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
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.