5 research outputs found
Predicting Thermal Behavior of Secondary Organic Aerosols
Volume
concentrations of secondary organic aerosol (SOA) are measured
in 139 steady-state, single precursor hydrocarbon oxidation experiments
after passing through a temperature controlled inlet. The response
to change in temperature is well predicted through a feedforward Artificial
Neural Network. The most parsimonious model, as indicated by Akaike’s
Information Criterion, Corrected (AIC,C), utilizes 11 input variables,
a single hidden layer of 4 tanh activation function nodes, and a single
linear output function. This model predicts thermal behavior of single
precursor aerosols to less than ±5%, which is within the measurement
uncertainty, while limiting the problem of overfitting. Prediction
of thermal behavior of SOA can be achieved by a concise number of
descriptors of the precursor hydrocarbon including the number of internal
and external double bonds, number of methyl- and ethyl- functional
groups, molecular weight, and number of ring structures, in addition
to the volume of SOA formed, and an indicator of which of four oxidant
precursors was used to initiate reactions (NO<sub><i>x</i></sub> photo-oxidation, photolysis of H<sub>2</sub>O<sub>2</sub>,
ozonolysis, or thermal decomposition of N<sub>2</sub>O<sub>5</sub>). Additional input variables, such as chamber volumetric residence
time, relative humidity, initial concentration of oxides of nitrogen,
reacted hydrocarbon concentration, and further descriptors of the
precursor hydrocarbon, including carbon number, number of oxygen atoms,
and number of aromatic ring structures, lead to over fit models, and
are unnecessary for an efficient, accurate predictive model of thermal
behavior of SOA. This work indicates that predictive statistical modeling
methods may be complementary to descriptive techniques for use in
parametrization of air quality models
Trends in the oxidation and relative volatility of chamber-generated secondary organic aerosol
<p>The relationship between the oxidation state and relative volatility of secondary organic aerosol (SOA) from the oxidation of a wide range of hydrocarbons is investigated using a fast-stepping, scanning thermodenuder interfaced with a high-resolution time-of-flight aerosol mass spectrometer (AMS). SOA oxidation state varied widely across the investigated range of parent hydrocarbons but was relatively stable for replicate experiments using a single hydrocarbon precursor. On average, unit mass resolution indicators of SOA oxidation (e.g., AMS <i>f</i><sub>43</sub> and <i>f</i><sub>44</sub>) are consistent with previously reported values. Linear regression of H:C vs. O:C obtained from parameterization of <i>f</i><sub>43</sub> and <i>f</i><sub>44</sub> and elemental analysis of high-resolution spectra in Van Krevelen space both yield a slope of ∼−0.5 across different SOA types. A similar slope was obtained for a distinct subset of toluene/NO<i><sub>x</sub></i> reactions in which the integrated oxidant exposure was varied to alter oxidation. The relative volatility of different SOA types displays similar variability and is strongly correlated with SOA oxidation state (<sub>C</sub>). On average, relatively low oxidation and volatility were observed for aliphatic alkene (including terpenes) and <i>n-</i>alkane SOA while the opposite is true for mono- and polycyclic aromatic hydrocarbon SOA. Effective enthalpy for total chamber aerosol obtained from volatility differential mobility analysis is also highly correlated with <sub>C</sub> indicating a primary role for oxidation levels in determining the volatility of chamber SOA. Effective enthalpies for chamber SOA are substantially lower than those of neat organic standards but are on the order of those obtained for partially oligomerized glyoxal and methyl glyoxal.</p> <p>© 2018 American Association for Aerosol Research</p
Photochemical Conversion of Surrogate Emissions for Use in Toxicological Studies: Role of Particulate- and Gas-Phase Products
The production of photochemical atmospheres
under controlled conditions
in an irradiation chamber permits the manipulation of parameters that
influence the resulting air-pollutant chemistry and potential biological
effects. To date, no studies have examined how contrasting atmospheres
with a similar Air Quality Health Index (AQHI), but with differing
ratios of criteria air pollutants, might differentially affect health
end points. Here, we produced two atmospheres with similar AQHIs based
on the final concentrations of ozone, nitrogen dioxide, and particulate
matter (PM<sub>2.5</sub>). One simulated atmosphere (SA-PM) generated
from irradiation of ∼23 ppmC gasoline, 5 ppmC α-pinene,
529 ppb NO, and 3 μg m<sup>–3</sup> (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> as a seed resulted in an average of 976 μg
m<sup>–3</sup> PM<sub>2.5</sub>, 326 ppb NO<sub>2</sub>, and
141 ppb O<sub>3</sub> (AQHI 97.7). The other atmosphere (SA-O<sub>3</sub>) generated from 8 ppmC gasoline, 5 ppmC isoprene, 874 ppb
NO, and 2 μg m<sup>–3</sup> (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub> resulted in an average of 55 μg m<sup>–3</sup> PM<sub>2.5</sub>, 643 ppb NO<sub>2</sub>, and 430 ppb O<sub>3</sub> (AQHI of 99.8). Chemical speciation by gas chromatography showed
that photo-oxidation degraded the organic precursors and promoted
the de novo formation of secondary reaction products such as formaldehyde
and acrolein. Further work in accompanying papers describe toxicological
outcomes from the two distinct photochemical atmospheres
2‑Hydroxyterpenylic Acid: An Oxygenated Marker Compound for α‑Pinene Secondary Organic Aerosol in Ambient Fine Aerosol
An oxygenated MW 188 compound is
commonly observed in substantial
abundance in atmospheric aerosol samples and was proposed in previous
studies as an α-pinene-related marker compound that is associated
with aging processes. Owing to difficulties in producing this compound
in sufficient amounts in laboratory studies and the occurrence of
isobaric isomers, a complete assignment for individual MW 188 compounds
could not be achieved in these studies. Results from a comprehensive
mass spectrometric analysis are presented here to corroborate the
proposed structure of the most abundant MW 188 compound as a 2-hydroxyterpenylic
acid diastereoisomer with 2<i>R</i>,3<i>R</i> configuration.
The application of collision-induced dissociation with liquid chromatography/electrospray
ionization-ion trap mass spectrometry in both negative and positive
ion modes, as well as chemical derivatization to methyl ester derivatives
and analysis by the latter technique and gas chromatography/electron
ionization mass spectrometry, enabled a comprehensive characterization
of MW 188 isomers, including a detailed study of the fragmentation
behavior using both mass spectrometric techniques. Furthermore, a
MW 188 positional isomer, 4-hydroxyterpenylic acid, was tentatively
identified, which also is of atmospheric relevance as it could be
detected in ambient fine aerosol. Quantum chemical calculations were
performed to support the diastereoisomeric assignment of the 2-hydroxyterpenylic
acid isomers. Results from a time-resolved α-pinene photooxidation
experiment show that the 2-hydroxyterpenylic acid 2<i>R</i>,3<i>R</i> diastereoisomer has a time profile distinctly
different from that of 3-methyl-1,2,3-butanetricarboxylic acid, a
marker for oxygenated (aged) secondary organic aerosol. This study
presents a comprehensive chemical data set for a more complete structural
characterization of hydroxyterpenylic acids in ambient fine aerosol,
which sets the foundation to better understand the atmospheric fate
of α-pinene in future studies
Epoxide Pathways Improve Model Predictions of Isoprene Markers and Reveal Key Role of Acidity in Aerosol Formation
Isoprene significantly contributes
to organic aerosol in the southeastern
United States where biogenic hydrocarbons mix with anthropogenic emissions.
In this work, the Community Multiscale Air Quality model is updated
to predict isoprene aerosol from epoxides produced under both high-
and low-NO<sub><i>x</i></sub> conditions. The new aqueous
aerosol pathways allow for explicit predictions of two key isoprene-derived
species, 2-methyltetrols and 2-methylglyceric acid, that are more
consistent with observations than estimates based on semivolatile
partitioning. The new mechanism represents a significant source of
organic carbon in the lower 2 km of the atmosphere and captures the
abundance of 2-methyltetrols relative to organosulfates during the
simulation period. For the parametrization considered here, a 25%
reduction in SO<sub><i>x</i></sub> emissions effectively
reduces isoprene aerosol, while a similar reduction in NO<sub><i>x</i></sub> leads to small increases in isoprene aerosol