Abstract.
The
particle-phase
state
is
crucial
for
reactive
gas
uptake,
heterogeneous,
and
multiphase
chemical
reactions,
thereby
impacting
secondary
aerosol
formation.
This
study
provides
valuable
insights
into
the
significance
of
transition
liquid
water
(ALW)
in
winter
particulate
growth.
Our
findings
reveal
that
particles
predominantly
exist
as
semi-solid
or
solid
during
clean
days
with
ambient
relative
humidity
(RH)
below
30
%.
However,
non-liquid
to
phase
occurs
when
ALW
mass
fraction
exceeds
15
%
(dry
mass)
at
RH
thresholds
40–60
During
haze
episodes,
transformation
rates
sulfate
nitrate
aerosols
rapidly
increase
through
increased
by
48
11
%,
respectively,
resulting
noticeable
increases
inorganic
(SIA).
presence
abundant
ALW,
favored
elevated
higher
proportion
SIA,
facilitates
heterogeneous
aqueous
processes
particles,
leading
a
substantial
formation
organic
oxidation.
Consequently,
overall
hygroscopicity
parameters
exhibit
enhancement
mean
value
23
These
results
highlight
key
factor
initiating
positive
feedback
loops
between
episodes
over
North
China
Plain.
Accurate
predictions
necessitate
explicit
consideration
transport
models.
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.
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
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
Nature Geoscience,
Journal Year:
2024,
Volume and Issue:
17(8), P. 747 - 754
Published: Aug. 1, 2024
Haze
in
Beijing
is
linked
to
atmospherically
formed
secondary
organic
aerosol,
which
has
been
shown
be
particularly
harmful
human
health.
However,
the
sources
and
formation
pathways
of
these
aerosols
remain
largely
unknown,
hindering
effective
pollution
mitigation.
Here
we
have
quantified
aerosol
via
direct
near-molecular
observations
central
Beijing.
In
winter,
arises
mainly
from
fresh
solid-fuel
emissions
originating
both
combustion
aqueous
processes,
probably
involving
multiphase
chemistry
with
aromatic
compounds.
The
most
severe
haze
combustion,
transported
Beijing-Tianjing-Hebei
Plain
rural
mountainous
areas
west
summer,
increased
fraction
dominated
by
Xi'an-Shanghai-Beijing
region,
while
contribution
biogenic
remains
relatively
small.
Overall,
identify
main
affecting
Beijing,
clearly
extend
beyond
local
Our
results
suggest
that
targeting
key
precursor
emission
sectors
regionally
may
needed
effectively
mitigate
pollution.
Abstract.
The
particle-phase
state
is
crucial
for
reactive
gas
uptake,
heterogeneous,
and
multiphase
chemical
reactions,
thereby
impacting
secondary
aerosol
formation.
This
study
provides
valuable
insights
into
the
significance
of
transition
liquid
water
(ALW)
in
winter
particulate
growth.
Our
findings
reveal
that
particles
predominantly
exist
as
semi-solid
or
solid
during
clean
days
with
ambient
relative
humidity
(RH)
below
30
%.
However,
non-liquid
to
phase
occurs
when
ALW
mass
fraction
exceeds
15
%
(dry
mass)
at
RH
thresholds
40–60
During
haze
episodes,
transformation
rates
sulfate
nitrate
aerosols
rapidly
increase
through
increased
by
48
11
%,
respectively,
resulting
noticeable
increases
inorganic
(SIA).
presence
abundant
ALW,
favored
elevated
higher
proportion
SIA,
facilitates
heterogeneous
aqueous
processes
particles,
leading
a
substantial
formation
organic
oxidation.
Consequently,
overall
hygroscopicity
parameters
exhibit
enhancement
mean
value
23
These
results
highlight
key
factor
initiating
positive
feedback
loops
between
episodes
over
North
China
Plain.
Accurate
predictions
necessitate
explicit
consideration
transport
models.
Abstract.
The
particle-phase
state
is
crucial
for
reactive
gas
uptake,
heterogeneous,
and
multiphase
chemical
reactions,
thereby
impacting
secondary
aerosol
formation.
This
study
provides
valuable
insights
into
the
significance
of
transition
liquid
water
(ALW)
in
winter
particulate
growth.
Our
findings
reveal
that
particles
predominantly
exist
as
semi-solid
or
solid
during
clean
days
with
ambient
relative
humidity
(RH)
below
30
%.
However,
non-liquid
to
phase
occurs
when
ALW
mass
fraction
exceeds
15
%
(dry
mass)
at
RH
thresholds
40–60
During
haze
episodes,
transformation
rates
sulfate
nitrate
aerosols
rapidly
increase
through
increased
by
48
11
%,
respectively,
resulting
noticeable
increases
inorganic
(SIA).
presence
abundant
ALW,
favored
elevated
higher
proportion
SIA,
facilitates
heterogeneous
aqueous
processes
particles,
leading
a
substantial
formation
organic
oxidation.
Consequently,
overall
hygroscopicity
parameters
exhibit
enhancement
mean
value
23
These
results
highlight
key
factor
initiating
positive
feedback
loops
between
episodes
over
North
China
Plain.
Accurate
predictions
necessitate
explicit
consideration
transport
models.
Abstract.
The
particle-phase
state
is
crucial
for
reactive
gas
uptake,
heterogeneous,
and
multiphase
chemical
reactions,
thereby
impacting
secondary
aerosol
formation.
This
study
provides
valuable
insights
into
the
significance
of
transition
liquid
water
(ALW)
in
winter
particulate
growth.
Our
findings
reveal
that
particles
predominantly
exist
as
semi-solid
or
solid
during
clean
days
with
ambient
relative
humidity
(RH)
below
30
%.
However,
non-liquid
to
phase
occurs
when
ALW
mass
fraction
exceeds
15
%
(dry
mass)
at
RH
thresholds
40–60
During
haze
episodes,
transformation
rates
sulfate
nitrate
aerosols
rapidly
increase
through
increased
by
48
11
%,
respectively,
resulting
noticeable
increases
inorganic
(SIA).
presence
abundant
ALW,
favored
elevated
higher
proportion
SIA,
facilitates
heterogeneous
aqueous
processes
particles,
leading
a
substantial
formation
organic
oxidation.
Consequently,
overall
hygroscopicity
parameters
exhibit
enhancement
mean
value
23
These
results
highlight
key
factor
initiating
positive
feedback
loops
between
episodes
over
North
China
Plain.
Accurate
predictions
necessitate
explicit
consideration
transport
models.