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UC Davis Plant Sciences


Carbon Dioxide (CO2) & Methane (CH4) Analysis by Trace Gas-IRMS

The SIF provides δ13C isotope analysis of CH4 and CO2 gases in headspace vials using a Thermo Scientific GasBench-PreCon trace gas system interfaced to a Delta V Plus IRMS.

 

Analysis of 13C in Carbon Dioxide

Stable isotope ratios of δ13C in carbon dioxide are measured using a ThermoScientific PreCon-GasBench system interfaced to a ThermoScientific Delta V Plus isotope ratio mass spectrometer (ThermoScientific, Bremen, DE).  For sample concentrations greater than 500ppm, CO2 is sampled by a six-port rotary valve (Valco, Houston TX) with a 100µL loop programmed to switch at the maximum CO2 concentration in the helium carrier gas; for lower concentrations, the entire CO2 content is frozen in a trapping loop then released to the GC column.  The CO2 is then separated from N2O and other residual gases by a Poroplot Q GC column (25m x 0.32mm ID, 45°C, 2.5 mL/min). A pure reference gas (CO2) is used to calculate provisional delta values of the sample peak.  Final δ13C values are obtained after adjusting the provisional values such that correct δ13C values for laboratory standards are obtained.  Two laboratory standards are analyzed with every 10 samples.  The laboratory standards are calibrated directly against NIST 8545.


Analysis of 13C in Methane
Stable isotope ratios of δ13C in methane are measured using a ThermoScientific PreCon concentration system interfaced to a ThermoScientific Delta V Plus isotope ratio mass spectrometer (ThermoScientific, Bremen, DE). Gas samples are purged from vials through a double-needle sampler into a helium carrier stream (20 mL/min), which is passed through a CO2 scrubber (Ascarite) and a cold trap cooled by liquid nitrogen. The CH4 is separated from residual gases by a Poroplot Q GC column (25m x 0.32mm ID, 30°C, 2.5 mL/min).  After CH4 elutes from the separation column, it is oxidized to CO2by reaction with nickel oxide at 1000°C and then transferred to the IRMS.  A pure reference gas (CO2) is used to calculate provisional delta values of the sample peak.  Final δ13C  values are obtained after adjusting the provisional values such that correct δ13C values for laboratory standards are obtained.  Two laboratory standards are analyzed with every 10 samples. The laboratory standards are commercially prepared CH4 gas diluted in helium and are calibrated directly against NIST 8560.

 

Limit of Quantitation and Long-term standard deviation for CO2 & CH4 Analysis by Trace Gas-IRMS

CH4 : Limit of Quantitation: approx. 300 picomoles

           Long-term standard deviation: 0.2 ‰

 

CO2 : Limit of Quantitation: approx. 150 nanomoles (without cryofocusing)

           Long-term standard deviation: 0.02 ‰


Maximum measurable gas concentrations are dependent upon both concentration and isotopic enrichment.  Please contact us if you intend to submit enriched samples at concentrations more than ten times that of ambient concentration.




 
e-mail: sif@ucdavis.edu | phone: 530-752-8100 | fax: 530-752-4361
UC Davis Stable Isotope Facility | Department of Plant Sciences
One Shields Avenue, Mail Stop #1 | Davis, California, 95616 | USA