Automated calibration of laser spectrometer measurements of δ18O and δ2H values in water vapour using a Dew Point Generator
Abstract
--- - "Rationale: Continuous measurement of stable O and H isotope compositions in water vapour requires automated calibration for remote field deployments. We developed a new low-cost device for calibration of both water vapour mole fraction and isotope composition." - "Methods: We coupled a commercially available dew point generator (DPG) to a laser spectrometer and developed hardware for water and air handling along with software for automated operation and data processing. We characterised isotopic fractionation in the DPG, conducted a field test and assessed the influence of critical parameters on the performance of the device." - "Results: An analysis time of 1hour was sufficient to achieve memory-free analysis of two water vapour standards and the O-18 and H-2 values were found to be independent of water vapour concentration over a range of approximate to 20,000-33,000ppm. The reproducibility of the standard vapours over a 10-day period was better than 0.14 and 0.75 parts per thousand for delta O-18 and delta H-2 values, respectively (1 sigma, n=11) prior to drift correction and calibration. The analytical accuracy was confirmed by the analysis of a third independent vapour standard. The DPG distillation process requires that isotope calibration takes account of DPG temperature, analysis time, injected water volume and air flow rate." - "Conclusions: The automated calibration system provides high accuracy and precision and is a robust, cost-effective option for long-term field measurements of water vapour isotopes. The necessary modifications to the DPG are minor and easily reversible."
Más información
| Título según WOS: | ID WOS:000432269600010 Not found in local WOS DB |
| Título de la Revista: | RAPID COMMUNICATIONS IN MASS SPECTROMETRY |
| Volumen: | 32 |
| Número: | 12 |
| Editorial: | Wiley |
| Fecha de publicación: | 2018 |
| Página de inicio: | 1008 |
| Página final: | 1014 |
| DOI: |
10.1002/rcm.8131 |
| Notas: | ISI |