Formation and suppression of AIF(3) during HF digestion of rock samples inTeflon bomb for precise trace element analyses by ICP-MS and ID-TIMS

An aluminum fluoride AlF4 forms during HF digestion of felsic rock sample, for trace element and isotope geochemistry, which use a Teflon bomb at high temperature and pressure. The AlF4 incorporates trace elements (Rb, Sr, Y, Cs, Ba, REE, Pb, Th, and U) and can not be decomposed by conventional meth ods such as evaporation with HClO4. The production of this AlF4 results in lower yields and poor accuracy in analyses of these trace elements by ICP-M S. The formation of AlF4 is controlled by the chemical composition of the r ock samples, in particular, AlF4 does not form during decomposition of the mafic samples with relatively high (Mg+Ca)/Al ratios. We have developed a n ew method to suppress the AlF4 formation, in which excess Mg is added to th e sample prior to acid digestion in the bomb. This new method makes it poss ible to accurately determine the trace element compositions of higher-Al ro ck samples with lower concentrations of Mg and Ca (e.g. rhyolite and granit e). In the trace element analyses by TIMS with isotope dilution techniques (II)-TIMS), AlF4 formation hinders the achievement of isotope equilibrium, resulting in erroneous results. However, the Mg-addition method removed thi s problem by suppression of AlF3 formation.