Nitrate (NO3) Analysis by Bacteria Denitrification
The SIF provides isotope analysis (15N, 18O) of NO3 in water by bacteria denitrification assay.
Analysis of 15N and 18O in Gas Mixtures
Trace gas isotope ratios are measured using a ThermoFinnigan GasBench + PreCon trace gas concentration system interfaced to a ThermoScientific Delta V Plus isotope-ratio mass spectrometer (Bremen, Germany). Gas samples are purged from vials through a double-needle sampler into a helium carrier stream (20 mL/min). Then, N2 and N2O are isolated and concentrated in preparation for isotopic analysis. First, N2 gas is sampled by a rotary 8-port valve fitted with a 20-100 µL sampling loop and timed to capture the peak N2 concentration in the carrier gas stream. This gas sample is passed to the IRMS through a molecular sieve 5A GC column (15m x 0.53mm ID, 25°C, 3 mL/min). A reference N2 peak is used to calculate provisional isotope ratios of the sample N2 peak.
As N2 is analyzed, the rest of the gas sample passes through a CO2 scrubber (Ascarite) and N2O is trapped and concentrated in 2 liquid nitrogen cryo-traps operated in series such that the N2O is held in the first trap until the non-condensing portion of the sample gas has been replaced by helium carrier, then passed to the second, smaller trap. Finally the second trap is warmed to ambient and the N2O is carried by helium to the IRMS via a Poroplot Q GC column (25m x 0.53 mm, 25°C, 1.8 mL/min). This column separates N2O from residual CO2. A reference N2O peak is used to calculate provisional isotope ratios of the sample N2O peak.
Final δ15N values are calculated by adjusting the provisional values such that correct δ15N values for working standards are obtained. Two working standards are analyzed every 10 samples. The working standards are mixtures of N2 and N2O (e.g., 3% N2 + 1 ppm N2O with the balance He or 1 ppm N2O with balance N2). The N2 is calibrated against an Oztech N2 standard (Oztech Trading Co., δ15N vs air = -0.61). The calibration of the N2O is problematic since there are no suitable international standards. Thus, we calibrated 15N and 18O by thermally decomposing N2O in a heated gold tube (800°C) to convert N2O to N2 + O2. The resulting N2 was calibrated against the Oztech N2 standard, and the O2 was calibrated against an Oztech O2 standard (δ18O vs VSMOW = 27.48).
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 |







