2018
DOI: 10.5194/amt-11-49-2018
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A reference data set for validating vapor pressure measurement techniques: homologous series of polyethylene glycols

Abstract: Abstract. To predict atmospheric partitioning of organic compounds between gas and aerosol particle phase based on explicit models for gas phase chemistry, saturation vapor pressures of the compounds need to be estimated. Estimation methods based on functional group contributions require training sets of compounds with well-established saturation vapor pressures. However, vapor pressures of semivolatile and low-volatility organic molecules at atmospheric temperatures reported in the literature often differ by … Show more

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Cited by 53 publications
(72 citation statements)
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References 43 publications
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“…Once trapped, a single particle sits in a nitrogen flow (200 mL min −1 , gas flow velocity of 3 cm s −1 ) of controlled RH and T . The RH is measured by fitting either the size vs. time profile of an evaporating probe water droplet (at RHs above 80 %) or the equilibrated radius of a NaCl or NaNO 3 aqueous solution probe droplet (below 80 %) by applying a literature evaporation-condensation kinetic model (Kulmala et al, 1993). The procedure is described in Rovelli et al (2016), where the uncertainties associated with the measured RH are also discussed (typically < ±0.2 % at RH > 90 % and ∼ ±1 % below 90 %).…”
Section: Experimental Oa Evaporation Datamentioning
confidence: 99%
“…Once trapped, a single particle sits in a nitrogen flow (200 mL min −1 , gas flow velocity of 3 cm s −1 ) of controlled RH and T . The RH is measured by fitting either the size vs. time profile of an evaporating probe water droplet (at RHs above 80 %) or the equilibrated radius of a NaCl or NaNO 3 aqueous solution probe droplet (below 80 %) by applying a literature evaporation-condensation kinetic model (Kulmala et al, 1993). The procedure is described in Rovelli et al (2016), where the uncertainties associated with the measured RH are also discussed (typically < ±0.2 % at RH > 90 % and ∼ ±1 % below 90 %).…”
Section: Experimental Oa Evaporation Datamentioning
confidence: 99%
“…Based on the limited number of direct comparisons between predicted and experimental data, and further assuming that the effect is roughly proportional to the maximum number of intramolecular H-bonds, the overestimation seems to be on the order of a factor of 5 per H-bond. If applied to the data in Kurtén et al (2016) on monoterpene autoxidation products, this would imply that the originally suggested approach of taking the geometric average of SIMPOL and COSMOtherm saturation vapor pressure predictions remains a reasonably good choice in the absence of other information. While COSMOtherm saturation vapor pressure predictions can be modified to agree better with experiments by scaling the hydrogen bond enthalpy parameter c1, the optimal value for this parameter is likely to depend on the system, and this approach can thus not generally be recommended.…”
Section: Atmospheric Implications and Conclusionmentioning
confidence: 99%
“…CC BY 4.0 License. measured at room temperature, demonstrating their thermal stability (Krieger et al, 2018). The stability of the PEG compounds allowed samples to be shared between the co-authors of Krieger et al, (2018), ensuring sample conformity.…”
Section: Choice Of Reference Compoundsmentioning
confidence: 95%
“…The vapour pressure of the Polyethylene glycol (PEG) series, as described in the Krieger et al, (2018) study, were measured by multiple techniques; KEMS (Booth et al, 2009), electrodynamic balance instruments (Zardini et al, 2006;Rovelli et al, 2016) and Tandem Differential Mobility Analyser (TDMA) including a laminar flow tube (Bilde et al, 2003)).…”
Section: Choice Of Reference Compoundsmentioning
confidence: 99%