D. Harris et al., CONTINUOUS-FLOW ISOTOPE RATIO MASS-SPECTROMETRY OF CARBON-DIOXIDE TRAPPED AS STRONTIUM CARBONATE, Communications in soil science and plant analysis, 28(9-10), 1997, pp. 747-757
The isotopic signal provided by differential discrimination against at
mospheric carbon dioxide ((CO2)-C-13) by C-3 and C-4 plant photosynthe
tic pathways is being widely used to study the processes of carbon (C)
fixation, soil organic matter formation, and mineralization in nature
. These studies have been facilitated by the availability of automated
C and nitrogen (N) combustion analyzers (ANCA) combined with continuo
us flow isotope ratio mass spectrometers (CFIRMS). Analysis of (CO2)-C
-13, in these instruments requires consistent sample mass for best pre
cision, a requirement that is easily satisfied for soil and tissue sam
ples by adjusting sample weight. Consistent CO2 sample size is much mo
re difficult to achieve using gas handling systems for samples of head
space gases when CO2 concentrations vary widely. Long storage of gaseo
us samples also is difficult. Extended respiration studies are most ea
sily conducted by trapping CO2 in alkali and conversion to an insolubl
e carbonate. Thermal decomposition of the carbonate in an on-line ANCA
allows consistent and optimal CO2 sample mass to be obtained. The use
of precipitated carbonates also facilitates storage of samples and en
ables full automation of sample analysis using an ANCA interfaced to a
CFIRMS. Calcium (Ca), strontium (Sr), and barium (Ba) carbonates were
tested. Strontium carbonate (SrCO3) with the addition of vanadium pen
toxide (V2O5) as a combustion catalyst was found most suitable.