Environmental Science Processes & Impacts,
Journal Year:
2017,
Volume and Issue:
19(10), P. 1220 - 1234
Published: Jan. 1, 2017
This
study
presents
a
newly
constructed
temperature
controlled
cold-room
smog
chamber
at
Aarhus
University,
Denmark.
The
is
herein
utilized
to
the
effect
of
sub-zero
on
formation
and
chemical
composition
secondary
organic
aerosol
(SOA)
from
ozone
initiated
oxidation
α-pinene.
α-pinene
SOA
formed
dark
ozonolysis
293
K
258
was
investigated
using
High-Resolution
Time-of-Flight
Aerosol
Mass
Spectrometry
(HR-ToF-AMS)
Ultra-High
Performance
Liquid
Chromatography/Electrospray
Ionization
Quadrupole
(UHPLC/ESI-qToF-MS).
For
comparison,
an
OH-initiated
experiment
performed
K.
In
experiments
it
found
that
oxygen-to-carbon
(O
:
C)
ratios
were
higher
in
particles
compared
A
total
16
different
acids
30
dimers
esters
quantified
collected
composing
up
34%
mass
with
increased
fraction
carboxylic
contrast,
dimer
showed
suppressed
reaction
temperature,
thus
contributing
3%
while
9%
resulted
low
concentrations
supporting
Criegee
intermediates
as
possible
pathway
ester
formation.
Vapour
pressure
estimates
identified
are
presented
show
how
otherwise
semi-volatile
sufficiently
temperatures
may
classify
or
even
extremely
volatile
compounds
(ELVOC),
add
enhanced
particle
observed
through
gas-to-particle
conversion.
change
ascribed
combination
effects:
decreased
vapour
pressures
hence
condensation
gas
phase
along
high
molecular
weight
chemistry
results
consequence
temperatures.
Reviews of Geophysics,
Journal Year:
2017,
Volume and Issue:
55(2), P. 509 - 559
Published: May 18, 2017
Abstract
Anthropogenic
emissions
and
land
use
changes
have
modified
atmospheric
aerosol
concentrations
size
distributions
over
time.
Understanding
preindustrial
conditions
in
organic
due
to
anthropogenic
activities
is
important
because
these
features
(1)
influence
estimates
of
radiative
forcing
(2)
can
confound
the
historical
response
climate
increases
greenhouse
gases.
Secondary
(SOA),
formed
atmosphere
by
oxidation
gases,
represents
a
major
fraction
global
submicron‐sized
aerosol.
Over
past
decade,
significant
advances
understanding
SOA
properties
formation
mechanisms
occurred
through
measurements,
yet
current
models
typically
do
not
comprehensively
include
all
processes.
This
review
summarizes
some
developments
during
decade
formation.
We
highlight
importance
processes
that
growth
particles
sizes
relevant
for
clouds
forcing,
including
extremely
low
volatility
organics
gas
phase,
acid‐catalyzed
multiphase
chemistry
isoprene
epoxydiols,
particle‐phase
oligomerization,
physical
such
as
viscosity.
Several
highlighted
this
are
complex
interdependent
nonlinear
effects
on
properties,
formation,
evolution
SOA.
Current
neglect
complexity
nonlinearity
thus
less
likely
accurately
predict
project
future
sensitivity
Efforts
also
needed
rank
most
influential
process‐related
interactions,
so
be
represented
chemistry‐climate
models.
Reviews of Geophysics,
Journal Year:
2019,
Volume and Issue:
57(2), P. 187 - 249
Published: March 21, 2019
Abstract
Atmospheric
aerosols
are
complex
mixtures
of
different
chemical
species,
and
individual
particles
exist
in
many
shapes
morphologies.
Together,
these
characteristics
contribute
to
the
aerosol
mixing
state.
This
review
provides
an
overview
measurement
techniques
probe
state,
discusses
how
state
is
represented
atmospheric
models
at
scales,
synthesizes
our
knowledge
state's
impact
on
climate‐relevant
properties,
such
as
cloud
condensation
ice
nucleating
particle
concentrations,
optical
properties.
We
present
findings
within
a
framework
that
defines
along
with
appropriate
metrics
quantify
it.
Future
research
directions
identified,
focus
need
for
integrating
measurements
modeling.
Atmospheric measurement techniques,
Journal Year:
2019,
Volume and Issue:
12(4), P. 2403 - 2421
Published: April 17, 2019
Abstract.
The
impact
of
aerosols
on
climate
and
air
quality
remains
poorly
understood
due
to
multiple
factors.
One
the
current
limitations
is
incomplete
understanding
contribution
oxygenated
products,
generated
from
gas-phase
oxidation
volatile
organic
compounds
(VOCs),
aerosol
formation.
Indeed,
atmospheric
gaseous
chemical
processes
yield
thousands
(highly)
species,
spanning
a
wide
range
formulas,
functional
groups
and,
consequently,
volatilities.
While
recent
mass
spectrometric
developments
have
allowed
extensive
on-line
detection
myriad
playing
central
role
in
chemistry,
detailed
quantification
characterization
this
diverse
group
extremely
challenging.
To
address
challenge,
we
evaluated
capability
state-of-the-art
spectrometers
equipped
with
different
ionization
sources
detect
products
formed
α-Pinene
ozonolysis
under
various
conditions.
Five
were
deployed
simultaneously
for
chamber
study.
Two
pressure
interface
time-of-flight
(CI-APi-TOF)
nitrate
amine
reagent
ion
chemistries
an
iodide
spectrometer
(TOF-CIMS)
used.
Additionally,
proton
transfer
reaction
(PTR-TOF
8000)
new
“vocus”
PTR-TOF
also
deployed.
In
study,
compared
around
1000
between
each
five
instruments,
aim
determining
which
VOCs
(OVOCs)
methods
sensitive
identifying
regions
where
two
or
more
instruments
able
species
similar
molecular
formulae.
We
utilized
large
variability
conditions
(including
VOCs,
ozone,
NOx
OH
scavenger
concentrations)
our
newly
constructed
simulation
comprehensive
correlation
analysis
all
instruments.
This
analysis,
combined
estimated
concentrations
identified
molecules
instrument,
yielded
both
expected
surprising
results.
As
anticipated
based
earlier
studies,
PTR
only
ones
measure
precursor
VOC,
TOF-CIMS
efficiently
detected
many
semi-volatile
(SVOCs)
three
oxygen
atoms,
CI-APi-TOF
was
mainly
highly
(O
>
5)
(HOMs).
addition,
vocus
showed
good
agreement
SVOC,
including
organonitrates.
agreed
well
HOM
dimers.
However,
loadings
experiments
caused
be
considerably
depleted,
causing
nonlinear
responses
monomers.
study
explores
highlights
benefits
currently
available
spectrometry
instrumentation
characterizing
variety
OVOCs
atmosphere.
specifically
shown
case
ozonolysis,
expect
general
findings
valid
other
VOC–oxidant
systems.
discussed
no
single
instrument
configuration
can
deemed
better
worse
than
others,
as
optimal
particular
ultimately
depends
specific
target
Atmospheric chemistry and physics,
Journal Year:
2018,
Volume and Issue:
18(19), P. 13839 - 13863
Published: Oct. 1, 2018
Abstract.
The
concentrations
of
terpenoids
(isoprene;
monoterpenes,
MTs;
and
sesquiterpenes,
SQTs)
oxygenated
volatile
organic
compounds
(OVOCs;
i.e.
aldehydes,
alcohols,
acetates
acids,
VOAs)
were
investigated
during
2
years
at
a
boreal
forest
site
in
Hyytiälä,
Finland,
using
situ
gas
chromatograph
mass
spectrometers
(GC-MSs).
Seasonal
diurnal
variations
terpenoid
OVOC
as
well
their
relationship
with
meteorological
factors
studied.
Of
the
VOCs
examined,
C2–C7
unbranched
VOAs
showed
highest
concentrations,
mainly
due
to
low
reactivity.
terpenoids,
MTs
site,
but
seven
different
highly
reactive
SQTs
also
detected.
monthly
daily
mean
most
aldehydes
dependent
on
temperature.
exponential
correlation
temperature
was
found
for
SQT
(β-caryophyllene)
summer.
could
be
explained
by
sources,
sinks
vertical
mixing.
MT
strongly
affected
Based
correlations
mixing
layer
height
(MLH),
simple
proxies
developed
estimating
concentrations.
To
estimate
importance
compound
groups
local
atmospheric
chemistry,
reactivity
main
oxidants
(hydroxyl
radical,
OH;
nitrate
NO3;
ozone,
O3)
production
rates
oxidation
products
(OxPRs)
calculated.
dominated
OH
NO3
radical
greatly
impacted
O3
even
though
30
times
lower
than
important
products.
Since
show
high
secondary
aerosol
(SOA)
yields,
results
clearly
indicate
SOA
production.
Environmental Science & Technology,
Journal Year:
2016,
Volume and Issue:
51(1), P. 119 - 127
Published: Dec. 8, 2016
Secondary
organic
aerosol
(SOA),
formed
in
the
photooxidation
of
diesel
fuel,
biodiesel
and
20%
fuel/80%
fuel
mixture,
are
prepared
under
high-NOx
conditions
presence
absence
sulfur
dioxide
(SO2),
ammonia
(NH3),
relative
humidity
(RH).
The
composition
condensed-phase
compounds
SOA
is
measured
using
several
complementary
techniques
including
mass
spectrometry
(AMS),
high-resolution
nanospray
desorption
electrospray
ionization
(nano-DESI/HRMS),
ultrahigh
resolution
accuracy
21T
Fourier
transform
ion
cyclotron
resonance
(21T
FT-ICR
MS).
Results
demonstrate
that
sulfuric
acid
condensed
organosulfur
species
experiments
with
SO2
present
particles.
Fewer
high
experiments,
performed
at
RH
90%,
comparison
done
dry
conditions.
There
a
strong
overlap
observed
this
study
previous
field
chamber
studies
SOA.
Many
MS
peaks
organosulfates
(R–OS(O)2OH)
previously
designated
as
biogenic
or
unknown
origin
might
have
originated
from
anthropogenic
sources,
such
hydrocarbons
fuel.
Environmental Science & Technology Letters,
Journal Year:
2018,
Volume and Issue:
5(7), P. 424 - 430
Published: June 11, 2018
Adverse
health
effects
due
to
exposure
particulate
matter
(PM)
are
among
the
most
important
global
environmental
risks.
However,
of
secondary
organic
aerosols
(SOA),
a
major
component
aerosol,
largely
unknown.
Here
we
exposed
lung
epithelial
cells
(A549)
fresh
and
aged
SOA
particles
investigated
effect
atmospheric
aging
on
cell
viability
gene
expression.
Naphthalene-
α-pinene-derived
were
formed
in
an
oxidation
flow
reactor
that
simulates
formation
dominated
by
OH
radical
under
NOx-free
conditions.
The
mass
chemical
composition
characterized
on-line
using
scanning
mobility
particle
sizer
aerosol
spectrometer.
Fresh
directed
air–liquid
interface
system.
Aged
naphthalene-
somewhat
more
toxic
than
SOA.
naphthalene
contained
peroxide
levels
higher
those
level
induction
Nrf2
signaling
increased
following
Given
prevalence
its
observed
toxicity,
this
study
calls
for
studies
aimed
at
understanding
underlying
mechanics.
Proceedings of the National Academy of Sciences,
Journal Year:
2018,
Volume and Issue:
115(33), P. 8301 - 8306
Published: Aug. 3, 2018
Dimeric
compounds
contribute
significantly
to
the
formation
and
growth
of
atmospheric
secondary
organic
aerosol
(SOA)
derived
from
monoterpene
oxidation.
However,
mechanisms
dimer
production,
in
particular
relevance
gas-
vs.
particle-phase
chemistry,
remain
unclear.
Here,
through
a
combination
mass
spectrometric,
chromatographic,
synthetic
techniques,
we
identify
suite
dimeric
(C15-19H24-32O5-11)
formed
concerted
O3
OH
oxidation
β-pinene
(i.e.,
accretion
O3-
OH-derived
products/intermediates).
These
dimers
account
for
an
appreciable
fraction
(5.9-25.4%)
SOA
are
designated
as
extremely
low-volatility
compounds.
Certain
dimers,
characterized
covalent
esters,
conclusively
shown
form
heterogeneous
while
evidence
production
via
gas-phase
reactions
is
also
presented.
The
synergistic
+
represents
potentially
significant,
heretofore-unidentified
source
SOA.
This
reactivity
suggests
that
current
treatment
sum
products
originating
isolated
individual
precursors
fails
accurately
reflect
complexity
pathways
at
play
real
atmosphere.
Accounting
role
ambient
could
help
resolve
discrepancy
between
measured
burden
predicted
by
regional
air
quality
global
climate
models.