Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument

We describe the first instrument for measurement of the rate constant (s<sup>−1</sup>) for reactive loss (i.e., the total reactivity) of NO<sub>3</sub> in ambient air. Cavity-ring-down spectroscopy is used to monitor the mixing ratio of synthetically generated NO<sub>3&...

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Main Authors: J. M. Liebmann, G. Schuster, J. B. Schuladen, N. Sobanski, J. Lelieveld, J. N. Crowley
Format: Article
Language:English
Published: Copernicus Publications 2017-03-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/10/1241/2017/amt-10-1241-2017.pdf
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author J. M. Liebmann
G. Schuster
J. B. Schuladen
N. Sobanski
J. Lelieveld
J. N. Crowley
author_facet J. M. Liebmann
G. Schuster
J. B. Schuladen
N. Sobanski
J. Lelieveld
J. N. Crowley
author_sort J. M. Liebmann
collection DOAJ
description We describe the first instrument for measurement of the rate constant (s<sup>−1</sup>) for reactive loss (i.e., the total reactivity) of NO<sub>3</sub> in ambient air. Cavity-ring-down spectroscopy is used to monitor the mixing ratio of synthetically generated NO<sub>3</sub> ( ≈  30–50 pptv) after passing through a flow-tube reactor with variable residence time (generally 10.5 s). The change in concentration of NO<sub>3</sub> upon modulation of the bath gas between zero air and ambient air is used to derive its loss rate constant, which is then corrected for formation and decomposition of N<sub>2</sub>O<sub>5</sub> via numerical simulation. The instrument is calibrated and characterized using known amounts of NO and NO<sub>2</sub> and tested in the laboratory with an isoprene standard. The lowest reactivity that can be detected (defined by the stability of the NO<sub>3</sub> source, instrumental parameters and NO<sub>2</sub> mixing ratios) is 0.005 s<sup>−1</sup>. An automated dilution procedure enables measurement of NO<sub>3</sub> reactivities up to 45 s<sup>−1</sup>, this upper limit being defined mainly by the dilution accuracy. The typical total uncertainty associated with the reactivity measurement at the center of its dynamic range is 16 %, though this is dependent on ambient NO<sub>2</sub> levels. Results from the first successful deployment of the instrument at a forested mountain site with urban influence are shown and future developments outlined.
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spelling doaj.art-bdeca72b77ff422489d40ff3125161672022-12-22T01:41:11ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482017-03-011031241125810.5194/amt-10-1241-2017Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrumentJ. M. Liebmann0G. Schuster1J. B. Schuladen2N. Sobanski3J. Lelieveld4J. N. Crowley5Atmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyAtmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyAtmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyAtmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyAtmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyAtmospheric Chemistry Department, Max-Planck-Institut für Chemie, 55128 Mainz, GermanyWe describe the first instrument for measurement of the rate constant (s<sup>−1</sup>) for reactive loss (i.e., the total reactivity) of NO<sub>3</sub> in ambient air. Cavity-ring-down spectroscopy is used to monitor the mixing ratio of synthetically generated NO<sub>3</sub> ( ≈  30–50 pptv) after passing through a flow-tube reactor with variable residence time (generally 10.5 s). The change in concentration of NO<sub>3</sub> upon modulation of the bath gas between zero air and ambient air is used to derive its loss rate constant, which is then corrected for formation and decomposition of N<sub>2</sub>O<sub>5</sub> via numerical simulation. The instrument is calibrated and characterized using known amounts of NO and NO<sub>2</sub> and tested in the laboratory with an isoprene standard. The lowest reactivity that can be detected (defined by the stability of the NO<sub>3</sub> source, instrumental parameters and NO<sub>2</sub> mixing ratios) is 0.005 s<sup>−1</sup>. An automated dilution procedure enables measurement of NO<sub>3</sub> reactivities up to 45 s<sup>−1</sup>, this upper limit being defined mainly by the dilution accuracy. The typical total uncertainty associated with the reactivity measurement at the center of its dynamic range is 16 %, though this is dependent on ambient NO<sub>2</sub> levels. Results from the first successful deployment of the instrument at a forested mountain site with urban influence are shown and future developments outlined.http://www.atmos-meas-tech.net/10/1241/2017/amt-10-1241-2017.pdf
spellingShingle J. M. Liebmann
G. Schuster
J. B. Schuladen
N. Sobanski
J. Lelieveld
J. N. Crowley
Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
Atmospheric Measurement Techniques
title Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
title_full Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
title_fullStr Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
title_full_unstemmed Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
title_short Measurement of ambient NO<sub>3</sub> reactivity: design, characterization and first deployment of a new instrument
title_sort measurement of ambient no sub 3 sub reactivity design characterization and first deployment of a new instrument
url http://www.atmos-meas-tech.net/10/1241/2017/amt-10-1241-2017.pdf
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