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Boreas: A Sample Preparation-Coupled Laser Spectrometer System for Simultaneous High-Precision In Situ Analysis of δ(13)C and δ(2)H from Ambient Air Methane

[Image: see text] We present a new instrument, “Boreas”, a cryogen-free methane (CH(4)) preconcentration system coupled to a dual-laser spectrometer for making simultaneous measurements of δ(13)C(CH(4)) and δ(2)H(CH(4)) in ambient air. Excluding isotope ratio scale uncertainty, we estimate a typical...

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Detalles Bibliográficos
Autores principales: Rennick, Chris, Arnold, Tim, Safi, Emmal, Drinkwater, Alice, Dylag, Caroline, Webber, Eric Mussell, Hill-Pearce, Ruth, Worton, David R., Bausi, Francesco, Lowry, Dave
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2021
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9584170/
https://www.ncbi.nlm.nih.gov/pubmed/34260200
http://dx.doi.org/10.1021/acs.analchem.1c01103
Descripción
Sumario:[Image: see text] We present a new instrument, “Boreas”, a cryogen-free methane (CH(4)) preconcentration system coupled to a dual-laser spectrometer for making simultaneous measurements of δ(13)C(CH(4)) and δ(2)H(CH(4)) in ambient air. Excluding isotope ratio scale uncertainty, we estimate a typical standard measurement uncertainty for an ambient air sample of 0.07‰ for δ(13)C(CH(4)) and 0.9‰ for δ(2)H(CH(4)), which are the lowest reported for a laser spectroscopy-based system and comparable to isotope ratio mass spectrometry. We trap CH(4) (∼1.9 μmol mol(–1)) from ∼5 L of air onto the front end of a packed column, subsequently separating CH(4) from interferences using a controlled temperature ramp with nitrogen (N(2)) as the carrier gas, before eluting CH(4) at ∼550 μmol mol(–1). This processed sample is then delivered to an infrared laser spectrometer for measuring the amount fractions of (12)CH(4), (13)CH(4), and (12)CH(3)D isotopologues. We calibrate the instrument using a set of gravimetrically prepared amount fraction primary reference materials directly into the laser spectrometer that span a range of 500–626 μmol mol(–1) (CH(4) in N(2)) made from a single pure CH(4) source that has been isotopically characterized for δ(13)C(CH(4)) by IRMS. Under the principle of identical treatment, a compressed ambient air sample is used as a working standard and measured between air samples, from which a final calibrated isotope ratio is calculated. Finally, we make automated measurements of both δ(13)C(CH(4)) and δ(2)H(CH(4)) in over 200 ambient air samples and demonstrate the application of Boreas for deployment to atmospheric monitoring sites.