J. Stix et al., A CRITICAL-LOOK AT QUANTITATIVE LASER-ABLATION ICP-MS ANALYSIS OF NATURAL AND SYNTHETIC GLASSES, Canadian Mineralogist, 33, 1995, pp. 435-444
In this paper, we examine techniques and problems of quantitative lase
r-ablation ICP-MS analysis for natural and synthetic glass samples and
discuss internal standardization, use of calibration curves, and sing
le-standard calibration. Internal standards are used to normalize raw
intensities and ate generally a low-abundance isotope of a major eleme
nt in the samples. For zoned minerals, internal standards are used tha
t show small compositional variations. Calibration curves are necessar
y to define the ICP-MS response over a range of concentrations and are
constructed using a series of geochemical reference standards of simi
lar composition to the unknown materials to be analyzed. A series of c
alibration curves for mafic-ultramafic acid felsic glasses are present
ed, which generally show linear behavior. However, Zr, Y, and Ce calib
rations are nonlinear and exhibit higher relative intensities for thes
e elements at higher concentrations, This nonlinearity may be the resu
lt of (1) large ranges in concentrations or (2) matrix effects involvi
ng iron and total trace-element content in the glasses. Calibrations u
sing a single geochemical reference standard can be attempted only if
the calibration curves are linear and pass through the origin, and if
the reference standard and the samples have similar compositions.