1.7-6173), Ba (9-36.5x10(3)), Pb (23-33.7x10(3)), Bi (0.1-116) and U (0.1-265). Much lower concentrations were detected in high altitude sites in the Alps. Measurement repeatability, in terms of RSD, ranged between 9 and 34%, depending on the element. The reliability of the analytical method was confirmed by analysis of a certified reference material (SLRS-3, river ine water) and by determination of Cd, Pb, Cu and Zn by ETAAS. For some of the elements investigated these results constitute the first available for recent Alpine snow and old ice.