L. Halicz et al., Determination of the U-234/U-238 ratio in water samples by inductively coupled plasma mass spectrometry, ANALYT CHIM, 422(2), 2000, pp. 203-208
U-234 belongs to the U-238 natural radioactive decay series, and at equilib
rium, the abundance ratio, U-234/U-238, corresponds to the ratio of their h
alf-lives, i.e. 54.8 x 10(-6). In natural waters, deviations from this rati
o reflect radioactive and geochemical processes and can be correlated with
the flow path of the water. Alpha spectrometry or thermal ionization mass s
pectrometry require tedious procedures for separation and preconcentration
of the uranium prior to analysis. Inductively coupled plasma quadrupole mas
s spectrometry can yield reliable results for the U-234/U-238 ratio without
any treatment of the sample (except acidification). Here, we show that com
bining a flow-injection sample introduction system with an ultrasonic nebul
izer, significantly increases the sensitivity and enhances the ability to c
ope with a relatively high salt content in non-saline water samples. The re
lative standard deviation attained is 5% at 50 pg l(-1) U-234. The method i
s extremely fast (1 min per measurement); pre-treatment is not required and
1 ml of the sample is needed for triplicate measurements. Therefore, it ma
y be used as a fast screening method. (C) 2000 Elsevier Science B.V. All ri
ghts reserved.