
NSF Org: |
AGS Division of Atmospheric and Geospace Sciences |
Recipient: |
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Initial Amendment Date: | April 25, 2017 |
Latest Amendment Date: | July 24, 2017 |
Award Number: | 1663740 |
Award Instrument: | Continuing Grant |
Program Manager: |
Sylvia Edgerton
sedgerto@nsf.gov (703)292-8522 AGS Division of Atmospheric and Geospace Sciences GEO Directorate for Geosciences |
Start Date: | May 1, 2017 |
End Date: | April 30, 2021 (Estimated) |
Total Intended Award Amount: | $462,568.00 |
Total Awarded Amount to Date: | $462,568.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
1251 MEMORIAL DR CORAL GABLES FL US 33146-2509 (305)421-4089 |
Sponsor Congressional District: |
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Primary Place of Performance: |
4600 Rickenbacker Causeway Key Biscayne FL US 33149-1031 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Atmospheric Chemistry |
Primary Program Source: |
01001819DB NSF RESEARCH & RELATED ACTIVIT 01001920DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): | |
Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Droughts mobilize natural dust from salt playas that can react with nitrogen oxides, criteria pollutants that are emitted by combustion sources. This reaction releases chlorine atoms that are potent atmospheric oxidants but are neglected in models used to assess regional air quality because of lack of measurements. The proposal will measure the fundamental rate constants of real-world playa dust particles with nitrogen oxides to enable robust assessments of regional air quality impacts in salt playas regions such as Texas.
Reactive chlorine (Cl) atoms when activated can serve as potent atmospheric oxidants that would effect lifetimes of greenhouse gases like methane and also tropospheric ozone abundance. The proposal hypothesizes that wind blown chloride-containing dust from dried saline lake beds (playas) can be converted to nitryl-chloride (ClNO2) by heterogeneous reactions with gaseous dinitrogen pentoxide (N2O5). The ClNO2 photolysis produces Cl atoms that could alter the ozone production photochemistry and the methane lifetime significantly. The research will measure the kinetics of ClNO2 production from reactions of salt with N2O5 in a trace gas-aerosol flow reactor. Chemical ionization mass spectrometry will be used to monitor ClNO2 in the reactor and the playa dusts will be analyzed using single-particle mass spectrometry, ion chromatography and X ray diffraction. The in depth analysis of the chemical and atmospheric conditions under which chlorine can be released from the saline playas will provide a mechanistic framework that could be implemented in chemistry-climate and air-quality models to make more robust predictions and assessments.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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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 goal of our project was to test our hypothesis that chemical reactions between pollutant gases and dust emitted from dried out lake beds, also known as playas, can generate reactive chlorine-containing gases that can lead to degraded air quality through the production of ozone, a criteria air pollutant regulated by the EPA. Through dedicated laboratory studies, we proved our hypothesis and further characterized how quickly and efficiently the reactions take place on playa dust. Further, we discovered that the playa dust mineralogy affected how much chlorine-containing gas was generated. Specifically, we found that competing chemical reactions with clays associated with playa dusts as well as the surface composition of playa dust particles played a key role in determining the outcome of our experiments. Our results are relevant for improving air quality models that aim to forecast pollutant exceedances. Traditional methods of modeling this chemistry rely on chemical methods that cannot account for competing reactions and surface composition. Because our findings are relevant for atmospheric particles (e.g., aerosols) other than playa dust, our work has broader implications for understanding how the chemical composition of aerosols from different sources affects their ability to contribute to ground-level concentrations of ozone and degraded air quality. Further, because the reactions that we studied are favorable in the wintertime, our work also contributes to a growing body of literature that aims to better understand recent observations of degraded wintertime air quality in regions such as Salt Lake City, which is also adjacent to a major dust emitting playa, the Great Salt Lake.
In addition to the scientific knowledge gained by this project, our work also resulted in several societal benefits. More broadly, our work contributed new knowledge regarding chemical pathways that enhance the production of ground-level ozone, a criteria air pollutant associated with negative health effects. Specifically, our work contributed to the early career training of a postdoctoral researcher, two PhD students, two undergraduate students, and a Master?s student. We also provided demonstrations of scientific concepts relevant to this work to middle school girls and first-generation college bound African and Latin American students. Due to COVID, our demonstrations were virtual in the last year of this project, increasing the reach of our outreach events to well over 1000 students.
Last Modified: 07/16/2021
Modified by: Cassandra Gaston
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