Abstract
Evaluation of the semi-continuous Monitor for AeRosols and GAses in ambient air (MARGA, Metrohm Ap-plikon B.V.) was conducted with an emphasis on examination of accuracy and precision associated with processing of chromatograms. Using laboratory standards and atmospheric measurements, analytical accuracy, precision and method detection limits derived using the commercial MARGA software were compared to an alternative chromatography procedure consisting of a custom Java script to reformat raw MARGA conductivity data and Chromeleon (Thermo Scientific Dionex) software for peak integration. Our analysis revealed issues with accuracy and precision resulting from misidentification and misintegration of chromatograph peaks by the MARGA automated software as well as a systematic bias at low concentrations for anions. Reprocessing and calibration of raw MARGA data using the alternative chromatography method lowered method detection limits and re-duced variability (precision) between parallel sampler boxes. Instrument performance was further evaluated during a 1-month intensive field campaign in the fall of 2014, including analysis of diurnal patterns of gaseous and particulate water-soluble species (NH3, SO2, HNO3, , and , gas-to-particle partitioning and particle neutralization state. At ambient concentrations below ~ 1 µg m–3, concentrations determined using the MARGA software are biased +30 and +10 % for and , respectively, compared to concentrations determined using the alternative chromatography procedure. Differences between the two methods increase at lower concentrations. We demonstrate that positively biased and measurements result in overestimation of aerosol acidity and introduce nontrivial errors to ion balances of inorganic aerosol. Though the source of the bias is uncertain, it is not corrected by the MARGA online single-point internal LiBr standard. Our results show that calibra-tion and verification of instrument accuracy by multilevel external standards is required to adequately control analytical accuracy. During the field intensive, the MARGA was able to capture rapid compositional changes in PM2.5 due to changes in meteorology and air mass history relative to known source regions of PM precursors, including a fine aerosol event associated with intrusion of Arctic air into the southeastern US.
Highlights
Secondary inorganic aerosols are formed from gaseous precursors including ammonia (NH3), nitric acid (HNO3) and sulfur dioxide (SO2), producing ammonium nitrate (NH4NO3), ammonium bisulfate (NH4HSO4) and ammonium sulfate ((NH4)2SO4) particles
wet rotating denuder (WRD), gaseous species are collected by diffusion into a liquid film while particles pass through the WRD to the steam jet aerosol collector (SJAC), where supersaturation grows the particles by condensation
Close examination of MARGA chromatograms revealed a number of issues, including misidentification and misintegration of analyte peaks
Summary
Secondary inorganic aerosols are formed from gaseous precursors including ammonia (NH3), nitric acid (HNO3) and sulfur dioxide (SO2), producing ammonium nitrate (NH4NO3), ammonium bisulfate (NH4HSO4) and ammonium sulfate ((NH4)2SO4) particles. These gaseous precursors and particulate matter, which partition between phases to establish a thermodynamic equilibrium of ammonium– sulfate–nitrate (Finlayson-Pitts and Pitts, 2000; Seinfeld and Pandis, 2006), represent a significant fraction of PM2.5 (Seinfeld and Pandis, 2006; Pinder et al, 2007) and contribute to atmospheric deposition of nutrients and acidity. High-frequency simultaneous measurements of the gas and aerosol components of the ammonium–sulfate–nitrate system are required to investigate inorganic aerosol characteristics (e.g., phase partitioning, acidity) and formation processes and to quantify the dry component of nitrogen deposition
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