Abstract.
The
hydroxyl
radical
(OH)
is
the
main
oxidant
responsible
for
removal
of
many
reduced
trace
gases
and
formation
secondary
air
pollutants.
However,
due
to
technical
difficulties
in
measuring
OH,
existing
measurements
atmospheric
OH
concentrations
are
limited,
its
sources
sinks
not
well
understood
under
low
NOx
conditions.
In
this
study,
we
observed
using
chemical
ionization
mass
spectrometry
at
a
coastal
site
Hong
Kong
from
October
November
2020.
average
noontime
concentration
over
study
period
was
measured
4.9
±
2.1
×
106
cm-3.
We
found
that
box
model
with
comprehensive
observational
constraints
reproduced
daytime
when
parcels
originated
continental
regions.
overpredicted
by
73
%
on
average.
Missing
reactivity
proposed
be
cause
overprediction.
High
missing
case
nitrogen
oxides
(NOx)
volatile
organic
compounds,
as
aged
air,
suggesting
there
could
unmeasured
species
overestimate
parcels.
Further
studies
needed
identify
these
their
contributions
budget,
order
better
quantify
Chlorine
radicals
(Cl·)
are
highly
reactive
and
affect
the
fate
of
air
pollutants.
Several
field
studies
in
China
have
revealed
elevated
levels
daytime
molecular
chlorine
(Cl2),
which,
upon
photolysis,
release
substantial
amounts
Cl·
but
poorly
represented
current
chemical
transport
models.
Here,
we
implemented
a
parametrization
for
formation
Cl2
through
photodissociation
particulate
nitrate
acidic
environments
into
regional
model
assessed
its
impact
on
coastal
quality
during
autumn
South
China.
The
could
reproduce
over
70%
high
level
measured
at
site,
revealing
discernible
presence
released
adjacent
areas.
Abundant
alters
oxidative
capacity
atmosphere,
consequently
increasing
O3
(6–12%)
PM2.5
(10–16%)
concentrations
high-NOx
areas
reducing
(3%)
concentration
low-NOx
Accounting
chemistry
shifts
–
precursor
relationships
from
VOC
limited
to
mixed
or
NOx
-limited
regimes,
enhancing
benefits
emission
reduction
mitigating
pollution.
Our
findings
suggest
that
tightening
control
two
pollutants,
SO2,
would
alleviate
production
adverse
quality.
ACS Earth and Space Chemistry,
Journal Year:
2024,
Volume and Issue:
8(4), P. 675 - 688
Published: April 1, 2024
The
oxidation
of
alkyl-substituted
aromatic
molecules
produces
oxygenated
volatile
organic
compounds
(OVOCs)
and
secondary
aerosols
(SOA)
that
are
major
components
ambient
urban
air.
Despite
their
ubiquity,
the
impacts
variable
conditions,
such
as
relative
humidity
(RH)
actinic
exposure,
on
physicochemical
processes
contribute
to
SOA
formation
still
subject
ongoing
research
refinement.
In
this
work,
we
perform
laboratory
environmental
chamber
experiments
use
an
I–
FIGAERO–CIMS
examine
molecular
composition
high-NOx
ethylbenzene
products
in
response
varied
(dry
40%
RH,
60%
RH)
during
either
dark
aging
or
photoaging
(with
∼354
nm
UV-A
lights).
Experiments
performed
a
mixed
Cl
OH
radical
environment.
Compared
chemistry,
chemistry
forms
greater
amount
nitroaromatic
by
enhancing
benzaldehyde
phenolic
H
abstraction
while
also
forming
several
organochlorine
may
serve
tracers
for
which
C2H3ClO2
(presumably
chloroacetic
acid)
appears
be
most
consistent
stable.
Organonitrate
(ON)
undergo
hydrolytic
photolytic
losses.
Nitroaromatic
condense
more
efficiently
under
humid
presumably
due
relatively
high
solubility
hydroxy
dihydroxy
molecules,
but
do
not
appear
stable
condensed
phase
photoaging.
Small
oxygenates
make
up
substantial
portion
increases
at
RH
(due
increased
uptake)
photolysis
fragmentation).
Photoaging
initially
leads
degree
oligomerization
before
continued
eventual
loss
these
other
compounds.
Our
results
show
substantially
impact
evolution
many
gas-
particle-phase
species
produced
suggest
factors
can
exert
strong
control
over
evolution,
particularly
regions.
Journal of the American Chemical Society,
Journal Year:
2023,
Volume and Issue:
145(29), P. 15652 - 15657
Published: July 18, 2023
Halogen
atoms
are
important
atmospheric
oxidants
that
have
unidentified
daytime
sources
from
photochemical
halide
oxidation
in
sea
salt
aerosols.
Here,
we
show
the
photolysis
of
nitrate
aqueous
chloride
solutions
generates
nitryl
(ClNO2)
addition
to
Cl2
and
HOCl.
Experimental
modeling
evidence
suggests
O(3P)
formed
minor
channel
oxidizes
HOCl,
which
reacts
with
nitrite
form
ClNO2.
This
chemistry
is
different
than
currently
accepted
mechanisms
involving
by
OH
could
shift
our
understanding
halogen
cycling
lower
atmosphere.
Journal of Geophysical Research Atmospheres,
Journal Year:
2023,
Volume and Issue:
128(22)
Published: Nov. 14, 2023
The
chlorine
radical
(Cl)
plays
a
crucial
role
in
the
formation
of
secondary
air
pollutants
by
determining
total
atmospheric
oxidative
capacity
(AOC).
However,
there
are
still
large
discrepancies
among
studies
on
chemistry,
mainly
due
to
uncertainties
from
three
aspects:
(a)
Anthropogenic
emissions
reactive
species
disinfectant
usage
typically
overlooked.
(b)
heterogeneous
reaction
uptake
coefficients
used
quality
models
resulted
certain
differences.
(c)
co-effect
anthropogenic
and
natural
is
rarely
investigated.
In
this
study,
Weather
Research
Forecasting
(WRF)-Community
Multiscale
Air
Quality
(CMAQ)
modeling
system
(updated
with
21
new
reactions
comprehensive
inventory)
was
simulate
combined
impact
coastal
city
cluster
Yangtze
River
Delta
(YRD)
region.
results
indicate
that
updated
gas-phase
chemistry
can
significantly
enhance
AOC
21.3%,
8.7%,
43.3%,
58.7%
spring,
summer,
autumn,
winter,
respectively.
This
more
evident
inland
areas
high
Cl
concentrations.
Our
updates
also
increases
monthly
mean
maximum
daily
8-hr
average
(MDA
8)
O3
mixing
ratio
4.1-7.0
ppbv
different
seasons.
Additionally,
promotes
fine
particulate
matter
(PM2.5),
enhancements
4.7-13.3
μg/m3
study
underlines
significance
adding
full
updating
models,
demonstrates
may
over
regions.
Abstract.
HOX
radicals
(OH
and
HO2)
are
crucial
oxidants
that
determine
atmospheric
oxidation
capacity
the
production
of
secondary
pollutants;
however,
their
sources
sinks
remain
incompletely
understood
in
certain
forest
maritime
environments.
This
study
measured
HO2
OH
concentrations
using
a
chemical
ionisation
mass
spectrometer
at
subtropical
rural
site
southern
China
from
12
November
to
19
December
2022.
The
average
peak
were
3.50
±
2.47
×
106
cm−3
for
1.34
0.93
108
HO2.
Calculations
based
on
an
observation-constrained
model
revealed
overestimation
during
warm
periods
field
study.
These
inaccuracies
resulted
overestimations
rates
simulation
by
up
98
%
ozone
341
nitric
acid.
Our
highlights
need
further
improving
understanding
sources/sinks
Chlorine
(Cl)
radicals
can
profoundly
affect
the
atmospheric
oxidation
capacity
and
fates
of
pollutants.
Hypochlorous
acid
(HOCl)
is
a
potentially
crucial
Cl
precursor,
yet
understanding
its
formation
mechanisms
impacts
still
limited.
Here,
we
observed
high
concentrations
HOCl
in
coastal
city
Southeast
China
during
autumn
2022,
with
an
average
daytime
peak
181
ppt.
Machine
learning
analysis
identified
Cl2,
O3,
nitrate,
temperature,
iron
as
primary
factors
affecting
distribution.
Beyond
Cl2
photolysis,
both
nitrate
photolysis
aerosol
photochemistry
also
contributed
to
radical
production,
which
drove
production
through
reactions
involving
ClO
HO2
presence
O3.
Both
OH
released
via
increased
levels
ROx
by
∼10%,
thereby
enhancing
O3
generation
capacity.
Our
findings
emphasize
significant
role
chemistry
suggest
that
controlling
could
alleviate
adverse
on
air
quality.
Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(7), P. 4083 - 4106
Published: April 10, 2025
Abstract.
Dimethyl
sulfide
(DMS)
is
primarily
emitted
by
marine
phytoplankton
and
oxidized
in
the
atmosphere
to
form
methanesulfonic
acid
(MSA)
sulfate
aerosols.
Ice
cores
regions
affected
anthropogenic
pollution
show
an
industrial-era
decline
MSA,
which
has
previously
been
interpreted
as
indicating
a
abundance.
However,
simultaneous
increase
DMS-derived
(bioSO4)
Greenland
ice
core
suggests
that
pollution-driven
oxidant
changes
caused
MSA
influencing
relative
production
of
versus
bioSO4.
Here
we
use
GEOS-Chem,
global
chemical
transport
model,
zero-dimensional
box
model
over
three
time
periods
(preindustrial
era,
peak
North
Atlantic
NOx
pollution,
21st
century)
investigate
drivers
bioSO4,
examine
whether
four
DMS
oxidation
mechanisms
reproduce
trends
seasonality
observations.
We
find
GEOS-Chem
simulations
can
only
partially
bioSO4
wide
variation
results
reflects
sensitivity
mechanism
concentrations.
Our
support
hypothesized
nitrate
radical
industrial
increases
production,
but
competing
factors
such
BrO
result
increased
some
simulations,
inconsistent
with
To
improve
understanding
oxidation,
future
work
should
aqueous-phase
chemistry,
produces
82
%–99
%
our
constrain
atmospheric
concentrations,
including
radical,
hydroxyl
reactive
halogens.