TCF selenium preconcentration in geological materials for determination at sub-mugg(-1) with INAA (Se/TCF-INAA).
In geological samples, Se concentration ranges from 1x10(-9)gg(-1) up to 1x10(-3)gg(-1). The analytical difficulty at low concentration (<1mugg(-1)), is one of the main reasons why the geological cycle of Se is poorly known. The analytical method that consisted of preconcentration of Se with thiol cotton fiber (TCF) followed by graphite furnace atomic absorption spectrometry (GFAAS) has been modified by finishing with instrumental neutron activation analysis (INAA). The modified technique involves sample dissolution (HF-HNO(3)-H(2)O(2)) and evaporation to dryness at low temperature (55-60 degrees C) to avoid selenium volatilization. Se(VI) is converted to Se(IV) by adding 6M HCl to the dry residuum and the solution is then heated in a covered boiling bath (95-100 degrees C). The solution is diluted to obtain 0.6M HCl and then collected on TCF. The TCF is placed in a polyethylene vial for irradiation in the SLOWPOKE II reactor (Montréal) for 30s at a neutron flux of 10(15)m(-2)s(-1). The 162keV peak of (77m)Se (half-life 17.36s) is read for 20s after a decay of 7s. The amount of sample to be dissolved is controlled by two competing effects. To obtain low detection limits, a larger amount of sample should be dissolved. On the other hand, the TCF could become saturated with chalcophile elements when large sample is used. Sulfur is a good indicator of the amount of Se and chalcophile elements present. In S poor sample (<100mugg(-1)) 3.0g of sample was used and the L(D) was approximately 2ngg(-1). In S high samples (>1.5% S) 0.05g of sample was used and the L(D) was approximately 120ngg(-1). The present work also includes suggested Se concentration for eight international geological reference materials (IGRM) that compare favorably with literature values.
Savard
Dany
D
Sciences de la Terre, Université du Québec à Chicoutimi, Chicoutimi, Que., Canada G7H 2B1.
Paul Bédard
L
L
Barnes
Sarah-Jane
SJ