Articles | Volume 10, issue 8
https://doi.org/10.5194/amt-10-3073-2017
https://doi.org/10.5194/amt-10-3073-2017
Research article
 | 
24 Aug 2017
Research article |  | 24 Aug 2017

Effects of variation in background mixing ratios of N2, O2, and Ar on the measurement of δ18O–H2O and δ2H–H2O values by cavity ring-down spectroscopy

Jennifer E. Johnson and Chris W. Rella

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Cited articles

Aemisegger, F., Sturm, P., Graf, P., Sodemann, H., Pfahl, S., Knohl, A., and Wernli, H.: Measuring variations of δ2H and δ18O in atmospheric water vapour using two commercial laser-based spectrometers: an instrument characterisation study, Atmos. Meas. Tech., 5, 1491–1511, https://doi.org/10.5194/amt-5-1491-2012, 2012.
Becker, M., Andersen, N., Fiedler, B., Fietzek, P., Körtzinger, A., Steinhoff, T., and Friedrichs, G.: Using cavity ringdown spectroscopy for continuous monitoring of δ13C(CO2) and fCO2 in the surface ocean, Limnol. Oceanogr.-Meth., 10, 752–766, https://doi.org/10.4319/lom.2012.10.752, 2012.
Berkelhammer, M., Hu, J., Bailey, A., Noone, D., J, S. C., Barnard, H., Gochis, D., Hsiao, G., Rahn, T., and Turnipseed, A.: The nocturnal water cycle in an open-canopy forest, J. Geophys. Res.-Atmos., 118, 10225–10242, 2013.
Brand, W. A., Geilmann, H., Crosson, E. R., and Rella, C. W.: Cavity ring-down spectroscopy versus high-temperature conversion isotope ratio mass spectrometry; a case study on δ2H and δ18O of pure water samples and alcohol/water mixtures, Rapid Commun. Mass Spectrom., 23, 1879–1884, https://doi.org/10.1002/rcm.4083, 2009.
Brewer, P. J., Brown, R. J. C., Miller, M. N., Miñarro, M. D., Murugan, A., Milton, M. J. T., and Rhoderick, G. C.: Preparation and Validation of Fully Synthetic Standard Gas Mixtures with Atmospheric Isotopic Composition for Global CO2 and CH4 Monitoring, Anal. Chem., 86, 1887–1893, https://doi.org/10.1021/ac403982m, 2014.
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Short summary
Cavity ring-down spectrometers (CRDS) can make accurate measurements of trace gases when the inert gas background is constant but are prone to errors when the background is variable. Here, we report that in one CRDS analyzer (L2120-i, Picarro), these errors result from broadening, narrowing, and shifting of the target absorption lines as well as neighboring lines. New spectral acquisition and analysis strategies are needed to make CRDS measurements robust to variable backgrounds.