Abstract.
Biogenic
volatile
organic
compounds
(BVOCs)
are
the
largest
source
of
secondary
aerosols
(SOA)
globally.
However,
complex
interactions
between
marine
and
terrestrial
BVOCs
remain
unclear,
inhibiting
our
in-depth
understanding
SOA
formation
in
coastal
areas
its
environmental
impacts.
Here,
we
performed
smog
chamber
experiments
with
mixed
α-pinene
(a
typical
monoterpene)
dimethyl
sulfide
(DMS,
a
emission
BVOC)
to
investigate
their
possible
subsequent
formation.
It
is
found
that
DMS
has
non-linear
effect
on
generation:
mass
concentration
yield
show
an
increasing
then
decreasing
trend
increase
initial
DMS.
The
can
be
attributed
OH
regeneration
together
acid-catalyzed
heterogeneous
reactions
by
oxidation
DMS,
while
explained
high
reactivity
inhibits
low
volatility
products.
results
from
infrared
spectra
reveal
contribution
sulfur-containing
molecules
system.
Moreover,
indicate
acidic
products
generated
photooxidation
enhance
O:C
ratio,
organosulfates
produced
contribute
SOA.
In
addition,
trends
relative
abundance
highly
oxygenated
(HOMs)
C8-C10
multiple
functional
groups
different
systems
agree
well
turning
point
yield.
findings
this
study
have
significant
implications
for
binary
or
more
atmosphere
areas.
The Journal of Physical Chemistry A,
Journal Year:
2022,
Volume and Issue:
126(40), P. 7309 - 7330
Published: Sept. 28, 2022
Dark
chamber
experiments
were
conducted
to
study
the
SOA
formed
from
oxidation
of
α-pinene
and
Δ-carene
under
different
peroxy
radical
(RO2)
fate
regimes:
RO2
+
NO3,
RO2,
HO2.
mass
yields
<1
∼25%
strongly
dependent
on
available
OA
up
∼100
μg
m-3.
The
strong
yield
dependence
is
driven
by
absorptive
partitioning
not
surface
area
for
condensation.
Yields
NO3
consistently
higher,
ranging
∼10-50%
with
some
<25
Explicit
kinetic
modeling
including
vapor
wall
losses
was
enable
comparisons
across
VOC
precursors
regimes
determine
atmospherically
relevant
yields.
Furthermore,
similar
each
monoterpene
nominal
or
HO2
regimes;
thus,
volatility
basis
sets
(VBS)
constructed
independent
chemical
regime.
Elemental
O/C
ratios
∼0.4-0.6
nitrate/organic
∼0.15
observed
in
particle
phase
both
monoterpenes
all
regimes,
using
aerosol
spectrometer
(AMS)
measurements.
An
empirical
relationship
estimating
density
AMS-derived
elemental
ratios,
previously
reported
literature
non-nitrate
containing
OA,
successfully
adapted
organic
nitrate-rich
SOA.
Observations
an
NO3-
ionization
(NO3-CIMS)
suggest
that
more
readily
forms
low-volatility
gas-phase
highly
oxygenated
molecules
(HOMs)
than
α-pinene,
which
primarily
volatile
semivolatile
species,
when
reacted
regardless
high
presence
HOMs,
unimolecular
multistep
processes
such
as
alkoxy
isomerization
decomposition
may
play
a
role
formation
NO3.
scarcity
peroxide
functional
groups
(on
average,
14%
C10
carried
group
one
test
experiment
regime)
appears
rule
out
major
autoxidation
(ROOH,
ROOR)
formation.
substantially
lower
pathways
are
less
this
precursor.
marked
robust
regime-independent
difference
two
precursor
suggests
order
accurately
model
production
forested
regions
mechanism
must
feature
distinction
among
monoterpenes.
ACS Earth and Space Chemistry,
Journal Year:
2024,
Volume and Issue:
8(2), P. 381 - 392
Published: Feb. 5, 2024
Throughout
the
U.S.,
summertime
fine
particulate
matter
(PM2.5)
exhibits
a
strong
temperature
(T)
dependence.
Reducing
PM2.5
enhancement
with
T
could
reduce
public
health
burden
of
now
and
in
warmer
future.
Atmospheric
models
are
critical
tool
for
probing
processes
components
driving
observed
behaviors.
In
this
work,
we
describe
how
modeled
aerosol
abundance
composition
vary
present-day
Eastern
specific
attention
to
two
major
components:
sulfate
(SO42–)
organic
carbon
(OC).
Observations
U.S.
show
an
average
measured
PM2.5-T
sensitivity
0.67
μg/m3/K,
CMAQv5.4
regional
model
predictions
closely
matching
value.
Observed
SO42–
OC
also
increase
T;
however,
has
component-specific
discrepancies
observations.
Specifically,
underestimates
concentrations
their
while
overestimating
T.
Here,
explore
series
interventions
aimed
at
correcting
these
deviations.
We
conclude
that
relationship
is
driven
by
inorganic
systems
highly
coupled,
it
possible
design
simultaneously
address
biases
component
as
well
responses
Science Advances,
Journal Year:
2022,
Volume and Issue:
8(42)
Published: Oct. 21, 2022
Secondary
organic
aerosol
(SOA),
formed
by
oxidation
of
volatile
compounds,
substantially
influence
air
quality
and
climate.
Highly
oxygenated
molecules
(HOMs),
particularly
those
from
biogenic
monoterpenes,
contribute
a
large
fraction
SOA.
During
daytime,
hydroxyl
radicals
initiate
monoterpene
oxidation,
mainly
addition
to
double
bonds.
Naturally,
related
HOM
formation
mechanisms
should
be
induced
that
reaction
route,
too.
However,
for
α-pinene,
the
most
abundant
atmospheric
monoterpene,
we
find
previously
unidentified
competitive
pathway
under
atmospherically
relevant
conditions:
is
predominately
via
hydrogen
abstraction
radicals,
generally
minor
pathway.
We
show
observations
theoretical
calculations
followed
rearrangement
alkoxy
prerequisite
fast
daytime
formation.
Our
analysis
provides
an
accurate
mechanism
yield,
demonstrating
pathways
can
become
major,
here
SOA
growth
impacts
on
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(17), P. 11323 - 11346
Published: Sept. 2, 2022
Abstract.
Nighttime
NO3-initiated
oxidation
of
biogenic
volatile
organic
compounds
(BVOCs)
such
as
monoterpenes
is
important
for
the
atmospheric
formation
and
growth
secondary
aerosol
(SOA),
which
has
significant
impact
on
climate,
air
quality,
human
health.
In
SOA
growth,
highly
oxygenated
molecules
(HOM)
may
be
crucial,
but
their
pathways
role
in
have
yet
to
clarified.
Among
monoterpenes,
limonene
particular
interest
its
high
emission
globally
yield.
this
work,
HOM
reaction
with
nitrate
radical
(NO3)
was
investigated
SAPHIR
chamber
(Simulation
Atmospheric
PHotochemistry
a
large
Reaction
chamber).
About
280
products
were
identified,
grouped
into
19
monomer
families,
11
dimer
3
trimer
families.
Both
closed-shell
open-shell
peroxy
radicals
(RO2⚫)
observed,
many
them
not
been
reported
previously.
Monomers
dimers
accounted
47
%
concentrations,
respectively,
trimers
making
up
remaining
6
%.
most
abundant
C10H15−17NO6−14,
carbonyl
outnumbered
hydroxyl
products,
indicating
importance
RO2⚫
termination
by
unimolecular
dissociation.
autoxidation
alkoxy–peroxy
found
processes
leading
HOM.
Time-dependent
concentration
profiles
containing
nitrogen
showed
mainly
second-generation
patterns.
Dimers
likely
formed
via
accretion
two
RO2⚫,
HOM-trimers
between
RO2⚫.
Trimers
are
suggested
play
an
new
particle
(NPF)
observed
our
experiment.
A
yield
1.5%-0.7%+1.7%
estimated
considering
only
first-generation
products.
mass
could
reasonably
explained
condensation
particles
assuming
irreversible
uptake
ultra-low
volatility
(ULVOCs),
extremely
low
(ELVOCs),
(LVOCs).
This
work
provides
evidence
+NO3
NPF
particles.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(15), P. 8855 - 8877
Published: Aug. 9, 2023
Abstract.
To
investigate
the
sources
and
formation
mechanism
of
oxidized
organic
nitrogen
(OON),
field
measurements
OON
were
conducted
using
an
iodide-adduct
chemical
ionization
mass
spectrometer
equipped
with
a
Filter
Inlet
for
Gases
AEROsols
(FIGAERO-CIMS)
during
fall
2018
in
megacity
Guangzhou,
China.
Using
levoglucosan
as
tracer
biomass
burning
emissions,
results
show
that
(49±23
%)
secondary
(51±23
accounted
comparable
fractions
to
total
particle-phase
(pOON)
but
24±25
%
76±25
gas-phase
(gOON),
respectively,
signifying
important
contribution
pOON
gOON
this
urban
area.
Calculations
production
rates
indicated
hydroxyl
radical
(42
nitrate
(NO3)
(49
oxidation
pathways
potentially
dominated
gOON.
A
high
concentration
NO3
radicals
afternoon
was
observed,
demonstrating
daytime
might
be
more
than
previous
recognition.
Monoterpenes,
found
major
precursors
gOON,
mainly
from
anthropogenic
emissions
The
ratio
Ox
([Ox]
=
[O3]
+
[NO2])
increased
function
relative
humidity
aerosol
surface
area,
indicating
heterogeneous
reaction
pathway
pOON.
Finally,
highly
6
11
oxygen
atoms
highlighting
complex
processes
ambient
air.
Overall,
our
improve
understanding
dynamic
variation
atmosphere.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(13), P. 7297 - 7319
Published: July 4, 2023
Abstract.
Highly
oxygenated
organic
molecules
(HOMs)
play
a
pivotal
role
in
the
formation
of
secondary
aerosol
(SOA).
Therefore,
distribution
and
yields
HOMs
are
fundamental
to
understand
their
fate
chemical
evolution
atmosphere,
it
is
conducive
ultimately
assess
impact
SOA
on
air
quality
climate
change.
In
this
study,
gas-phase
formed
from
reaction
limonene
with
OH
radicals
photooxidation
were
investigated
SAPHIR
(Simulation
Atmospheric
PHotochemistry
large
Reaction
chamber),
using
time-of-flight
ionization
mass
spectrometer
nitrate
reagent
ion
(NO3--CIMS).
A
number
HOMs,
including
monomers
(C9–10)
dimers
(C17–20),
detected
classified
into
various
families.
Both
closed-shell
products
open-shell
peroxy
(RO2)
identified
under
low
NO
(0.06–0.1
ppb)
high
conditions
(17
ppb).
C10
most
abundant
HOM
account
for
over
80
%
total
HOMs.
Closed-shell
two
radical
family,
C10H15Ox⚫
(x=6–15)
C10H17Ox⚫
(x=6–15),
respective
termination
reactions
NO,
RO2,
HO2.
While
likely
by
addition
C10H16,
dominant
initial
step
plus
OH,
C10H15Ox⚫,
via
H
abstraction
OH.
related
contributed
41
42
at
demonstrating
that
H-abstraction
pathways
significant
Combining
theoretical
kinetic
calculations,
structure–activity
relationships
(SARs),
data
literature,
observed
RO2
intensities,
we
proposed
tentative
mechanisms
both
pathways.
We
further
estimated
molar
be
1.97-1.06+2.52
0.29-0.16+0.38
respectively.
Our
study
highlights
importance
provides
yield
oxidation
simulate
formation.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(14), P. 8305 - 8324
Published: July 25, 2023
Abstract.
Atmospheric
humic-like
substances
(HULIS)
affect
the
global
radiation
balance
due
to
their
strong
light
absorption
at
ultraviolet
wavelength.
The
potential
sources
and
molecular
compositions
of
water-soluble
HULIS
a
suburban
site
in
Yangtze
River
Delta
from
2017
2018
were
discussed,
based
on
results
radiocarbon
(14C)
analysis
combining
Fourier
transform
ion
cyclotron
resonance
mass
spectrometry
(FT-ICR-MS)
technique
this
study.
14C
showed
that
averaged
non-fossil-fuel
source
contributions
39
±
8
%
36
6
summer
winter,
respectively,
indicating
significant
fossil
fuel
HULIS.
Van
Krevelen
diagrams
obtained
FT-ICR-MS
proportions
tannin-like
carbohydrate-like
groups
higher
summer,
suggesting
contribution
biogenic
secondary
organic
aerosols
(SOAs).
condensed
aromatic
structures
winter
suggested
increasing
anthropogenic
emissions.
Molecular
composition
CHO,
CHON,
CHOS,
CHONS
subgroups
relatively
intensities
high
O-containing
macromolecular
oligomers
CHO
compounds
further
stronger
SOA
formation
summer.
High-intensity
phenolic
flavonoids,
which
related
biomass
burning
polycyclic
hydrocarbon
(PAH)
derivatives
combustion
emissions,
found
compounds.
Besides,
two
high-intensity
containing
ring
(C9H6O7
C10H5O8)
identified
samples
similar
those
off-road
engine
samples,
traffic
emissions
one
important
study
site.
CHON
mainly
composed
nitro
or
organonitrates
with
significantly
associated
addition
enhanced
NOx
winter.
However,
formulas
referring
N-heterocyclic
compounds,
produced
atmospheric
processes
involving
reduced
N
species
(e.g.,
ammonium).
S-containing
organosulfates
(OSs)
derived
precursors,
namely
long-chain
alkane
hydrocarbon,
illustrate
mixed
Generally,
different
policies
need
be
considered
for
each
season
seasonal
(i.e.,
sources,
both
seasons,
additional
coal
winter).
Measures
control
motor
vehicles
industrial
Additional
measures
power
plants
should
applied
These
findings
add
our
understanding
interaction
between
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(14), P. 8383 - 8402
Published: July 26, 2023
Abstract.
Secondary
organic
aerosols
(SOAs)
play
a
key
role
in
climate
change
and
public
health.
However,
the
oxidation
state
volatility
of
SOAs
are
still
not
well
understood.
Here,
we
investigated
highly
oxygenated
molecules
(HOMs)
formed
from
ozonolysis
β-pinene
limonene.
Fourier
transform
ion
cyclotron
resonance
mass
spectrometry
(FT-ICR
MS)
was
used
to
characterize
HOMs
aerosol
filter
samples,
scanning
mobility
particle
sizer
(SMPS)
measure
concentration
size
distribution
SOA
particles.
The
relative
abundance
(i.e.,
ratio
summed
peak
intensity
totally
identified
compounds)
limonene
14
%–20
%,
higher
than
(3
%–13
%),
exhibiting
different
trends
with
increasing
ozone
concentrations.
oxidation-derived
exhibit
yield
at
high
concentration,
accompanied
by
substantial
formation
ultra-low-volatile
compounds
(ULVOCs).
Limonene
moderate
concentrations,
semi-,
low-,
extremely
low-volatile
(SVOCs,
LOVCs,
ELVOCs)
major
role.
Combined
experimental
evidence
theoretical
analysis
indicate
that
oxygen-increasing-based
peroxy
radical
chemistry
is
plausible
mechanism
for
10
carbon
atoms.
Our
findings
show
species
largely
different.
concentration-driven
evolution
monoterpenes
suggested
be
considered
future
or
exposure
risk
models,
which
may
enable
more
accurate
air
quality
prediction
management.