Chemical identification of new particle formation and growth precursors through positive matrix factorization of ambient ion measurements
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Published:2023-05-17
Issue:9
Volume:23
Page:5567-5585
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Katz Daniel JohnORCID, Abdelhamid Aroob, Stark Harald, Canagaratna Manjula R., Worsnop Douglas R., Browne Eleanor C.ORCID
Abstract
Abstract. In the lower troposphere, rapid collisions between ions
and trace gases result in the transfer of positive charge to the highest
proton affinity species and negative charge to the lowest proton affinity
species. Measurements of the chemical composition of ambient ions thus
provide direct insight into the most acidic and basic trace gases and their
ion–molecule clusters – compounds thought to be important for new particle
formation and growth. We deployed an atmospheric pressure interface
time-of-flight mass spectrometer (APi-ToF) to measure ambient ion chemical
composition during the 2016 Holistic Interactions of Shallow Clouds,
Aerosols, and Land Ecosystems (HI-SCALE) campaign at the United States
Department of Energy Atmospheric Radiation Measurement facility in the
Southern Great Plains (SGP), an agricultural region. Cations and anions were
measured for alternating periods of ∼ 24 h over 1 month.
We use binned positive matrix factorization (binPMF) and generalized Kendrick
analysis (GKA) to obtain information about the chemical
formulas and temporal variation in ionic composition without the need for
averaging over a long timescale or a priori high-resolution peak fitting.
Negative ions consist of strong acids including sulfuric and nitric acid,
organosulfates, and clusters of NO3- with highly oxygenated organic
molecules (HOMs) derived from monoterpene (MT) and sesquiterpene (SQT) oxidation.
Organonitrates derived from SQTs account for most of the HOM
signal. Combined with the diel profiles and back trajectory analysis, these
results suggest that NO3 radical chemistry is active at this site.
SQT oxidation products likely contribute to particle growth at the
SGP site. The positive ions consist of bases including alkyl pyridines and
amines and a series of high-mass species. Nearly all the positive ions
contained only one nitrogen atom and in general support ammonia and amines
as being the dominant bases that could participate in new particle
formation. Overall, this work demonstrates how APi-ToF measurements combined
with binPMF analysis can provide insight into the temporal evolution of
compounds important for new particle formation and growth.
Funder
Biological and Environmental Research
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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