Abstract.
Secondary
organic
aerosols
(SOA)
can
exist
in
liquid,
semi-solid
or
amorphous
solid
states,
which
are
rarely
accounted
for
current
chemical
transport
models
(CTMs).
Missing
the
information
of
SOA
phase
state
and
viscosity
CTMs
impedes
accurate
representation
formation
evolution,
affecting
predictions
aerosol
effects
on
air
quality
climate.
We
have
previously
developed
a
method
to
estimate
glass
transition
temperature
(Tg)
an
compound
based
volatility.
In
this
study,
we
apply
predict
particles
over
China
summer
2018
using
Weather
Research
Forecasting
model
coupled
Chemistry
(WRF-Chem).
This
is
first
time
that
spatial
distributions
investigated
by
regional
CTM.
Simulations
show
Tg
values
dry
range
from
~287
K
305
K,
with
higher
northwestern
where
larger
mass
fractions
low
volatility
compounds.
Considering
water
uptake
particles,
also
shows
prominent
geospatial
gradient
highly
viscous
mainly
found
China.
The
lowest
highest
both
occur
Qinghai-Tibet
Plateau
predicted
high-altitude
areas
liquid
south
plateau
high
relative
humidity
during
monsoon
season.
characteristic
mixing
timescale
molecules
200
nm
calculated
simulated
particle
bulk
diffusion
coefficient
molecules.
Calculations
period
percent
longer
than
1
h
>
70
%
at
surface
500
hPa
most
northern
China,
indicating
kinetic
partitioning
considering
may
be
required
more
prediction
concentrations
size
these
areas.
Sensitivity
simulations
including
extremely
low-volatile
compounds,
decreases
up
12
southeastern
period.
With
assumption
inorganic
compounds
always
internally
mixed
one
phase,
absorbed
species
significantly
lower
indicates
constraining
uncertainties
accurately
predicting
occurrence
separation
would
improve
multicomponent
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(1)
Published: Jan. 1, 2024
Abstract
Anthropogenic
dust
is
an
important
constituent
of
airborne
particles
in
the
urban
environment
but
its
ice
nucleation
activity
remains
poorly
investigated.
Here,
we
studied
sources
and
nucleating
properties
size‐resolved
atmosphere
under
mixed‐phase
cloud
conditions.
The
heat‐resistant
(INPs)
unexpectedly
contributed
∼70%
supermicron
INPs
at
temperatures
below
−15°C.
A
detailed
chemical
composition
analysis
revealed
that
these
were
associated
with
anthropogenic
dust,
such
as
traffic‐influenced
road
dust.
parameterization
based
on
was
developed
to
predict
INP
concentration,
given
their
correlations
concentration
similarity
compositions.
Once
integrated
into
global
models,
this
holds
potential
assess
contribution
a
scale.
Given
considerable
presence
significant
role
INPs,
suggest
it
may
be
aerosol
source
influencing
microphysics
warrant
further
investigations.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(8), P. 4809 - 4826
Published: April 23, 2024
Abstract.
Secondary
organic
aerosols
(SOAs)
can
exist
in
liquid,
semi-solid,
or
amorphous
solid
states.
Chemical
transport
models
(CTMs),
however,
usually
assume
that
SOA
particles
are
homogeneous
and
well-mixed
liquids,
with
rapid
establishment
of
gas–particle
equilibrium
for
simulations
formation
partitioning.
Missing
the
information
phase
state
viscosity
CTMs
impedes
accurate
representation
evolution,
affecting
predictions
aerosol
effects
on
air
quality
climate.
We
have
previously
developed
a
parameterization
to
estimate
glass
transition
temperature
(Tg)
an
compound
based
volatility
predict
SOA.
In
this
study,
we
apply
method
over
China
summer
2018
using
Weather
Research
Forecasting
model
coupled
Chemistry
(WRF-Chem).
The
simulated
Tg
dry
(Tg,org)
agrees
well
value
estimated
from
ambient
measurements
at
urban
site
Beijing.
For
spatial
distributions
Tg,org,
show
surface
values
Tg,org
range
∼287
305
K,
higher
northwestern
China,
where
larger
mass
fractions
low-volatility
compounds.
Considering
water
uptake
by
particles,
shows
prominent
geospatial
gradient
which
highly
viscous
mainly
predicted
China.
lowest
highest
both
occur
Qinghai–Tibet
Plateau,
is
high-altitude
areas
liquid
south
plateau
high
relative
humidity
during
monsoon
season.
Sensitivity
that,
including
extremely
compounds,
percent
time
particle
decreases
up
12
%
southeastern
period.
With
assumption
inorganic
compounds
internally
mixed
one
phase,
absorbed
species
significantly
lower
This
indicates
constraining
uncertainties
mixing
would
improve
prediction
multicomponent
also
calculate
characteristic
timescale
molecules
200
m
evaluate
kinetic
limitations
Calculations
period
longer
than
1
h
>70
500
hPa
most
northern
indicating
partitioning
considering
bulk
diffusion
may
be
required
more
concentrations
size
these
areas.
Environment International,
Journal Year:
2025,
Volume and Issue:
195, P. 109251 - 109251
Published: Jan. 1, 2025
The
rapid
urbanization
in
China
has
brought
about
serious
air
pollution
problems,
which
are
likely
to
persist
for
a
considerable
period
as
the
process
continues.
In
urban
areas,
spatial
distribution
of
pollutants
represented
by
PM
A
coal
ban
policy
in
northern
China
during
winter
2017
enforced
a
switch
from
to
gas
or
electricity
for
residential
heating,
providing
unique
opportunity
study
the
effect
of
reduced
combustion
emissions
on
organic
aerosol
(OA).
This
explores
OA
composition,
sources,
and
atmospheric
transformations
Beijing
before
using
online
chemical
speciation
monitor
(ACSM)
offline
14C
measurements.
Four
primary
factors
(hydrocarbon-like,
cooking,
biomass
burning,
OA)
one
secondary
factor
(oxygenated
OA,
OOA)
were
resolved
ACSM.
In
response
ban,
concentrations
generally
decreased,
but
decreased
most
strongly,
consistent
with
fossil
carbon
contributions
(67
±
3%
vs
55
4%
ban).
Concurrently,
OOA
fraction
increased
45
72%,
due
larger
decrease
(POA;
59-88%)
compared
(34%),
highlighting
enhanced
formation
period.
aligns
evidence
higher
water-soluble
(which
has
mostly
sources).
During
period,
Ox
doubled
positively
correlated
fraction,
strong
photochemical
production.
The
results
show
that
reduction
POA
stringent
clean
air
actions
is
partially
offset
by
formation.
ACS ES&T Air,
Journal Year:
2024,
Volume and Issue:
1(9), P. 960 - 972
Published: July 10, 2024
This
study
leverages
explainable
machine
learning,
specifically
XGBoost
models
with
Shapley
Additive
Explanations
(SHAP),
to
explore
the
chemical
properties
of
atmospheric
aerosols
in
Seoul,
Korea,
during
summer
2019.
Focusing
on
non-refractory
particulate
matter
(NR-PM1)
measured
by
high-resolution
time-of-flight
aerosol
mass
spectrometry
(HR-ToF-AMS),
research
extends
organic
(OA)
sources
identified
via
positive
matrix
factorization
MS
data.
The
achieved
good
predictive
accuracy
(R2
>
0.90)
for
all
species
concentrations,
except
hydrocarbon-like
OA
(HOA)
due
frequent
concentration
fluctuations.
model
outcomes
aligned
well
those
previously
using
conventional
methods
(chemical
transport
and
correlational
analysis),
confirming
that
relative
humidity
is
associated
nocturnal
nitrate
photochemistry
sulfate
summertime
Seoul.
Importantly,
revealed
mostly
nonlinear
relationships
between
factors,
such
as
temperature
(PM)
components,
thereby
deepening
understanding
formation
processes.
Notably,
different
potential
mechanisms
were
discerned
more
oxidized
oxygenated
(MO-OOA)
primary
(OPOA).
For
MO-OOA,
SHAP
analysis
showed
a
plateau
values
at
an
Ox
0.085
ppm,
which
suggested
fragmentation
from
further
oxidation
agreed
previous
chamber
experiments.
Conversely,
lack
OPOA
implied
ongoing
oxidation,
suggesting
higher
longer
potential.
approach
offers
rapid
insights
into
complex
It
essential
acknowledge
do
not
establish
causality,
knowledge
underlying
physical
processes
was
required
conclude
valid
comprehensive
interpretations
ML
results.
Abstract.
Aerosol
hygroscopic
growth
and
activation
under
high
relative
humidity
(RH)
conditions
significantly
influence
the
physicochemical
properties
of
submicron
aerosols
(PM1).
However,
this
process
remains
poorly
characterized
due
to
limited
measurements.
To
address
gap,
we
deployed
an
advanced
aerosol-fog
sampling
system
that
automatically
switched
between
PM1,
PM2.5,
TSP
inlets
at
a
rural
site
in
North
China
Plain
cold
season.
The
results
revealed
aerosol
swelling
water
vapor
uptake
influenced
RH
by
shifting
cut-off
size
impactors.
Under
subsaturated
(>
90
%),
over
25
%
mass
with
dry
diameters
below
1
μm
resided
supermicron
ranges,
while
supersaturated
foggy
conditions,
more
than
70
migrated
ranges.
Hygroscopic
particularly
affected
highly
hydrophilic
inorganic
salts
significant
sulfate
nitrate
particles
27
–
33
95
≤
99
%,
65.5
conditions.
Moreover,
10
biomass
burning
organic
grew
beyond
2.5
during
fog
events,
fossil
fuel-related
OA
(FFOA)
remained
dominantly
suggesting
inefficient
aqueous
conversion
FFOA.
two
SOA
factors
(OOA1
OOA2)
behaved
differently
OOA2
exhibiting
higher
activated
fraction
despite
lower
oxygen-to-carbon
ratio.
A
substantial
increase
organosulfur
concentrations
droplets
events
suggested
conversions
formations
brown
carbon
potential
radiative
impacts.
Overall,
our
study
highlights
remarkably
different
processing
primary
secondary
PM1
components
distinct
ambient
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(16), P. 9387 - 9399
Published: Aug. 28, 2024
Abstract.
Aerosol
hygroscopic
growth
and
activation
under
high-relative-humidity
(RH)
conditions
significantly
influence
the
physicochemical
properties
of
submicron
aerosols
(PM1).
However,
this
process
remains
poorly
characterized
due
to
limited
measurements.
To
address
gap,
we
deployed
an
advanced
aerosol–fog
sampling
system
that
automatically
switched
between
PM1,
PM2.5
total
suspended
particulate
(TSP)
inlets
at
a
rural
site
in
North
China
Plain
cold
season.
The
results
revealed
aerosol
swelling
water
vapor
uptake
influenced
high-RH
by
shifting
cut-off
size
impactors.
At
subsaturated
high
RH
(>
90
%),
over
25
%
mass
with
dry
diameters
below
1
µm
resided
supermicron
ranges,
while
supersaturated
foggy
conditions,
more
than
70
migrated
ranges.
Hygroscopic
particularly
affected
highly
hydrophilic
inorganic
salts,
significant
number
sulfate
nitrate
particles
27
%–33
95
≤
99
78
conditions.
Moreover,
10
biomass
burning
organic
grew
beyond
2.5
during
fog
events,
fossil-fuel-related
(FFOA)
remained
dominantly
suggesting
inefficient
aqueous
conversion
FFOA.
two
secondary
(SOA)
factors
(OOA1
OOA2)
behaved
differently
OOA2
exhibiting
higher
activated
fraction
despite
lower
oxygen
/
carbon
ratio.
A
substantial
increase
organosulfur
concentrations
droplets
events
suggested
conversions
formations
brown
potential
radiative
impacts.
Overall,
our
study
highlights
remarkably
different
cloud
processing
behaviors
primary
aerosols,
which
would
benefit
better
understanding
aerosol–cloud
interactions
distinct
atmospheric
Abstract.
Secondary
organic
aerosols
(SOA)
can
exist
in
liquid,
semi-solid
or
amorphous
solid
states,
which
are
rarely
accounted
for
current
chemical
transport
models
(CTMs).
Missing
the
information
of
SOA
phase
state
and
viscosity
CTMs
impedes
accurate
representation
formation
evolution,
affecting
predictions
aerosol
effects
on
air
quality
climate.
We
have
previously
developed
a
method
to
estimate
glass
transition
temperature
(Tg)
an
compound
based
volatility.
In
this
study,
we
apply
predict
particles
over
China
summer
2018
using
Weather
Research
Forecasting
model
coupled
Chemistry
(WRF-Chem).
This
is
first
time
that
spatial
distributions
investigated
by
regional
CTM.
Simulations
show
Tg
values
dry
range
from
~287
K
305
K,
with
higher
northwestern
where
larger
mass
fractions
low
volatility
compounds.
Considering
water
uptake
particles,
also
shows
prominent
geospatial
gradient
highly
viscous
mainly
found
China.
The
lowest
highest
both
occur
Qinghai-Tibet
Plateau
predicted
high-altitude
areas
liquid
south
plateau
high
relative
humidity
during
monsoon
season.
characteristic
mixing
timescale
molecules
200
nm
calculated
simulated
particle
bulk
diffusion
coefficient
molecules.
Calculations
period
percent
longer
than
1
h
>
70
%
at
surface
500
hPa
most
northern
China,
indicating
kinetic
partitioning
considering
may
be
required
more
prediction
concentrations
size
these
areas.
Sensitivity
simulations
including
extremely
low-volatile
compounds,
decreases
up
12
southeastern
period.
With
assumption
inorganic
compounds
always
internally
mixed
one
phase,
absorbed
species
significantly
lower
indicates
constraining
uncertainties
accurately
predicting
occurrence
separation
would
improve
multicomponent
Abstract.
Secondary
organic
aerosols
(SOA)
can
exist
in
liquid,
semi-solid
or
amorphous
solid
states,
which
are
rarely
accounted
for
current
chemical
transport
models
(CTMs).
Missing
the
information
of
SOA
phase
state
and
viscosity
CTMs
impedes
accurate
representation
formation
evolution,
affecting
predictions
aerosol
effects
on
air
quality
climate.
We
have
previously
developed
a
method
to
estimate
glass
transition
temperature
(Tg)
an
compound
based
volatility.
In
this
study,
we
apply
predict
particles
over
China
summer
2018
using
Weather
Research
Forecasting
model
coupled
Chemistry
(WRF-Chem).
This
is
first
time
that
spatial
distributions
investigated
by
regional
CTM.
Simulations
show
Tg
values
dry
range
from
~287
K
305
K,
with
higher
northwestern
where
larger
mass
fractions
low
volatility
compounds.
Considering
water
uptake
particles,
also
shows
prominent
geospatial
gradient
highly
viscous
mainly
found
China.
The
lowest
highest
both
occur
Qinghai-Tibet
Plateau
predicted
high-altitude
areas
liquid
south
plateau
high
relative
humidity
during
monsoon
season.
characteristic
mixing
timescale
molecules
200
nm
calculated
simulated
particle
bulk
diffusion
coefficient
molecules.
Calculations
period
percent
longer
than
1
h
>
70
%
at
surface
500
hPa
most
northern
China,
indicating
kinetic
partitioning
considering
may
be
required
more
prediction
concentrations
size
these
areas.
Sensitivity
simulations
including
extremely
low-volatile
compounds,
decreases
up
12
southeastern
period.
With
assumption
inorganic
compounds
always
internally
mixed
one
phase,
absorbed
species
significantly
lower
indicates
constraining
uncertainties
accurately
predicting
occurrence
separation
would
improve
multicomponent