EGU25-5412, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-5412
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 15:15–15:25 (CEST)
 
Room 2.95
Establishment of a purge and trap continuous flow isotope ratio mass spectrometer system for analysis of stable nitrate isotopes (δ15N and δ18O) in water samples by Ti(III) reduction
Monis Nolitha Gcakasi1, Christine Stumpp1, and Andrea Watzinger2
Monis Nolitha Gcakasi et al.
  • 1Institute for Soil Physics and Rural Water Management, BOKU University, Vienna, Austria (christine.stumpp@boku.ac.at)
  • 2Institute of Soil Research, BOKU University, Vienna, Austria (andrea.watzinger@boku.ac.at)

Pollution of surface and shallow groundwater by nitrate (NO3-) is a global concern resulting in deterioration of drinking water quality. Stable isotopes of NO3- 15N and δ18O) can be used to trace its sources which have distinct N and O isotopic signatures. The isotopic values can also be used to identify areas of natural remediation through biogeochemical processes such as denitrification. Conversion of aqueous NO3- to N2O headspace gas by Ti(III) reduction is a new method for analysis of NO3- stable isotopes. Previous literature introduces the analytical procedure but provides limited guidelines for instrument set-up and operation. Here, we present an automated purge and trap isotope ratio mass spectrometer (P&T-IRMS) combined with the Ti(III) reduction method for analysis of δ15N and δ18O in NO3-. The P&T-IRMS base analytical precision was ±0.3‰ and ±0.2‰ for δ15N and δ18O, respectively. Isotopic values were quantified down to an N2O gas concentration of 1 µl L-1 for δ15N and 2 µl L-1 for δ18O. The target NO3--N concentration needed for accurate measurements was 0.2 mg L-1. Comparison of δ15N and δ18O measured using the P&T-IRMS by Ti(III) reduction with EA-IRMS values showed high accuracy. The measurement precision (SD) and uncertainties (u) for our KNO3- internal standard were ±0.2 (±0.6) and ±0.2 (±0.9) for δ15N and δ18O, respectively. The P&T-IRMS and Ti(III) reduction method set-up showed low quantification limits and acceptable accuracy and precision in line with other well-established methods for analysis of NO3- stable isotopes. The provided guidelines will assist laboratories which utilize IRMS headspace gas instrumentation with the process of IRMS set-up and operation and establishment of an independent analytical procedure for the Ti(III) reduction method. 

How to cite: Gcakasi, M. N., Stumpp, C., and Watzinger, A.: Establishment of a purge and trap continuous flow isotope ratio mass spectrometer system for analysis of stable nitrate isotopes (δ15N and δ18O) in water samples by Ti(III) reduction, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-5412, https://doi.org/10.5194/egusphere-egu25-5412, 2025.