Headspace solid phase microextraction – GC/C-IRMS for δ13CVPDB measurements of mono-aromatic hydrocarbons using EA-IRMS calibration
This work aims at comparing the δ13CVPDB of mono-aromatic hydrocarbons benzene, toluene, ethylbenzene and xylene isomers (BTEX) measured by elemental analyser (EA)-isotope ratio mass spectrometer (IRMS) with the δ13CVPDB measured on the same compounds by headspace solid phase microextraction – GC/C-IRMS (hSPME – GC/C-IRMS) with the final goal of using these compounds as internal standards on the latter system. The EA-IRMS measurements were done using calcium and lithium carbonate isotopic reference materials: NBS19 and L-SVEC for establishing the δ13CVPDB scale. The EA-IRMS measurements with helium dilution of a set of five reference materials (USGS40, USGS41, IAEA-CH-6, IAEA-CH-3 and IAEA-601) show systematic bias of 1‰ relative to their assigned values. This bias due to the dilution mechanism in the used ConfloII interface device could not be avoided. As the selected hydrocarbons: BTEX could not be analysed by EA-IRMS without helium dilution, their δ13CVPDB must be corrected from this observed bias using an external calibration. The CO2 gas calibrated using EA-IRMS without helium dilution, was used as an in-house reference for the δ13CVPDB measurements of the BTEX by the hSPME – GC/C-IRMS system. The comparison made between the δ13CVPDB measured on the same BTEX compounds by EA-IRMS (with external calibration) and by hSPME – GC/C-IRMS techniques showed good agreement.
Present-Day Radiocarbon Content of Select Flavoring Compounds Reveals Vanillin Production Pathway
Radiocarbon and stable isotope determination in foods, flavors, and beverages, for the authentication of source material and process of formation, is a well-established method of identity used in industry. New methods of provenance determination, using stable isotopes of oxygen and hydrogen, have added to the host of other isotopic methods used for characterizing natural or botanically derived products. The unambiguous determinant of a product's fossil fuel origin be it from petroleum, natural gas, or coal, is through the measurement of its 14C content. The 14C content can also be used to determine the fraction dilution of recently grown and harvested material with that derived from fossil fuel, and even confirms the vintage of agricultural products based on the well-established decrease of bomb-produced atmospheric 14C. This paper documents 14C measurements at the University of Georgia's Center for Applied Isotope Studies accelerator mass spectrometry and stable isotope laboratories, over the last 3 yr, for 10 important flavoring compounds. By establishing an accurate and current level of 14C in botanically derived products, we were able to confirm a particular source for vanilla production, the most popular consumer flavor in the marketplace. Over the years, vanilla extract has been produced less and less from vanilla beans (Vanilla planifolia), particularly those from Madagascar and the Comoros Islands, and more from other botanical precursors such as ferulic acid, clove oil, and guaiacol. We report isotopic data to support this precursor for vanilla production based on high 14C levels accumulated during the tree's life, incorporated in the tree rings and their associated stable isotope abundances.
Forensic Studies by EA-IRMS.
Abstract The authenticity of natural and synthetic matter can be checked by measurement of the isotope ratios of C, N and S. Controlled substances like drugs of abuse (cocaine, heroin) and explosives (TNT) or, simply, traces of paint can hold information in their isotope pattern. Total combustion of samples in an elemental analyzer followed by on-line determination of the isotopes of the combustion products (CO(2), N(2), SO(2)) in an isotope ratio mass spectrometer (EA-IRMS) provides high sample throughout with a minimum of sample preparation.