1. Determination of 16O and 18O abundance ratios in natural carbon dioxide reservoirs
- Author
-
M. Schidlowski and A. Zyakun
- Subjects
Isotope ,Chemistry ,δ18O ,Analytical chemistry ,Mineralogy ,chemistry.chemical_element ,Condensed Matter Physics ,Mass spectrometric ,Oxygen ,Isotopes of oxygen ,chemistry.chemical_compound ,Homogeneous ,Abundance (ecology) ,Carbon dioxide ,Physical and Theoretical Chemistry ,Instrumentation ,Spectroscopy - Abstract
A mathematical formalism is presented that, based on the relative proportions of the 18O/16O-distinctive CO2 species C16O2, C16O18O, and C18O2 in a given CO2 pool, allows the calculation of 18O/16O ratios for the two different oxygen positions in the CO2 molecules of this particular pool. The quantities of the isotopically distinctive CO2 species can be determined as mass peak intensities 44I (for C16O2), 46I (for C16O18O), and 48I (for C18O2) by suitable adaptations of conventional mass spectrometric techniques. The δ18O(1,2) values obtained for each of the above positions furnish information as to either a probabilistic (“homogeneous”; with δ18O(1)=δ18O(2)) or a nonprobabilistic (“nonhomogeneous”) 18O/16O distribution (with δ18O(1)≠δ18O(2)) in the respective CO2 pool. Using δ18O(1,2), we may consequently obtain information pertaining to the oxygen sources of the CO2 molecules in the pool as well as to reservoir changes reflected by differential diffusion rates of the isotopically distinctive CO2 species that have left and entered the reservoir. This approach may become potentially important for an assessment of the sources and the reservoir dynamics of the atmospheric CO2 pool. Keywords: Carbon dioxide; oxygen isotopes; isotope variation measurements; mathematical modeling
- Published
- 2000