Award Abstract # 1452317
EAGER: Nanoparticle Growth from Salting-in and Mobile Infrared Column Observations

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: THE REGENTS OF THE UNIVERSITY OF COLORADO
Initial Amendment Date: July 30, 2014
Latest Amendment Date: May 17, 2016
Award Number: 1452317
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: September 1, 2014
End Date: August 31, 2017 (Estimated)
Total Intended Award Amount: $258,856.00
Total Awarded Amount to Date: $310,551.00
Funds Obligated to Date: FY 2014 = $258,856.00
FY 2016 = $51,695.00
History of Investigator:
  • Rainer Volkamer (Principal Investigator)
    rainer.volkamer@colorado.edu
Recipient Sponsored Research Office: University of Colorado at Boulder
3100 MARINE ST
Boulder
CO  US  80309-0001
(303)492-6221
Sponsor Congressional District: 02
Primary Place of Performance: University of Colorado at Boulder
3100 Marine Street, Room 481
Boulder
CO  US  80309-0572
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): SPVKK1RC2MZ3
Parent UEI:
NSF Program(s): Atmospheric Chemistry
Primary Program Source: 01001415DB NSF RESEARCH & RELATED ACTIVIT
01001617DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): OTHR, 7916
Program Element Code(s): 152400
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This research includes the development of a new mobile instrument for providing data on the column absorption of infrared radiation by hydrocarbons in the atmosphere, a process that can lead to an atmospheric warming. The Principal Investigator of the project also has been invited to visit the Paul-Scherrer Institute in Switzerland to design a series of experiments at the CLOUD chamber facility at CERN. This facility will enable him to study the formation of secondary organic aerosol (SOA) in the atmosphere under varying conditions of ambient temperature and pressure. It is important to understand the mechanisms that lead to the fast formation and growth of secondary organic aerosol since they are important in predicting air quality and climate change.

The proposed CLOUD chamber experiments will focus on the 'salting-in' effect as a mechanism for explaining accelerated nanoparticle growth rates. In the case of glyoxal, 'salting-in' consists of the displacement of water molecules from the hydration shell of sulfate ions by hydrated glyoxal molecules. Preliminary studies show efficient growth from glyoxal at relative humidity (RH) of up to 20% for highly acidic nanoclusters. However, there are currently no experimental data available at RH above 20% and for neutral nanoclusters, where the multiphase chemistry is expected to proceed via different pathways. The proposed research will address the following questions related to the formation of SOA (associated with glyoxal) in the atmosphere: (1) What is the 'threshold cluster size' at which glyoxal begins to assists with the stabilization/growth of clusters; and (2) How does the growth rate of stable clusters depend on relative humidity and pH? The 'salting-in' mechanism has been incorporated in an atmospheric model to successfully explain the fast formation of SOA from glyoxal that was observed in a recent NSF-supported field campaign to study air pollution in Mexico City.

The development of the mobile Solar Occultation Flux instrument and the acquisition of new expertise for IR retrievals from the instrument will offer a novel way to better quantify atmospheric composition and changes in composition. The experiments at the CLOUD chamber may result in transformative research on the mechanisms for formation and growth of secondary organic aerosol. This research is funded through the EArly-concept Grants for Exploratory Research (EAGER) program.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Chiu, R., L. Tinel, L. Gonzalez-Palacios, R. Ciuraru, F. Bernard, C. George, R. Volkamer "UV Photochemistry of Carboxylic Acids at the Air-Sea Boundary: A Relevant Source of Glyoxal and other OVOC in the Marine Atmosphere" Geophysical Research Letters , v.44 , 2017 10.1002/2016GL071240
Waxman, E.; J. Elm, T. Kurtén, K. Mikkelsen, P. Ziemann, R. Volkamer "Glyoxal and Methyl Glyoxal Setschenow Salting Constants in Sulfate, Nitrate and Chloride Solutions: Measurements and Gibbs Energies" Environmental Science and Technology , v.49 , 2015 10.1021/acs.est.5b02782
Sareen, N., E.M. Waxman, B.J. Turpin, R. Volkamer, A.G. Carlton "Potential of aerosol liquid water to facilitate organic aerosol formation: assessing knowledge gas about precursors and partitioning" Environmental Science and Technology , v.51 , 2017 10.1021/acs.est.6b04540
Kille, N., S. Baidar, P. Handley, I. Ortega, R. Sinreich, O. R. Cooper, F. Hase, J. W. Hannigan, G. Pfister, and R. Volkamer. "The CU Mobile Solar Occultation Flux Instrument: structure functions and emission rates of NH3, NO2 and C2H6" Atmospheric Measurement Techniques , v.10 , 2017 10.5194/amt-10-373-2017
Hoyle, C.R., C. Fuchs, E. Järvinen, H. Saathoff, A. Dias, I. El Haddad, M. Gysel, S.C. Coburn, J. Tröstl, A.-K. Bernhammer, F. Bianchi, M. Breitenlechner, J.C. Corbin, J. Craven, N.M. Donahue, J. Duplissy, S. Ehrhart, C. Frege, H. Gordon, N. Höppel, M. He "Aqueous phase oxidation of sulphur dioxide by ozone in cloud droplets" Atmospheric Chemistry and Physics , v.16 , 2016 10.5194/acp-16-1693-2016
Hoyle, C.R., C. Fuchs, E. Järvinen, H. Saathoff, A. Dias, I. El Haddad, M. Gysel, S.C. Coburn, J. Tröstl, A.-K. Bernhammer, F. Bianchi, M. Breitenlechner, J.C. Corbin, J. Craven, N.M. Donahue, J. Duplissy, S. Ehrhart, C. Frege, H. Gordon, N. Höppel, M. He "Aqueous phase oxidation of sulphur dioxide by ozone in cloud droplets" Atmospheric Chemistry and Physics , v.16 , 2016 , p.1693 10.5194/acp-16-1693-2016
Höpfner, M., R. Volkamer, U. Grabowski, M. Grutter, J. Orphal, G. Stiller, T. von Clarmann, and G. Wetzel "First detection of ammonia (NH3) in the Asian monsoon upper troposphere" Atmospheric Chemistry and Physics , v.16 , 2016 10.5194/acp-16-14357-2016
González Palacios, L., P. Corral Arroyo, K. Z. Aregahegn, S. S. Steimer, T. Bartels-Rausch, B. Noziere, C. George, M. Ammann, and R. Volkamer "Heterogeneous photochemistry of imidazole-2-carboxaldehyde: HO2 radical formation and aerosol growth" Atmospheric Chemistry and Physics , v.16 , 2016 10.5194/acp-2016-67
González Palacios, L., P. Corral Arroyo, K. Z. Aregahegn, S. S. Steimer, T. Bartels-Rausch, B. Noziere, C. George, M. Ammann, and R. Volkamer "Heterogeneous photochemistry of imidazole-2-carboxaldehyde: HO2 radical formation and aerosol growth" Atmospheric Chemistry and Physics , v.16 , 2016 , p.11823 10.5194/acp-2016-67
Eleanor M. Waxman, Jonas Elm, Theo Kurtén, Kurt V. Mikkelsen, Paul J. Ziemann, and Rainer Volkamer "Glyoxal and Methylglyoxal Setschenow Salting Constants in Sulfate, Nitrate and Chloride Solutions: Measurements and Gibbs Energies" Environmental Science and Technology , 2015 10.1021/acs.est.5b02782

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.

Cost effective new methods to quantify emissions of trace gases benefit society, because pollution poses a costly risk to human health. For example, wildfires are important for ecosystems, but are also a major source of airborne smoke and pollution that poses a risk to human health and property; yet difficulties to quantify fire emissions arise from limitations with access to plumes that often travel decoupled from ground-level, complex terrain, plume heterogeneity, and uncertain plume rise and transport. 

This project explored Solar Occultation Flux (SOF), based on infrared absorption spectroscopy from aircraft, as a high risk and potentially transformative approach to study biomass burning emissions using aircraft. An early airborne SOF prototype, developed at the University of Colorado at Boulder, was successfully flown on research aircraft. The use of SOF to quantify emissions of harmful ammonia (NH3), an aerosol precursor, and nitrogen oxides (NOx = NO + NO2) from agricultural soils was further demonstrated using a ground-based prototype. Better knowledge about emissions is pre-requisite to protecting society from the harmful impacts of pollution. It is shown that NOx emissions from agricultural soils, most likely due to microbial activity, are missing in National Emission Inventories. Such unaccounted NOx sources are likely to gain relative importance in the future as other sources continue to decrease. Further, the emissions of NH3 were underestimated during our case studies. Airborne SOF is a versatile tool that in principle is capable to measure many other gases. 

Professor Volkamer, an academic professor and CIRES Fellow who lead the project, spent a productive sabbatical stay in Europe. In collaboration with KIT, Germany his research group explored creative new ways to quantify and disentangle methane emissions from natural and anthropogenic sources by relatively low-cost COCCON type networks of column sensors, and simultaneous measurements of chemical tracers by CU SOF. In a proof-of-concept study it is shown that the relative contributions of different source sectors can be disentangled using small networks designed for longer-term operation on regional scales. 

Furthermore, in collaboration with Dr. Michael Hoepfner at KIT, infrared emission spectroscopy was used to detect NH3 in the free troposphere (FT). There are no previous measurements of NH3 in the upper troposphere, where even small amounts of NH3 can form ammonium sulfate aerosol, and have potential to strongly modify new particle formation and growth at cold temperatures in the upper troposphere.

Aerosols are harmful to human health, and their properties can modify clouds and rain fall. The oxidation of sulfur dioxide and isoprene in cloud droplets were studied at the CLOUD simulation chamber at CERN, Switzerland, in bench-top experiments in Boulder, and through modeling. We have measured Setschenow salting constants of glyoxal and methyl glyoxal, and estimated that of isoprene epoxide. These three molecules are formed from isoprene, and are deemed responsible to form aerosol mass from multiphase chemistry in suspended droplets (aerosols and clouds) over forests. The laboratory findings were incorporated into the CMAQ model (collaboration with Professor Carlton, now UC Irvine), and suggest that anthropogenic sulfate could regulate biogenic aerosol formation in ways not presently included in atmospheric models. In collaboration with Professor Amman at the Paul Scherrer Institute, Switzerland, surface reactions of light absorbing products from glyoxal multiphase chemistry were shown to be a source of radical species at aqueous interfaces. Finally, fatty acid photochemistry as a source of small oxygenated volatile organic carbon (OVOC) molecules found over oceans were explored in a photochemical reactor that simulates the ocean surface in collaboration with Dr. George at IRCELYON, France. 

The broader impacts of this project are that a principal investigator engaged new disciplines through collaborations with experts in infrared spectroscopy, aerosol formation and growth, and photocatalysis. Five graduate students, one postdoc, and one undergraduate student received training on the development of instrumentation for use from mobile platforms (ground, aircraft), conducted field observations and laboratory research as part of interdisciplinary teams, engaged novel disciplines, and interacted with researchers in National Laboratories in Germany, France, Switzerland, and the US. The project has contributed to the development of a globally engaged work force in environmental science, and provided training beyond the laboratory bench that is useful for careers in academia, government and/or industry.


Last Modified: 12/18/2017
Modified by: Rainer M Volkamer

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