Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(18), P. 12629 - 12646
Published: Sept. 28, 2022
Abstract.
Nitrate
(NO3−)
has
been
the
dominant
and
least
reduced
chemical
component
of
fine
particulate
matter
(PM2.5)
since
stringent
emission
controls
implemented
in
China
2013.
The
formation
pathways
NO3−
vary
seasonally
differ
substantially
daytime
vs.
nighttime.
They
are
affected
by
precursor
emissions,
atmospheric
oxidation
capacity,
meteorological
conditions.
Understanding
provides
insights
for
design
effective
control
strategies
to
mitigate
pollution.
In
this
study,
Community
Multiscale
Air
Quality
(CMAQ)
model
was
applied
investigate
impact
regional
transport,
predominant
physical
processes,
different
total
nitrate
(TNO3,
i.e.,
HNO3+
NO3−)
production
Yangtze
River
Delta
(YRD)
region
during
four
seasons
2017.
NO3-/PM2.5
NO3-/TNO3
highest
winter,
reaching
21
%
94
%,
respectively.
adjusted
gas
ratio
(adjGR
=
([NH3]+
[NO3−])/([HNO3]+
[NO3−]))
YRD
is
generally
greater
than
2
across
most
areas
YRD,
indicating
that
mostly
NH3-rich
regime
limited
HNO3
formation.
Local
emissions
transportation
contribute
concentrations
throughout
50
%–62
38
%–50
majority
transport
contributed
indirect
(i.e.,
formed
transported
precursors
reacting
with
local
precursors).
Aerosol
(AERO,
including
condensation,
coagulation,
new
particle
formation,
aerosol
growth)
processes
source
summer,
dominated
AERO
(TRAN,
sum
horizontal
vertical
transport)
processes.
OH
+
NO2
pathway
contributes
60
%–83
TNO3
production,
N2O5
heterogeneous
(HET
N2O5)
10
%–36
region.
HET
contribution
becomes
more
important
cold
warm
seasons.
Within
planetary
boundary
layer
Shanghai,
day
(98
%)
summer
spring
night
(61
winter.
contributions
dominate
day,
while
dominates
at
night.
Journal of Geophysical Research Atmospheres,
Journal Year:
2025,
Volume and Issue:
130(4)
Published: Feb. 14, 2025
Abstract
Recent
years
have
witnessed
a
surge
in
nitrate‐driven
aerosol
pollution
across
China
with
N
2
O
5
hydrolysis
emerging
as
critical
formation
pathway.
Common
surface
measurements
may
misleadingly
imply
this
process
due
to
low
nighttime
ozone
at
level
winter.
However,
our
study
reveals
more
complex
picture
by
unveiling
the
vertical
dynamics
of
nitrate
through
an
integration
tethered
airship
campaign,
long‐term
ground
measurements,
and
model
simulations.
Interestingly,
we
observed
rapid
growth
approximately
400
m
altitude,
where
box
revealed
optimal
conditions
for
sustained
nocturnal
production.
The
accumulated
overnight
residual
layer
(RL)
is
transported
downward
next
morning
boundary
breaks
down,
substantially
increasing
surface‐level
thus
exacerbating
pollution.
Annual‐averaged
diurnal
patterns
measured
station
clearly
confirm
increase.
mixing
from
RL
contributes
up
80%
total
10:00
LT
its
influence
persisting
31%
even
after
sunset.
Air
mass
trajectory
analysis
further
confirms
that
emissions
city‐cluster
significantly
contribute
downwind
transporting
pollutants
into
RL.
This
research
underscores
important
role
chemical
processes,
facilitated
elevated
ozone,
shaping
It
highlights
indispensability
profiling
understanding
advocates
regionally
coordinated
control
strategies
eastern
China.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(14), P. 9287 - 9308
Published: July 19, 2019
Abstract.
Mountain
basins
in
Northern
Utah,
including
the
Salt
Lake
Valley
(SLV),
suffer
from
wintertime
air
pollution
events
associated
with
stagnant
atmospheric
conditions.
During
these
events,
fine
particulate
matter
concentrations
(PM2.5)
can
exceed
national
ambient
quality
standards.
Previous
studies
SLV
have
found
that
PM2.5
is
primarily
composed
of
ammonium
nitrate
(NH4NO3),
formed
condensation
gas-phase
ammonia
(NH3)
and
nitric
acid
(HNO3).
Additional
several
western
basins,
SLV,
suggested
production
HNO3
nocturnal
heterogeneous
N2O5
uptake
dominant
source
NH4NO3
during
winter.
The
rate
this
process,
however,
remains
poorly
quantified,
part
due
to
limited
vertical
measurements
above
surface,
where
chemistry
most
active.
2017
Utah
Winter
Fine
Particulate
Study
(UWFPS)
provided
first
aircraft
detailed
chemical
composition
SLV.
Coupled
ground-based
observations,
analyses
day-
nighttime
research
flights
confirm
principally
NH4NO3,
by
HNO3.
Here,
observations
box
model
assess
contribution
aerosol
using
NO3-
rate,
coefficient
(γ(N2O5)),
yield
ClNO2
(φ(ClNO2)),
which
had
medians
1.6
µg
m−3
h−1,
0.076,
0.220,
respectively.
While
fit
values
γ(N2O5)
may
be
biased
high
a
potential
under-measurement
surface
area,
other
quantities
are
unaffected.
Lastly,
additional
simulations
suggest
produces
between
2.4
3.9
per
day
when
considering
possible
effects
dilution.
This
sufficient
account
for
52
%–85
%
daily
observed
surface-level
buildup
nitrate,
though
accurate
quantification
dependent
on
modeled
dilution,
mixing
processes,
photochemistry.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(24), P. 17569 - 17580
Published: Dec. 6, 2022
Tropospheric
ozone
(O3)
is
a
harmful
gas
compound
to
humans
and
vegetation,
it
also
serves
as
climate
change
forcer.
O3
formed
in
the
reactions
of
nitrogen
oxides
volatile
organic
compounds
(VOCs)
with
light.
In
this
study,
an
pollution
episode
encountered
Shenzhen,
South
China
2018
was
investigated
illustrate
influence
aerosols
on
local
production.
We
used
box
model
comprehensive
heterogeneous
mechanisms
empirical
prediction
photolysis
rates
reproduce
episode.
Results
demonstrate
that
aerosol
light
extinction
NO2
showed
comparable
but
opposite
signs
Hence,
from
different
processes
largely
counteracted.
Sensitivity
tests
suggest
production
increases
further
reduction
while
continued
NOx
finally
shifts
NOx-limited
regime
respect
traditional
O3-NOx-VOC
sensitivity.
Our
results
shed
role
highlight
mitigation
not
only
limiting
helping
ease
particulate
nitrate,
path
for
cocontrol
fine
particle
pollution.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(18), P. 12629 - 12646
Published: Sept. 28, 2022
Abstract.
Nitrate
(NO3−)
has
been
the
dominant
and
least
reduced
chemical
component
of
fine
particulate
matter
(PM2.5)
since
stringent
emission
controls
implemented
in
China
2013.
The
formation
pathways
NO3−
vary
seasonally
differ
substantially
daytime
vs.
nighttime.
They
are
affected
by
precursor
emissions,
atmospheric
oxidation
capacity,
meteorological
conditions.
Understanding
provides
insights
for
design
effective
control
strategies
to
mitigate
pollution.
In
this
study,
Community
Multiscale
Air
Quality
(CMAQ)
model
was
applied
investigate
impact
regional
transport,
predominant
physical
processes,
different
total
nitrate
(TNO3,
i.e.,
HNO3+
NO3−)
production
Yangtze
River
Delta
(YRD)
region
during
four
seasons
2017.
NO3-/PM2.5
NO3-/TNO3
highest
winter,
reaching
21
%
94
%,
respectively.
adjusted
gas
ratio
(adjGR
=
([NH3]+
[NO3−])/([HNO3]+
[NO3−]))
YRD
is
generally
greater
than
2
across
most
areas
YRD,
indicating
that
mostly
NH3-rich
regime
limited
HNO3
formation.
Local
emissions
transportation
contribute
concentrations
throughout
50
%–62
38
%–50
majority
transport
contributed
indirect
(i.e.,
formed
transported
precursors
reacting
with
local
precursors).
Aerosol
(AERO,
including
condensation,
coagulation,
new
particle
formation,
aerosol
growth)
processes
source
summer,
dominated
AERO
(TRAN,
sum
horizontal
vertical
transport)
processes.
OH
+
NO2
pathway
contributes
60
%–83
TNO3
production,
N2O5
heterogeneous
(HET
N2O5)
10
%–36
region.
HET
contribution
becomes
more
important
cold
warm
seasons.
Within
planetary
boundary
layer
Shanghai,
day
(98
%)
summer
spring
night
(61
winter.
contributions
dominate
day,
while
dominates
at
night.