Abstract.
Photooxidants
drive
many
atmospheric
chemical
processes.
The
photoexcitation
of
light-absorbing
organic
compounds
(i.e.,
brown
carbon
(BrC))
in
waters
can
lead
to
the
generation
reactive
triplet
excited
states
(3C∗),
which
undergo
further
reactions
produce
other
photooxidants
such
as
singlet
oxygen
(1O2).
To
determine
importance
these
aqueous
SOA
formation
and
transformation,
we
must
know
their
steady-state
concentrations
quantum
yields.
However,
there
has
been
limited
measurements
3C∗1O2
samples
outside
North
America
Europe.
In
this
work,
report
first
yields
produced
aerosols
South
China.
We
quantified
production
illuminated
extracts
PM2.5
collected
different
seasons
at
two
urban
sites
one
coastal
semi-rural
site
during
a
year-round
study
conducted
Hong
Kong,
mass
absorption
coefficients
300
nm
for
BrC
ranged
from
0.49
×
104
2.01
cm2
g-C−1
three
sites.
Both
were
year-round.
([1O2]ss)
spanned
orders
magnitude,
ranging
1.56
10−14
1.35
10−12
M,
with
average
(4.02
±
3.52)
10−13
M.
([3C∗]ss)
2.93
10−16
8.08
(1.09
1.39)
[1O2]ss
[3C∗]ss
correlated
concentration
absorbance
BrC,
thus
implying
that
amount
drives
photooxidants.
locations
(urban
vs.
semi-rural)
did
not
have
significant
effect
on
[1O2]ss,
indicated
local
sources
influence
production.
and
1O2
found
be
highest
winter
lowest
summer
all
observed
seasonal
trends
could
attributed
variations
long-range
air
transport.
Our
analysis
highlighted
key
role
regional
play
influencing
composition
water-soluble
contributed
current
results
will
useful
modeling
aerosol
photochemistry
China
region.
Atmospheric chemistry and physics,
Год журнала:
2024,
Номер
24(1), С. 1 - 21
Опубликована: Янв. 2, 2024
Abstract.
Fog/cloud
drops
and
aerosol
liquid
water
are
important
sites
for
the
transformations
of
atmospheric
species,
largely
through
reactions
with
photoformed
oxidants
such
as
hydroxyl
radical
(⚫OH),
singlet
molecular
oxygen
(1O2∗),
oxidizing
triplet
excited
states
organic
matter
(3C∗).
Despite
their
importance,
few
studies
have
measured
these
or
seasonal
variations.
To
address
this
gap,
we
collected
ambient
PM2.5
from
Davis,
California,
over
course
a
year
photooxidant
concentrations
light
absorption
in
dilute
aqueous
extracts.
Mass
coefficients
(MACs)
normalized
by
dissolved
carbon
range
0.4–3.8
m2
per
gram
C
at
300
nm.
Concentrations
⚫OH,
1O2∗,
3C∗
extracts
(0.2–4.7)
×
10−15
M,
(0.7–45)
10−13
(0.03–7.9)
respectively,
biomass
burning
brown
playing
major
role
formation
1O2∗
3C∗.
Extrapolating
kinetics
our
particle
to
concentrated
(ALW)
conditions
gives
an
estimated
⚫OH
concentration
7
M
ranges
(0.6–7)
10−12
(0.2–1)
respectively.
Compared
results
Kaur
et
al.
(2019),
ALW
predictions
show
roughly
10
times
higher
up
5
3C,
that
lower
factors
20–100.
These
suggest
dominate
processing
compounds
react
quickly
(e.g.,
phenols
furans,
respectively),
while
is
more
less
reactive
organics.
Atmospheric chemistry and physics,
Год журнала:
2023,
Номер
23(15), С. 8805 - 8821
Опубликована: Авг. 9, 2023
Abstract.
Aerosol
liquid
water
(ALW)
is
a
unique
reaction
medium,
but
its
chemistry
poorly
understood.
For
example,
little
known
of
photooxidant
concentrations
–
including
hydroxyl
radicals
(⚫OH),
singlet
molecular
oxygen
(1O2*),
and
oxidizing
triplet
excited
states
organic
matter
(3C*)
even
though
they
likely
drive
much
ALW
chemistry.
Due
to
the
very
limited
content
particles,
it
difficult
quantify
oxidant
in
directly.
To
predict
these
values,
we
measured
illuminated
aqueous
particle
extracts
as
function
dilution
used
resulting
kinetics
extrapolate
conditions.
We
prepared
series
from
two
sets
particles
collected
Davis,
California:
one
winter
(WIN)
summer
(SUM).
Both
periods
are
influenced
by
biomass
burning,
with
dissolved
carbon
(DOC)
ranging
10
495
mg
C
L−1.
In
sample,
⚫OH
concentration
independent
mass
concentration,
an
average
value
5.0
(±
2.2)
×
10−15
M,
while
increases
DOC
range
(0.4–7.7)
M.
both
samples,
3C*
increase
rapidly
then
plateau
under
more
concentrated
conditions,
(0.2–7)
10−13
WIN
SUM
have
same
1O2*
concentrations,
(0.2–8.5)
10−12
linearly
DOC,
approaches
plateau.
next
extrapolated
relationships
formation
rates
sinks
our
dilute
condition
aerosol
water.
Predicted
(including
transport
gas
phase)
(5–8)
similar
those
fog/cloud
waters.
contrast,
predicted
approximately
100
times
higher
than
cloud/fogs,
values
(4–9)
M
(1–5)
respectively.
Although
often
considered
main
sink
for
compounds
atmospheric
phase,
suggest
photooxidants
will
be
important
many
organics
Atmospheric chemistry and physics,
Год журнала:
2023,
Номер
23(16), С. 9245 - 9263
Опубликована: Авг. 22, 2023
Abstract.
Photooxidants
drive
many
atmospheric
chemical
processes.
The
photoexcitation
of
light-absorbing
organic
compounds
(i.e.,
brown
carbon,
BrC)
in
waters
can
lead
to
the
generation
reactive
triplet
excited
states
(3C∗),
which
undergo
further
reactions
produce
other
photooxidants
such
as
singlet
oxygen
(1O2∗).
To
determine
importance
these
aqueous
secondary
aerosol
(SOA)
formation
and
transformation,
we
must
know
their
steady-state
concentrations
quantum
yields.
However,
there
have
been
limited
measurements
3C∗
1O2∗
samples
outside
North
America
Europe.
In
this
work,
report
first
yields
produced
aerosols
South
China.
We
quantified
production
illuminated
extracts
PM2.5
collected
different
seasons
at
two
urban
sites
one
coastal
semi-rural
site
during
a
year-round
study
conducted
Hong
Kong
SAR,
mass
absorption
coefficients
300
nm
for
BrC
ranged
from
0.49
2.01
m2
g-C−1
three
sites.
Both
were
year-round.
([1O2∗]ss)
1.56×10-14
1.35×10-12
M,
with
average
(4.02±3.52)×10-13
M.
At
nearly
2
orders
magnitude
lower
than
[1O2∗]ss,
([3C∗]ss)
2.93×10-16
8.08×10-14
(1.09±1.39)×10-14
also
spanned
wide
ranges
across
samples,
range
1.19
%
13.74
an
(5.19±2.63)
0.05
3.24
(0.56±0.66)
3C∗.
[1O2∗]ss
[3C∗]ss
correlated
concentration
absorbance
BrC,
thus
implying
that
amount
drives
photooxidants.
locations
(urban
vs.
semi-rural)
did
not
significant
effect
on
indicated
local
sources
influence
production.
found
be
highest
winter
lowest
summer
all
observed
seasonal
trends
could
attributed
variations
long-range
air
transport.
Our
analysis
highlighted
key
role
regional
play
influencing
composition
water-soluble
contributed
current
results
will
useful
modeling
photochemistry
China
region.
Biogeosciences,
Год журнала:
2025,
Номер
22(1), С. 243 - 256
Опубликована: Янв. 13, 2025
Abstract.
Microorganisms
in
the
atmosphere
comprise
a
small
fraction
of
Earth's
microbiome.
A
significant
portion
this
aeromicrobiome
consists
bacteria
that
typically
remain
airborne
for
few
days
before
being
deposited.
Unlike
other
spheres
(e.g.,
litho-,
hydro-,
phyllo-,
cryospheres),
atmospheric
are
aerosolized,
residing
individual
particles
and
separated
from
each
other.
In
atmosphere,
encounter
chemical
physical
conditions
affect
their
stress
levels
survival.
This
article
goes
beyond
previous
overviews
by
placing
these
context
fundamental
microphysical
concepts
related
to
aerosols.
We
provide
ranges
water
amounts
surrounding
bacterial
cells
both
inside
outside
clouds
suggest
volumes
cloud
droplets
lead
nutrient
oxidant
limitations.
may
result
greater
limitation
but
lower
oxidative
than
previously
thought.
Various
factors
enhance
or
reduce
microbial
oxidative,
osmotic,
UV-induced),
affecting
functioning
survival
bacteria.
illustrate
could
impact
under
polluted
conditions,
indicating
conclusions
about
role
pollutants
directly
causing
changes
abundance
can
be
erroneous.
The
perspectives
presented
here
aim
motivate
future
experimental
modeling
studies
disentangle
complex
interplay
with
Such
will
help
comprehensively
characterize
modifying
Earth'
microbiome,
which
regulates
stability
global
ecosystems
biodiversity.
Atmosphere,
Год журнала:
2025,
Номер
16(5), С. 567 - 567
Опубликована: Май 9, 2025
Atmospheric
aqueous-phase
reactions
have
been
recognized
as
an
important
source
of
secondary
organic
aerosols
(SOAs).
However,
the
unclear
reaction
kinetics
and
mechanics
hinder
in-depth
understanding
SOA
sources
formation
processes.
This
study
selected
ten
different
substituted
phenolic
compounds
(termed
PhCs)
emitted
from
biomass
burning
precursors,
to
investigate
using
OH
oxidation
under
simulated
sunlight.
The
factors
influencing
rates
were
examined,
contribution
reactive
oxygen
species
(ROS)
was
evaluated
through
quenching
kinetic
analysis
experiments.
results
showed
that
pseudo-first-order
rate
constants
(kobs)
for
ranged
1.03
×
10−4
7.85
s−1
sunlight
irradiation
with
initial
H2O2
concentration
3
mM.
Precursors
electron-donating
groups
(-OH,
-OCH3,
-CH3,
etc.)
exhibited
higher
electrophilic
radical
reactivity
due
enhanced
electron
density
benzene
ring,
leading
than
those
electron-withdrawing
(-NO2,
-CHO,
-COOH).
At
pH
2,
second-order
(kPhCs,
OH)
lower
at
5.
kobs
did
not
show
dependence
on
pH.
presence
O2
facilitated
phenols’
photodecay.
Inorganic
salts
transition
metal
ions
varying
effects
rates.
Specifically,
NO3−
Cu2+
promoted
kPhCs,
OH,
Cl−
significantly
while
SO42−
inhibited
reaction.
determined
be
in
range
109~1010
L
mol−1
via
bimolecular
method,
a
modest
relationship
their
potential
found.
Additionally,
multiple
substituents
can
suppress
toward
•OH
based
Hammett
plots.
Quenching
experiments
revealed
played
dominant
role
compound
degradation
(exceeding
65%).
Electron
paramagnetic
resonance
confirmed
generation
singlet
(1O2)
system,
probe-based
quantification
further
explored
concentrations
1O2
system.
Based
concentrations,
atmospheric
lifetimes
estimated,
providing
valuable
insights
expanding
databases
chemical
transformation
persistence
substances
atmosphere.
Environmental Science Atmospheres,
Год журнала:
2024,
Номер
4(10), С. 1170 - 1182
Опубликована: Янв. 1, 2024
This
study
explores
the
potential
contribution
of
secondary
production
OH
radicals
in
aerosols
and
cloud/fog
conditions
arising
from
brown
carbon
(BrC)
triplet
state
chemistry.
Proceedings of the National Academy of Sciences,
Год журнала:
2024,
Номер
121(51)
Опубликована: Дек. 13, 2024
Biomass-burning
organic
aerosol(s)
(BBOA)
are
rich
in
brown
carbon,
which
significantly
absorbs
solar
irradiation
and
potentially
accelerates
global
warming.
Despite
its
importance,
the
multiphase
photochemistry
of
BBOA
after
light
absorption
remains
poorly
understood
due
to
challenges
determining
oxidant
concentrations
reaction
kinetics
within
aerosol
particles.
In
this
study,
we
explored
photochemical
reactivity
particles
S(IV)
oxidation
sulfate.
We
found
that
sulfate
formation
under
is
predominantly
driven
by
photosensitization
involving
triplet
excited
states
(
3
*
)
instead
iron,
nitrate,
photochemistry.
Rates
three
orders
magnitude
higher
than
those
observed
bulk
solution,
primarily
fast
interfacial
reactions.
Our
results
highlight
chemistry
can
greatly
contribute
sulfate,
as
an
example
secondary
pollutants.
Photosensitization
will
likely
become
increasingly
crucial
intensified
wildfires.
Abstract.
Photooxidants
drive
many
atmospheric
chemical
processes.
The
photoexcitation
of
light-absorbing
organic
compounds
(i.e.,
brown
carbon
(BrC))
in
waters
can
lead
to
the
generation
reactive
triplet
excited
states
(3C∗),
which
undergo
further
reactions
produce
other
photooxidants
such
as
singlet
oxygen
(1O2).
To
determine
importance
these
aqueous
SOA
formation
and
transformation,
we
must
know
their
steady-state
concentrations
quantum
yields.
However,
there
has
been
limited
measurements
3C∗
1O2
samples
outside
North
America
Europe.
In
this
work,
report
first
yields
produced
aerosols
South
China.
We
quantified
production
illuminated
extracts
PM2.5
collected
different
seasons
at
two
urban
sites
one
coastal
semi-rural
site
during
a
year-round
study
conducted
Hong
Kong,
mass
absorption
coefficients
300
nm
for
BrC
ranged
from
0.49
×
104
2.01
cm2
g-C−1
three
sites.
Both
were
year-round.
([1O2]ss)
spanned
orders
magnitude,
ranging
1.56
10−14
1.35
10−12
M,
with
average
(4.02
±
3.52)
10−13
M.
([3C∗]ss)
2.93
10−16
8.08
(1.09
1.39)
[1O2]ss
[3C∗]ss
correlated
concentration
absorbance
BrC,
thus
implying
that
amount
drives
photooxidants.
locations
(urban
vs.
semi-rural)
did
not
have
significant
effect
on
[1O2]ss,
indicated
local
sources
influence
production.
found
be
highest
winter
lowest
summer
all
observed
seasonal
trends
could
attributed
variations
long-range
air
transport.
Our
analysis
highlighted
key
role
regional
play
influencing
composition
water-soluble
contributed
current
results
will
useful
modeling
aerosol
photochemistry
China
region.