Boron Determination in Twenty One Silicate Rock Reference Materials by Isotope Dilution ICP‐MS

Abstract

The concentration of boron was determined in twenty one geochemical reference materials (silicate rocks) by isotope dilution inductively coupled plasma‐mass spectrometry. Boron was extracted from the rocks using HF digestion, suppressing boron volatilisation through boron‐mannitol complexation. Sample solutions, in a diluted HCl matrix, were analysed by ICP‐MS without any separation of boron from the matrix elements. The results obtained were in agreement with the literature data and indicate that using the described procedure, trace amounts of boron can be very easily determined in complex matrices with rapidity and precision. With the instrumentation and reagents used in this study, this procedure can be used for the determination of 0.5 μg g−1 boron in a 15 0 mg silicate rock sample. Replicate analyses of the twenty one geochemical reference materials (GRM), ranging in boron concentration from 1.35 to 15 7 μg g−1, yielded precisions (relative standard deviation) varying between 0.9 and 9.8%.