Implementation of an original approach on the Mines-Douai Comparative Reactivity Method (MD-CRM) instrument to identify part of the missing OH reactivity at an urban site

Abstract:

Due to the large number of Volatile Organic Compounds (VOCs) expected in the atmosphere (10⁴-10⁵) (Goldstein and Galbally, ES&T, 2007), exhaustive measurements of VOCs appear to be currently unfeasible using common analytical techniques. In this context, measurements of the total sink of OH, referred as total OH reactivity, can provide a critical test to assess the completeness of trace gas measurements during field campaigns. This can be done by comparing the measured total OH reactivity to values calculated from trace gas measurements. Indeed, large discrepancies are usually found between measured and calculated OH reactivity values revealing the presence of important unmeasured reactive species, which have yet to be identified.

A Comparative Reactivity Method (CRM) instrument has been setup at Mines Douai to allow sequential measurements of VOCs and OH reactivity using the same Proton Transfer Reaction-Time of Flight Mass Spectrometer. This approach aims at identifying unmeasured reactive VOCs based on a method proposed by Kato et al. (Atmos. Environ., 2011), taking advantage of VOC oxidations occurring in the CRM sampling reactor. MD-CRM has been deployed at an urban site in Dunkirk (France) during July 2014 to test this new approach. During this campaign, a large fraction of the OH reactivity was not explained by collocated measurements of trace gases (67% on average). In this presentation, we will first describe the approach that was implemented in the CRM instrument to identify part of the observed missing OH reactivity and we will then discuss the OH reactivity budget regarding the origin of air masses reaching the measurement site.