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Automated calibration of laser spectrometer measurements of δ18 O and δ2 H values in water vapour using a Dew Point Generator.
Munksgaard, Niels C; Cheesman, Alexander W; Gray-Spence, Andrew; Cernusak, Lucas A; Bird, Michael I.
Affiliation
  • Munksgaard NC; Research Institute for the Environment and Livelihoods, Charles Darwin University, Darwin, Australia.
  • Cheesman AW; College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Cairns, Australia.
  • Gray-Spence A; College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Cairns, Australia.
  • Cernusak LA; Information & Communications Technology, Division of Services and Resources, James Cook University, Cairns, Australia.
  • Bird MI; College of Science and Engineering and Centre for Tropical Environmental and Sustainability Science, James Cook University, Cairns, Australia.
Rapid Commun Mass Spectrom ; 32(12): 1008-1014, 2018 Jun 30.
Article in En | MEDLINE | ID: mdl-29603458
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 1 hour was sufficient to achieve memory-free analysis of two water vapour standards and the δ18 O and δ2 H values were found to be independent of water vapour concentration over a range of ≈20,000-33,000 ppm. The reproducibility of the standard vapours over a 10-day period was better than 0.14 ‰ and 0.75 ‰ for δ18 O and δ2 H values, respectively (1 σ, 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.

Full text: 1 Collection: 01-internacional Database: MEDLINE Type of study: Prognostic_studies Language: En Journal: Rapid Commun Mass Spectrom Year: 2018 Document type: Article Affiliation country: Australia

Full text: 1 Collection: 01-internacional Database: MEDLINE Type of study: Prognostic_studies Language: En Journal: Rapid Commun Mass Spectrom Year: 2018 Document type: Article Affiliation country: Australia
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