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Title: Application of high-resolution time-of-flight chemical ionization mass spectrometry measurements to estimate volatility distributions of α-pinene and naphthalene oxidation products

Journal Article · · Atmospheric Measurement Techniques (Online)
 [1];  [2];  [1];  [3];  [1];  [2];  [4];  [5];  [1]
  1. Aerodyne Research, Inc., Billerica, MA (United States)
  2. Aerodyne Research, Inc., Billerica, MA (United States); Boston College, Chestnut Hill, MA (United States)
  3. Aerodyne Research, Inc., Billerica, MA (United States); Univ. of Colorado, Boulder, CO (United States)
  4. Boston College, Chestnut Hill, MA (United States)
  5. Aerodyne Research, Inc., Billerica, MA (United States); Univ. of Colorado, Boulder, CO (United States); TOFWERK AG, Thun (Switzerland)

Recent developments in high-resolution time-of-flight chemical ionization mass spectrometry (HR-ToF-CIMS) have made it possible to directly detect atmospheric organic compounds in real time with high sensitivity and with little or no fragmentation, including low-volatility, highly oxygenated organic vapors that are precursors to secondary organic aerosol formation. Here, using ions identified by high-resolution spectra from an HR-ToF-CIMS with acetate reagent ion chemistry, we develop an algorithm to estimate the vapor pressures of measured organic acids. The algorithm uses identified ion formulas and calculated double bond equivalencies, information unavailable in quadrupole CIMS technology, as constraints for the number of possible oxygen-containing functional groups. The algorithm is tested with acetate chemical ionization mass spectrometry (acetate-CIMS) spectra of O3 and OH oxidation products of α-pinene and naphthalene formed in a flow reactor with integrated OH exposures ranged from 1.2 × 1011 to 9.7 × 1011 molec s cm−3, corresponding to approximately 1.0 to 7.5 days of equivalent atmospheric oxidation. Measured gas-phase organic acids are similar to those previously observed in environmental chamber studies. For both precursors, we find that acetate-CIMS spectra capture both functionalization (oxygen addition) and fragmentation (carbon loss) as a function of OH exposure. The level of fragmentation is observed to increase with increased oxidation. The predicted condensed-phase secondary organic aerosol (SOA) average acid yields and O/C and H/C ratios agree within uncertainties with previous chamber and flow reactor measurements and ambient CIMS results. Furthermore, while acetate reagent ion chemistry is used to selectively measure organic acids, in principle this method can be applied to additional reagent ion chemistries depending on the application.

Research Organization:
Boston College, Chestnut Hill, MA (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
SC0006980; SC0004577; FG02-05ER63995
OSTI ID:
1197858
Alternate ID(s):
OSTI ID: 1455196
Journal Information:
Atmospheric Measurement Techniques (Online), Vol. 8, Issue 1; ISSN 1867-8548
Publisher:
European Geosciences UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 35 works
Citation information provided by
Web of Science

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