Award Abstract # 2035225
Reconciling Atmospheric OH Reactivity Measurements with PTR-ToF-MS Observations and Photochemical Box Model Simulations

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: UNIVERSITY OF CALIFORNIA IRVINE
Initial Amendment Date: December 18, 2020
Latest Amendment Date: May 20, 2021
Award Number: 2035225
Award Instrument: Standard Grant
Program Manager: Sylvia Edgerton
sedgerto@nsf.gov
 (703)292-8522
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: January 1, 2021
End Date: December 31, 2024 (Estimated)
Total Intended Award Amount: $569,010.00
Total Awarded Amount to Date: $569,010.00
Funds Obligated to Date: FY 2021 = $569,010.00
History of Investigator:
  • Saewung Kim (Principal Investigator)
    saewungk@uci.edu
  • Alex Guenther (Co-Principal Investigator)
Recipient Sponsored Research Office: University of California-Irvine
160 ALDRICH HALL
IRVINE
CA  US  92697-0001
(949)824-7295
Sponsor Congressional District: 47
Primary Place of Performance: University of California-Irvine
3216 Croul Hall
Irvine
CA  US  92697-3100
Primary Place of Performance
Congressional District:
47
Unique Entity Identifier (UEI): MJC5FCYQTPE6
Parent UEI: MJC5FCYQTPE6
NSF Program(s): Atmospheric Chemistry
Primary Program Source: 01002122DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 152400
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Ozone and particulate matter are components of air pollution that affect the environment and human health; however, gaps remain in current understanding of how these components are formed. In the present project, laboratory experiments are conducted to shed light on reactions of atmospheric precursor molecules. Results are compared to existing models and field data and will provide new mechanistic insight that can help inform air pollution control strategies. Participating graduate students are integrated in the outreach plan to engage K-12 students and teaches.

Systematic laboratory studies are performed on reactive volatile organic compounds (VOCs) and oxidation intermediates and products to improve current understanding of tropospheric photochemistry. The tandem chamber reactor system used for experiments is equipped with state-of-the-art analytical tools including high-resolution proton transfer reaction-mass spectrometry (PTR-ToF-MS) and comparative reactivity method (CRM) for analysis of components and to quantify OH reactivity, respectively. Method development and instrument calibration are an integral part of this work. New observations are evaluated with existing box models and compared to previously obtained field datasets for re-examination. Results may reveal fundamental new mechanisms and help gain greater insight into ozone and particulate matter production under various pollution levels. PIs and diverse graduate students are supported through this project, and outreach is planned to elementary school students and teachers, while middle school students will be provided opportunities to visit campus and experience hands-on air sampling and gas analyses instrumentation.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The chemical composition of ambient air has significant implications for human health and long-term weather. As we always breathe air, our fundamental curiosity to explore what is in the air justifies scientific investigations.  The NSF grant allowed us to evaluate an analytical technique to quantify the total amount of atmospheric reactive gases. The observable is called OH (hydroxyl radical) reactivity, notating the reciprocal of the atmospheric lifetime of OH.  Although these gases determine air quality as they are precursors in producing major air pollutants such as ozone and fine particles, it has long been speculated that we, as the scientific community, have yet to quantify the total amount completely. The laboratory characterization allows us to deploy the OH reactivity quantification system to the New York Metropolitan area as a part of the community field campaign.  The comparison with the observed trace gas dataset illustrates that the unmeasured reactive trace gas amount increases as ambient temperature increases. This is also when isoprene, a reactive biogenic volatile organic compound, and ozone concentrations were observed at elevated levels. The dataset provides a critical dataset to evaluate ozone photochemical production regimes in different temperature environments. The evaluation suggests that higher temperatures bring a physical and chemical environment with more efficient ozone production. We used a box model with detailed photochemical reaction mechanisms to predict ambient ozone levels in the area. Warmer weather will bring higher evaporative VOC emissions along with higher biogenic VOC emissions. At the same time, reactive nitrogen oxides (NO and NO2) emissions, mostly from combustion sources such as internal combustion engines, are expected to decrease. The detailed mechanistic analysis illustrates that the occurrence of high ozone episodes will most likely increase. This developed streamlined research framework, from experimental to computational methodologies, can be applied to other metropolitan areas, as our fundamental desire is to breathe cleaner air. 

 


Last Modified: 04/29/2025
Modified by: Saewung Kim

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