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Molecular composition and volatility of isoprene photochemical oxidation secondary organic aerosol under low- and high-NOx conditions

D'Ambro, E. L. (author)
Lee, B. H. (author)
Liu, J. M. (author)
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Shilling, J. E. (author)
Gaston, C. J. (author)
Lopez-Hilfiker, F. D. (author)
Schobesberger, S. (author)
Zaveri, R. A. (author)
Mohr, C. (author)
Lutz, Anna, 1986 (author)
Gothenburg University,Göteborgs universitet,Institutionen för kemi och molekylärbiologi,Department of Chemistry and Molecular Biology
Zhang, Z. F. (author)
Gold, A. (author)
Surratt, J. D. (author)
Rivera-Rios, J. C. (author)
Keutsch, F. N. (author)
Thornton, J. A. (author)
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 (creator_code:org_t)
2017-01-04
2017
English.
In: Atmospheric Chemistry and Physics. - : Copernicus GmbH. - 1680-7316 .- 1680-7324. ; 17:1, s. 159-174
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • We present measurements of secondary organic aerosol (SOA) formation from isoprene photochemical oxidation in an environmental simulation chamber at a variety of oxidant conditions and using dry neutral seed particles to suppress acid-catalyzed multiphase chemistry. A high-resolution time-of-flight chemical ionization mass spectrometer (HR-ToF-CIMS) utilizing iodide-adduct ionization coupled to the Filter Inlet for Gases and Aerosols (FIGAERO) allowed for simultaneous online sampling of the gas and particle composition. Under high-HO2 and low-NO conditions, highly oxygenated (O : C >= 1) C-5 compounds were major components (similar to 50 %) of SOA. The SOA composition and effective volatility evolved both as a function of time and as a function of input NO concentrations. Organic nitrates increased in both the gas and particle phases as input NO increased, but the dominant non-nitrate particle-phase components monotonically decreased. We use comparisons of measured and predicted gas-particle partitioning of individual components to assess the validity of literature-based group-contribution methods for estimating saturation vapor concentrations. While there is evidence for equilibrium partitioning being achieved on the chamber residence timescale (5.2 h) for some individual components, significant errors in group-contribution methods are revealed. In addition, >30% of the SOA mass, detected as low-molecular-weight semivolatile compounds, cannot be reconciled with equilibrium partitioning. These compounds desorb from the FIGAERO at unexpectedly high temperatures given their molecular composition, which is indicative of thermal decomposition of effectively lower-volatility components such as larger molecular weight oligomers.

Subject headings

NATURVETENSKAP  -- Kemi -- Analytisk kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences -- Analytical Chemistry (hsv//eng)
NATURVETENSKAP  -- Kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences (hsv//eng)
NATURVETENSKAP  -- Kemi -- Organisk kemi (hsv//swe)
NATURAL SCIENCES  -- Chemical Sciences -- Organic Chemistry (hsv//eng)

Keyword

southeastern united-states
vapor-pressure estimation
alpha-pinene
reactive uptake
soa formation
2-methylglyceric acid
biogenic
emissions
epoxide formation
cross-sections
photooxidation
Meteorology & Atmospheric Sciences

Publication and Content Type

ref (subject category)
art (subject category)

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