4 research outputs found
Volatility of organic aerosol and its components in the megacity of Paris
Using a mass transfer model and the volatility basis set, we estimate the
volatility distribution for the organic aerosol (OA) components during summer
and winter in Paris, France as part of the collaborative project MEGAPOLI.
The concentrations of the OA components as a function of temperature were
measured combining data from a thermodenuder and an aerosol mass spectrometer
(AMS) with Positive Matrix Factorization (PMF) analysis. The hydrocarbon-like
organic aerosol (HOA) had similar volatility distributions for the summer and
winter campaigns with half of the material in the saturation concentration
bin of 10 µg m<sup>−3</sup> and another 35–40 % consisting of low
and extremely low volatility organic compounds (LVOCs with effective
saturation concentrations <i>C</i>* of 10<sup>−3</sup>–0.1 µg m<sup>−3</sup> and
ELVOCs <i>C</i>* less or equal than 10<sup>−4</sup> µg m<sup>−3</sup>,
respectively). The winter cooking OA (COA) was more than an order of
magnitude less volatile than the summer COA. The low-volatility oxygenated OA
(LV-OOA) factor detected in the summer had the lowest volatility of all the
derived factors and consisted almost exclusively of ELVOCs. The volatility
for the semi-volatile oxygenated OA (SV-OOA) was significantly higher than
that of the LV-OOA, containing both semi-volatile organic components (SVOCs
with <i>C</i>* in the 1–100 µg m<sup>−3</sup> range) and LVOCs. The
oxygenated OA (OOA) factor in winter consisted of SVOCs (45 %), LVOCs
(25 %) and ELVOCs (30 %). The volatility of marine OA (MOA) was
higher than that of the other factors containing around 60 % SVOCs. The
biomass burning OA (BBOA) factor contained components with a wide range of
volatilities with significant contributions from both SVOCs (50 %) and
LVOCs (30 %). Finally, combining the bulk average O : C ratios and
volatility distributions of the various factors, our results are placed into
the two-dimensional volatility basis set (2D-VBS) framework. The OA factors
cover a broad spectrum of volatilities with no direct link between the
average volatility and average O : C of the OA components
Simulation of atmospheric organic aerosol using its volatility–oxygen-content distribution during the PEGASOS 2012 campaign
A lot of effort has been made to understand and constrain the
atmospheric aging of the organic aerosol (OA). Different parameterizations of
the organic aerosol formation and evolution in the two-dimensional volatility
basis set (2D-VBS) framework are evaluated using ground and airborne
measurements collected in the 2012 Pan-European Gas
AeroSOls-climate interaction Study (PEGASOS) field campaign in the Po
Valley (Italy). A number of chemical aging schemes are examined, taking into
account various functionalization and fragmentation pathways for biogenic and
anthropogenic OA components. Model predictions and measurements, both at the
ground and aloft, indicate a relatively oxidized OA with little average
diurnal variation. Total OA concentration and O : C ratios
are reproduced within experimental error by a number of chemical aging
schemes. Anthropogenic secondary OAÂ (SOA) is predicted to contribute
15–25 % of the total OA, while SOA from intermediate volatility
compound oxidation contributes another 20–35 %. Biogenic SOA (bSOA) contributions varied
from 15 to 45 % depending on the modeling scheme. Primary OA contributed
around 5 % for all schemes and was comparable to the hydrocarbon-like
OAÂ (HOA) concentrations derived from the positive matrix factorization of the
aerosol mass spectrometer (PMF-AMS) ground measurements. The average OA and
O : C diurnal variation and their vertical profiles showed
a surprisingly modest sensitivity to the assumed vaporization enthalpy for
all aging schemes. This can be explained by the interplay between the
partitioning of the semi-volatile compounds and their gas-phase chemical
aging reactions.</p
A Systematic Review of the Treatment of Fears and Phobias Among Children with Autism Spectrum Disorders
Research indicates that fears and phobias are significantly more prevalent and emerge in response to a greater variety of stimuli, among children with autism spectrum disorders (ASD) than among their developmentally disabled or typically developing peers. Such findings are problematic given the difficulty of assessing and identifying fears or phobias among the ASD population and the challenge of identifying effective treatments for those with core diagnostic deficits in comprehension, communication, and attentional skills. The current review aimed to evaluate the literature describing interventions to treat fears, specific phobia, or social phobia among children with ASD and to identify evidence-based practice in this area. The review indicated that a variety of interventions, described as both traditional and novel, were successful in treating fearful or phobic behavioral responses to stimuli. The findings also suggest that behavioral intervention, including reinforcement, modeling, and exposure, may be considered evidence-based practice in the treatment of fears and phobias among children with ASD. However, the current research base is limited by the predominant focus on the behavioral element of the fear response, and the lack of research examining the cognitive or physiological responses during assessment or treatment