Production of artifact methylmercury during the analysis of certified reference sediments: use of ionic exchange in the sample treatment step to minimise the problem.
Production of artifact methylmercury (MeHg(+)) during the analysis of two certified reference sediments, CRM-580 and IAEA-405, was investigated. Leaching of the analyte from the solid sample was achieved by ultrasound assisted acidic extraction. The aqueous leachate was either ethylated (NaBEt(4)) or phenylated (NaBPh(4)) using acetic/acetate or citric/citrate to buffer the solution. Preconcentration of the volatile compounds was carried out by extraction with an organic solvent (n-hexane) or solid phase microextraction (SPME). MeHg(+) was finally separated and detected by gas chromatography with atomic emission or mass spectrometry detection (GC-MIP-AED or GC-MS). In all the cases the concentrations obtained for MeHg(+) in the CRM-580 were significantly higher than the certified value. For the IAEA-405, however, the MeHg(+) concentration found was always statistically indistinguishable from the certified value. Experiments were also conducted with synthetic samples, such as aqueous mixtures of MeHg(+) and inorganic mercury (Hg(2+)) or silica-gel spiked with both compounds. The methylation rates found (defined as the percentage of Hg(2+) present in the sample which methylates to give artifact MeHg(+)) ranged from not observable (in certain synthetic aqueous mixtures) to 0.57% (analysis of CRM-580 under certain conditions). As the amount of Hg(2+) available in the sample seems to be the main factor controlling the magnitude of the artifact, several experiments were conducted using an ionic exchange resin (Dowex M-41) in order to minimise the concentration of this chemical in the reaction medium. First, a hydrochloric leachate of the sample was passed through a microcolumn packed with the exchanger. Second, the resin was mixed with the sample prior to extraction with HCl. In both cases, the predominant Hg(2+) species, HgCl(4)(2-), was adsorbed on the resin, whereas MeHg(+), mainly as MeHgCl, remained in solution. Following the second option, a new method to analyse MeHg(+) in conflictive matrices like certain sediments was proposed. This approach produced better results for the CRM-580, but a MeHg(+) concentration slightly, but statistically significant, higher than the reference value was still obtained.
Delgado
Alejandra
A
Kimika Analitikoa Saila, Euskal Herriko Unibertsitatea, 644 P.K., E-48080 Bilbao, Spain.
Prieto
Ailette
A
Zuloaga
Olatz
O
de Diego
Alberto
A
Madariaga
Juan Manuel
JM
D016477:Artifacts; D008401:Gas Chromatography-Mass Spectrometry; D019015:Geologic Sediments / Q000737:chemistry*; D006863:Hydrogen-Ion Concentration; D008767:Methylmercury Compounds / Q000032:analysis*; D012016:Reference Values
D008767:Methylmercury Compounds