Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(18), P. 12873 - 12885
Published: Sept. 9, 2022
The
light-absorbing
organic
aerosol
(OA)
constitutes
an
important
fraction
of
absorbing
components,
counteracting
major
cooling
effect
aerosols
to
climate.
mechanisms
in
linking
the
complex
and
changeable
chemistry
OA
with
its
properties
remain
be
elucidated.
Here,
by
using
solvent
extraction,
ambient
from
urban
environment
was
fractionated
according
polarity,
which
further
nebulized
online
characterized
compositions
properties.
Water
extracted
high-polar
compounds
a
significantly
higher
oxygen
carbon
ratio
(O/C)
than
methanol
extracts.
A
transition
O/C
about
0.6
found,
below
above
enhancement
reduction
absorptivity
were
observed
increasing
O/C,
occurring
on
less
polar
high
compounds,
respectively.
In
particular,
co-increase
nitrogen
elements
suggests
role
nitrogen-containing
functional
groups
enhancing
(e.g.,
forming
aromatics),
while
oxidation
(O/C
>
0.6)
likely
led
fragmentation
bleaching
chromophores.
results
here
may
reconcile
previous
observations
darkening
or
whitening
chromophores
brown
carbon,
parametrization
has
potential
link
changing
polarity
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(4), P. 2513 - 2532
Published: March 2, 2020
Abstract.
Brown
carbon
(BrC)
plays
an
essential
impact
on
radiative
forcing
due
to
its
ability
absorb
sunlight.
In
this
study,
the
optical
properties
and
molecular
characteristics
of
water-soluble
methanol-soluble
organic
(OC;
MSOC)
emitted
from
simulated
combustion
biomass
coal
fuels
vehicle
emissions
were
investigated
using
ultraviolet–visible
(UV–vis)
spectroscopy,
excitation–emission
matrix
(EEM)
Fourier
transform
ion
cyclotron
resonance
mass
spectrometry
(FT-ICR
MS)
coupled
with
electrospray
ionization
(ESI).
The
results
showed
that
these
smoke
aerosol
samples
burning
(BB)
(CC)
had
a
higher
absorption
efficiency
at
365
nm
(MAE365)
than
emission
samples.
A
stronger
MAE365
value
was
also
found
in
MSOC
(WSOC),
indicating
low
polar
compounds
would
possess
light
capacity.
Parallel
factor
(PARAFAC)
analysis
identified
six
types
fluorophores
(P1–6)
WSOC
including
two
humic-like
substances
(HULIS-1)
(P1
P6),
three
protein-like
(PLOM)
(P2,
P3,
P5),
one
undefined
substance
(P4).
HULIS-1
mainly
aging
exhaust
particles;
P2
only
abundant
BB
aerosols;
P3
ubiquitous
all
tested
P4
fossil
P5
more
intense
fresh
particles.
chromophores
(six
components;
C1–6)
exhibited
consistent
WSOC,
suggesting
method
could
be
used
indicate
origins
chromophores.
FT-ICR
spectra
CHO
CHON
most
components
but
S-containing
appeared
abundance
CC
aerosols
aerosols,
while
considerably
fewer
largely
detected
MSOC.
unique
formulas
different
sources
van
Krevelen
(VK)
diagram
presented
distributions.
To
specific,
medium
H
∕
C
O
ratio,
opposite
ratio.
Moreover,
capacity
positively
associated
unsaturation
degree
weight
source
aerosols.
above
are
potentially
applicable
further
studies
EEM-based
or
molecular-characteristic-based
apportionment
atmospheric
Nature Geoscience,
Journal Year:
2023,
Volume and Issue:
16(8), P. 683 - 688
Published: Aug. 1, 2023
Wildfires
emit
large
amounts
of
black
carbon
and
light-absorbing
organic
carbon,
known
as
brown
into
the
atmosphere.
These
particles
perturb
Earth's
radiation
budget
through
absorption
incoming
shortwave
radiation.
It
is
generally
thought
that
loses
its
absorptivity
after
emission
in
atmosphere
due
to
sunlight-driven
photochemical
bleaching.
Consequently,
atmospheric
warming
effect
exerted
by
remains
highly
variable
poorly
represented
climate
models
compared
with
relatively
nonreactive
carbon.
Given
wildfires
are
predicted
increase
globally
coming
decades,
it
increasingly
important
quantify
these
radiative
impacts.
Here
we
present
measurements
ensemble-scale
particle-scale
smoke
plumes
from
western
United
States.
We
find
a
type
dark
contributes
three-quarters
short
visible
light
half
long
absorption.
This
strongly
absorbing
aerosol
species
water
insoluble,
resists
daytime
photobleaching
increases
night-time
processing.
Our
findings
suggest
parameterizations
need
be
revised
improve
estimation
forcing
associated
warming.
Environmental Science & Technology,
Journal Year:
2019,
Volume and Issue:
53(23), P. 13607 - 13617
Published: Nov. 4, 2019
Water-soluble
organic
compounds
(WSOC)
and
methanol-soluble
(MSOC)
in
smoke
particles
emitted
from
residential
coal
combustion
were
characterized
by
ultrahigh-resolution
mass
spectrometry.
The
results
showed
that
the
molecular
compositions
of
WSOC
MSOC
are
different.
S-containing
(CHOS
CHONS)
found
to
be
dominant
components
(65-87%)
WSOC,
whereas
CHO
CHON
make
a
great
contribution
(79-96%)
samples.
It
is
worth
noting
greater
abundance
was
produced
compared
biomass
burning
atmospheric
also
varied
significantly
depending
on
maturity
coal.
derived
low-maturity
contained
higher
proportion
oxidized
functional
groups
but
with
lower
degree
aromaticity
than
high-maturity
Our
findings
suggest
molecules
high
modified
index,
low
O/C
ratio,
polarity
stronger
light
absorption.
This
study
suggests
contributed
absorption
may
stronger.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(9), P. 5701 - 5710
Published: April 7, 2021
Smog
chamber
experiments
were
conducted
to
characterize
the
light
absorption
of
brown
carbon
(BrC)
from
primary
and
photochemically
aged
coal
combustion
emissions.
Light
was
measured
by
UV–visible
spectrophotometric
analysis
water
methanol
extracts
filter
samples.
The
single-scattering
albedo
at
450
nm
0.73
±
0.10
for
emissions
0.75
0.13
coefficient
365
higher
than
that
a
factor
10
7
This
suggests
majority
BrC
is
water-insoluble
even
after
aging.
mass
efficiency
this
(MAE365)
OA
(POA)
dependent
on
conditions,
with
an
average
0.84
0.54
m2
g–1,
which
significantly
(0.24
0.18
g–1).
Secondary
(SOA)
dominated
decreased
MAE365
aging
indicates
SOA
less
absorbing
POA
and/or
bleached
(oxidized)
estimated
(0.14
0.08
g–1)
much
lower
POA.
A
comparison
residential
other
anthropogenic
sources
are
among
strongest
organics.
Proceedings of the National Academy of Sciences,
Journal Year:
2022,
Volume and Issue:
119(38)
Published: Sept. 12, 2022
Biomass
burning
organic
aerosol
(BBOA)
in
the
atmosphere
contains
many
compounds
that
absorb
solar
radiation,
called
brown
carbon
(BrC).
While
BBOA
is
atmosphere,
BrC
can
undergo
reactions
with
oxidants
such
as
ozone
which
decrease
absorbance,
or
whiten.
The
effect
of
temperature
and
relative
humidity
(RH)
on
whitening
has
not
been
well
constrained,
leading
to
uncertainties
when
predicting
direct
radiative
climate.
Using
an
flow-tube
reactor,
we
show
by
oxidation
strongly
dependent
RH
temperature.
a
poke-flow
technique,
viscosity
also
depends
these
conditions.
measured
rate
described
data,
assuming
due
occurring
bulk
BBOA,
within
thin
shell
beneath
surface.
our
combined
datasets,
developed
kinetic
model
this
process,
lifetime
1
d
less
below
∼1
km
altitude
but
often
much
longer
than
above
altitude.
Including
dependence
chemical
transport
causes
large
change
predicted
warming
Overall,
results
illustrate
need
be
considered
understand
role
atmosphere.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(10), P. 6449 - 6470
Published: May 19, 2022
Abstract.
Brown
carbon
(BrC)
aerosols
exert
vital
impacts
on
climate
change
and
atmospheric
photochemistry
due
to
their
light
absorption
in
the
wavelength
range
from
near-ultraviolet
(UV)
visible
light.
However,
optical
properties
formation
mechanisms
of
ambient
BrC
remain
poorly
understood,
limiting
estimation
radiative
forcing.
In
present
study,
fine
particles
(PM2.5)
were
collected
during
2016–2017
a
day/night
basis
over
urban
Tianjin,
megacity
northern
China.
Light
fluorescence
water
extracts
PM2.5
investigated
obtain
seasonal
diurnal
patterns
water-soluble
BrC.
There
obvious
seasonal,
but
no
evident
diurnal,
variations
winter,
showed
much
stronger
light-absorbing
ability,
with
mass
efficiency
at
365
nm
(MAE365)
winter
(1.54±0.33
m2
gC−1)
that
was
1.8
times
larger
than
MAE365
summer
(0.84±0.22
gC−1).
Direct
effects
by
relative
black
UV
54.3±16.9
%
44.6±13.9
summer,
respectively.
addition,
five
fluorescent
components
BrC,
including
three
humic-like
fluorophores
two
protein-like
identified
excitation–emission
matrix
spectrometry
parallel
factor
(PARAFAC)
analysis.
The
less
oxygenated
contributed
more
nighttime
samples,
while
increased
daytime
samples.
higher
humification
index
(HIX),
together
lower
biological
(BIX)
(FI),
suggests
chemical
compositions
associated
high
aromaticity
degree
photobleaching.
Fluorescent
indicate
wintertime
predominantly
affected
primary
emissions
fresh
secondary
organic
aerosol
(SOA),
ones
influenced
aging
processes.
Results
source
apportionments
using
molecular
same
set
reveal
fossil
fuel
combustion
processes,
bioaerosol
emission,
biomass
burning,
biogenic
anthropogenic
SOA
main
sources
Biomass
burning
nighttime,
daytime.
particular,
our
study
highlights
emission
is
an
important
Tianjin
summer.