A two-dimensional volatility basis set: 1. organic-aerosol mixing thermodynamics
By N. Donahue, S. Epstein, Spyros N. Pandis, A. Robinson. 2010
754 citations recorded by the source corpus.
We develop the thermodynamic underpinnings of a two-dimensional volatility basis set (2D-VBS) employ- ing saturation mass concentration (C o ) and the oxygen con- tent (O:C) to describe volatility, mixing thermodynamics, and chemical evolution of organic aerosol. The work ad- dresses a simple question: "Can we reasonably constrain organic-aerosol composition in the atmosphere based on only two measurable organic properties, volatility and the extent of oxygenation?" This is an extension of our earlier one- dimensional approach employing volatility only (C = C o , where is an activity coefficient). Using available con- straints on bulk organic-aerosol composition, we argue that one can reasonably predict the composition of organics (car- bon, oxygen and hydrogen numbers) given a location in the C o - O:C space. Further, we argue that we can constrain the activity coefficients at various locations in this space based on the O:C of the organic aerosol.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/f42a9e50c4e8958d7192542f8ed0fb4a1d485f81
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In Atmospheric Science
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- B. Aumont
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- Julia Laskin
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In Global and Planetary Change
- G. Isaacman-VanWertz
- B. Aumont
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- M. Shiraiwa
- Paul O. Wennberg
- D. Worsnop
Citations in the corpus
- Online coupled regional meteorology chemistry models in Europe: current status and prospects (2013, background): “The approach has been recently extended to account also for the degree of oxidation of SOA species (Donahue et al., 2011).”
- Predicting the glass transition temperature and viscosity of secondary organic material using molecular composition (2017, methodology): “1a in Shiraiwa et al. (2017)), we use an equation with a similar formulation to the 182 equation used to predict the saturation mass concentration or volatility (Donahue et al., 2011; Li 183 et al., 2016): 184 Tg = (𝑛!!”
- Understanding atmospheric organic aerosols via factor analysis of aerosol mass spectrometry: a review (2011, background): “Because both of these axes can be experimentally obtained, this 2D model provides a useful framework for describing OA evolution that can be constrained by measurements [111].”
- Highly Oxygenated Organic Molecules (HOM) from Gas-Phase Autoxidation Involving Peroxy Radicals: A Key Contributor to Atmospheric Aerosol (2019, methodology): “This assumption of extremely low vapor pressure was motivated in part by utilizing existing structure−activity relationships (SAR) (e.g., (Donahue et al., 2011) for the observed elemental compositions).28 Ehn et al. (2014) also showed that the behavior of the observed molecules when in contact with…”
- Impact of organic molecular structure on the estimation of atmospherically relevant physicochemical parameters (2021, methodology): “…of compounds across∼ 15 orders of magnitude in vapor pressure (Jimenez et al., 2009), wide ranges of oxygenation, volatility and solubility (e.g., Donahue et al., 2011; Hodzic et al., 2014; Lannuque et al., 2018), and several orders of magnitude in reactivities (Lee et al., 2006), with many…”