Mechanism Development and Structure-Activity Relationships for Gas-Phase Atmospheric Chemistry

A special issue of Atmosphere (ISSN 2073-4433). This special issue belongs to the section "Air Quality".

Deadline for manuscript submissions: closed (1 August 2022) | Viewed by 2780

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Department of Physics, University of Texas at El Paso, El Paso, TX 79968, USA
Interests: atmospheric chemistry; air quality modeling; biosphere–atmosphere interactions; public policy
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Guest Editor
Howard University, Washington, DC 20059, USA
Interests: atmospheric chemistry; air quality modeling; public policy; human health; chemical mechanims

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Guest Editor
Air Quality Research Center, University of California, Davis, CA 95616, USA
Interests: atmospheric chemistry; chemical mechanisms; air quality modeling; public policy; low-cost air sensors

Special Issue Information

Dear Colleagues,

Ozone, particulate matter and atmospheric acids adversely affect human health, the environment and climate. Atmospheric gas-phase chemistry plays a critical role in determining the concentrations of these air pollutants. The gas-phase chemistry of the atmosphere is very complex. Much of the chemistry in the lower troposphere is dominated by the reactions of nitrogen oxides and volatile organic compounds. Sulfur dioxide and ammonia emissions also contribute to the formation of particulate matter. Atmospheric inorganic chemistry is relatively straightforward compared with the chemistry of volatile organic compounds. There are at least thousands of anthropogenic and biogenic organic compounds emitted. Each compound may form many other unique compounds and intermediates when it oxidizes in the atmosphere. Therefore, a complete gas-phase atmospheric chemical mechanism consists of on-the-order-of several million reactions and compounds. Now, there are important efforts to build highly detailed gas-phase mechanisms that attempt to be as complete as possible. However, many of the required reactions for highly detailed mechanisms must be constructed from structure–activity relationships. The development of highly detailed gas-phase mechanisms is a very valuable component of atmospheric chemistry research. On the other hand, more simplified gas-phase atmospheric chemical mechanisms are used in meteorological air quality models for making public policy. Both types of chemical mechanisms and their development procedures are of interest for this Special Issue. Methods of condensation, including machine learning and other approaches, used to link the development of simplified mechanisms to the highly detailed gas-phase mechanisms are of deep interest for this Special Issue.

Prof. Dr. William R. Stockwell
Dr. Emily Saunders
Dr. Ajith Kaduwela
Guest Editors

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Keywords

  • atmospheric chemistry
  • structure-activity relationships
  • air quality
  • ozone
  • particulate matter
  • nitrogen oxides
  • volatile organic compounds
  • halogens
  • sulfurous compounds
  • mechanism condensation

Published Papers (1 paper)

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Research

23 pages, 1435 KiB  
Article
Estimation of Rate Constants for Reactions of Organic Compounds under Atmospheric Conditions
by William P. L. Carter
Atmosphere 2021, 12(10), 1250; https://doi.org/10.3390/atmos12101250 - 26 Sep 2021
Cited by 1 | Viewed by 1732
Abstract
Structure–activity (SAR) methods are presented for estimating rate constants at 298 K and approximate temperature dependences for the reactions of organic compounds with OH, NO3, and Cl radicals and O3, and O(3P) in the lower atmosphere. These [...] Read more.
Structure–activity (SAR) methods are presented for estimating rate constants at 298 K and approximate temperature dependences for the reactions of organic compounds with OH, NO3, and Cl radicals and O3, and O(3P) in the lower atmosphere. These are needed for detailed mechanisms for the atmospheric reactions of organic compounds. Base rate constants are assigned for the various types of H-abstraction and addition reactions, with correction factors for substituents around the reaction site and in some cases for rings and molecule structure or size. Rate constant estimates are made for hydrocarbons and a wide variety of oxygenates, organic nitrates, amines, and monosubstituted halogen compounds. Rate constants for most hydrocarbons and monofunctional compounds can be estimated to within ±30%, though predictions are not as good for multifunctional compounds, and predictions for ~15% of the rate constants are off by more than a factor of 2. Estimates are more uncertain in the case of NO3 and O3 reactions. The results serve to demonstrate the capabilities and limitations of empirical methods for predicting rate constants for the full variety of organic compounds that may be of interest. Areas where future work is needed are discussed. Full article
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