Abstract.
Secondary
organic
aerosols
(SOA)
formed
by
oxidation
of
typical
precursors
largely
emitted
biomass
burning,
such
as
PAHs
and
furans,
are
still
poorly
characterized
in
terms
formation
yields,
physical
light
absorption
properties,
particularly
those
generated
at
night
following
reaction
with
nitrate
radicals
(NO3).
In
the
present
study,
we
evaluated
compared
effective
density
(ρeff),
Ångström
exponent
(α),
mass
coefficient
(MAC)
laboratory-generated
SOA
from
three
furan
compounds
(furan,
2-methylfuran,
2,5-dimethylfuran)
four
(naphthalene,
acenaphthylene,
fluorene,
phenanthrene).
were
an
flow
reactor
between
hydroxyl
(OH;
0.1–20
equivalent
aging
days)
or
NO3
(0.05–6
nights
14
h)
single
PAH.
The
ρeff,
α,
MAC
varied
depending
on
precursor
oxidant
considered.
ρeff
OH
tended
to
increase
particle
size
before
reaching
a
“plateau”.
This
was
evident
for
nighttime
chemistry
experiments
(1.2
1.6
average
particles
>
100
nm).
Such
results
highlighted
potential
differences
chemical
composition
SOA,
well
probably
their
morphology,
according
size.
Three
times
lower
yields
obtained
OH.
PAH
(18
76
%)
5
6
higher
than
furans
(3–12
%).
While
showed
low
negligible
found
have
significant
impact
UV-Visible
region,
implying
contribution
atmospheric
brown
carbon
(BrC).
No
values
observed
processes,
due
nitrogen-containing
chromophores
through
homogeneous
gas
phase
processes
only
(without
NOx).
Overall,
this
work
demonstrated
that
both,
day-
substantial
aerosol
properties
so
climate.
Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(1)
Published: Jan. 4, 2024
Abstract
Furans
are
a
major
class
of
volatile
organic
compounds
emitted
from
biomass
burning.
Their
high
reactivity
with
atmospheric
oxidants
leads
to
the
formation
secondary
aerosol
(SOA),
including
brown
carbon
(BrC)
that
can
affect
global
climate
via
interactions
solar
radiation.
Here,
we
investigate
optical
properties
and
chemical
composition
SOA
generated
photooxidation
furfural,
2‐methylfuran,
3‐methylfuran
under
dry
(RH
<
5%)
humid
∼
50%)
conditions
in
presence
nitrogen
oxides
(NO
x
)
ammonium
sulfate
seed
aerosol.
Dry
furfural
oxidation
has
greatest
BrC
formation,
reduced
nitrogen‐containing
(NOCs)
SOA,
which
dominated
by
amines
amides
formed
reactions
between
carbonyls
ammonia/ammonium.
Based
on
products
detected,
propose
novel
pathways
NOCs
photooxidation,
contribute
accretion
during
photochemical
aging
burning
plumes.
ACS Earth and Space Chemistry,
Journal Year:
2024,
Volume and Issue:
8(5), P. 857 - 899
Published: April 8, 2024
Furanoids
are
a
class
of
reactive
volatile
organic
compounds
that
major
products
from
the
pyrolysis
and
combustion
biomass
polymers,
including
cellulose,
hemicellulose,
lignin.
Biomass
burning
is
an
atmospheric
source
furanoids
increasing
in
frequency
intensity
throughout
regions
world.
Once
emitted
to
atmosphere,
may
react
with
oxidants
form
secondary
pollutants
hazardous
human
health,
ozone
(O3)
aerosol
(SOA).
This
review
comprehensive
assessment
literature
between
1977
present
describing
emissions
fate
wild,
prescribed,
domestic
fires.
The
organized
by
presenting
physical
properties
key
first,
followed
summary
biopolymer
reactions
lead
furanoid
formation.
Next,
factors
compiled
across
typical
fuels
consumed
highlight
species
smoke.
We
next
available
kinetic
degradation
mechanism
data
characterize
reaction
rates,
gas-phase
products,
SOA
formed
as
result
OH,
NO3,
O3,
Cl
radicals.
then
describe
studies
have
focused
on
evaluating
chemistry
their
impacts
air
quality
using
combination
field
observations
model
simulations.
conclude
perspective
identifies
future
research
directions
would
address
gaps
improve
understanding
processes.
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(48), P. 20085 - 20096
Published: Nov. 20, 2023
The
light
absorption
properties
of
brown
carbon
(BrC),
which
are
linked
to
molecular
chromophores,
may
play
a
significant
role
in
the
Earth's
energy
budget.
While
nitroaromatic
compounds
have
been
identified
as
strong
chromophores
wildfire-driven
BrC,
other
types
remain
be
investigated.
Given
electron-withdrawing
nature
carbonyls
ubiquitous
atmosphere,
we
characterized
carbonyl
BrC
samples
from
nighttime
oxidation
furan
and
pyrrole
derivatives,
important
but
understudied
precursors
secondary
organic
aerosols
primarily
found
wildfire
emissions.
Various
were
quantified
samples,
their
ultraviolet-visible
spectra
simulated
by
using
time-dependent
density
functional
theory.
Our
findings
suggest
that
with
bonded
nitrogen
(i.e.,
imides
amides)
derived
N-containing
heterocyclic
substantially
contribute
absorption.
contributed
over
40%
total
at
wavelengths
below
350
nm
above
430
BrC.
contributions
differed
significantly
wavelength,
highlighting
divergent
importance
different
wavelength
ranges.
Overall,
our
highlight
significance
underscore
need
for
further
investigation.
ACS ES&T Air,
Journal Year:
2024,
Volume and Issue:
1(5), P. 426 - 437
Published: April 9, 2024
Light-absorbing
secondary
organic
aerosols
(SOAs),
also
known
as
brown
carbon
(BrC),
are
major
components
of
wildfire
smoke
that
can
have
a
significant
impact
on
the
climate
system;
however,
how
environmental
factors
such
relative
humidity
(RH)
influence
their
formation
is
not
fully
understood,
especially
for
heterocyclic
precursors.
We
conducted
chamber
experiments
to
investigate
BrC
from
nighttime
oxidation
furan
and
pyrrole,
two
primary
precursors
in
wildfires,
presence
pre-existing
particles
at
RH
<
20%
∼
50%.
Our
findings
revealed
increasing
significantly
affected
size
distribution
dynamics
both
SOAs,
with
pyrrole
SOA
showing
stronger
potential
generate
ultrafine
via
intensive
nucleation
processes.
Higher
led
increased
mass
fractions
oxygenated
compounds
suggesting
enhanced
gas-phase
and/or
multiphase
under
humid
conditions.
Moreover,
higher
reduced
absorption
coefficients
BrC,
contrasting
those
homocyclic
precursors,
due
non-absorbing
high-molecular-weight
decreasing
molecular
chromophores.
Overall,
our
demonstrate
unique
dependence
which
may
critically
modulate
radiative
effects
change.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(23), P. 15077 - 15096
Published: Dec. 7, 2023
Abstract.
Secondary
organic
aerosols
(SOAs)
formed
by
oxidation
of
typical
precursors
largely
emitted
biomass
burning,
such
as
polycyclic
aromatic
hydrocarbons
(PAHs)
and
furans,
are
still
poorly
characterized.
We
evaluated
compared
the
formation
yields,
effective
density
(ρeff),
absorption
Ångström
exponent
(α),
mass
coefficient
(MAC)
laboratory-generated
SOAs
from
three
furan
compounds
four
PAHs.
were
generated
in
an
flow
reactor
under
day-
(OH
radicals)
or
nighttime
(NO3
conditions.
The
ρeff,
α,
MAC
varied
depending
on
precursor
oxidant
considered.
ρeff
with
OH
NO3
tended
to
increase
particle
size
before
reaching
a
“plateau”,
highlighting
potential
differences
SOA
chemical
composition
and/or
morphology,
according
size.
Three
times
lower
yields
obtained
OH.
PAH
(18
%–76
%)
five
six
higher
than
those
for
furans
(3
%–12
%).
While
showed
low
negligible
light
properties,
had
significant
impact
UV–visible
region,
implying
contribution
atmospheric
brown
carbon.
No
values
was
observed
processes,
probably
due
nitrogen-containing
chromophores
only
(without
NOx).
results
demonstrated
that
PAHs
through
both,
have
substantial
aerosol
properties.
Abstract.
Secondary
organic
aerosols
(SOA)
formed
by
oxidation
of
typical
precursors
largely
emitted
biomass
burning,
such
as
PAHs
and
furans,
are
still
poorly
characterized
in
terms
formation
yields,
physical
light
absorption
properties,
particularly
those
generated
at
night
following
reaction
with
nitrate
radicals
(NO3).
In
the
present
study,
we
evaluated
compared
effective
density
(ρeff),
Ångström
exponent
(α),
mass
coefficient
(MAC)
laboratory-generated
SOA
from
three
furan
compounds
(furan,
2-methylfuran,
2,5-dimethylfuran)
four
(naphthalene,
acenaphthylene,
fluorene,
phenanthrene).
were
an
flow
reactor
between
hydroxyl
(OH;
0.1–20
equivalent
aging
days)
or
NO3
(0.05–6
nights
14
h)
single
PAH.
The
ρeff,
α,
MAC
varied
depending
on
precursor
oxidant
considered.
ρeff
OH
tended
to
increase
particle
size
before
reaching
a
“plateau”.
This
was
evident
for
nighttime
chemistry
experiments
(1.2
1.6
average
particles
>
100
nm).
Such
results
highlighted
potential
differences
chemical
composition
SOA,
well
probably
their
morphology,
according
size.
Three
times
lower
yields
obtained
OH.
PAH
(18
76
%)
5
6
higher
than
furans
(3–12
%).
While
showed
low
negligible
found
have
significant
impact
UV-Visible
region,
implying
contribution
atmospheric
brown
carbon
(BrC).
No
values
observed
processes,
due
nitrogen-containing
chromophores
through
homogeneous
gas
phase
processes
only
(without
NOx).
Overall,
this
work
demonstrated
that
both,
day-
substantial
aerosol
properties
so
climate.
Molecular
characterization
of
organic
aerosol
(OA)
is
crucial
for
understanding
its
sources
and
atmospheric
processes.
However,
the
chemical
components
OA
remain
not
well
constrained.
This
study
used
gas
chromatography–Orbitrap
mass
spectrometry
(GC-Orbitrap
MS)
GC-Quadrupole
MS
(GC-qMS)
to
investigate
composition
in
PM2.5
from
Xi'an,
Northwest
China.
GC-Orbitrap
identified
335
tracers,
including
overlooked
isomers
low-concentration
molecules,
approximately
1.6
times
more
than
GC-qMS.
The
"molecular
corridor"
assessment
shows
superior
capability
identifying
an
expansive
range
compounds
with
higher
volatility
oxidation
states,
such
as
furanoses/pyranoses,
di/hydroxy/ketonic
acids,
di/poly
alcohols,
aldehydes/ketones,
amines/amides.
Seasonal
variations
reflect
diverse
sources:
increased
alcohols
winter
are
derived
indoor
emissions,
furanoses/pyranoses
heterocyclics
spring
summer
might
be
biogenic
emissions
secondary
formation,
amides
autumn
probably
biomass
burning.
Integrating
partial
least
squares
discriminant
analysis
(PLS-DA)
potential
source
contribution
function
(PSCF)
models,
similarities
differences
further
elucidated,
highlighting
role
local
transport
southern
cities.
offers
new
insights
into
aided
by
high
resolution
sensitivity
MS.
ACS ES&T Air,
Journal Year:
2024,
Volume and Issue:
1(12), P. 1637 - 1649
Published: Nov. 27, 2024
Sulfur-containing
volatile
organic
compounds
emitted
during
wildfire
events,
such
as
dimethyl
sulfide,
are
known
to
form
secondary
aerosols
containing
inorganic
sulfate
(SO42–)
and
surfactant-like
compounds;
however,
little
is
about
the
fate
of
sulfur
in
other
reduced
organosulfur
species.
This
study
aimed
determine
sulfurous
product
distribution
resulting
from
nighttime
oxidation
thiophene
a
model
system.
Ion
chromatography
(IC)
aerosol
mass
spectrometry
(a
mini
spectrometer,
mAMS)
were
used
constrain
proportions
produced
under
wildfire-relevant
conditions
([NO2]/[O3]
=
0.1).
With
constraints
IC,
results
indicated
that
particle
consisted
30.3
±
6.6%
SO42–,
while
mAMS
fractionation
attributed
24.5
1.6%
total
signal
15.4
1.9%
organosulfates,
60.1
0.9%
sulfonates.
Empirical
formulas
products
identified
C1–C8
organosulfates
sulfonates
using
complementary
techniques.
highlights
its
derivatives
source
SO42–
particulate
compounds,
which
have
important
implications
for
atmospheric
budget
aerosol/droplet
physical
chemical
properties.
Abstract.
Secondary
organic
aerosols
(SOA)
formed
by
oxidation
of
typical
precursors
largely
emitted
biomass
burning,
such
as
PAHs
and
furans,
are
still
poorly
characterized
in
terms
formation
yields,
physical
light
absorption
properties,
particularly
those
generated
at
night
following
reaction
with
nitrate
radicals
(NO3).
In
the
present
study,
we
evaluated
compared
effective
density
(ρeff),
Ångström
exponent
(α),
mass
coefficient
(MAC)
laboratory-generated
SOA
from
three
furan
compounds
(furan,
2-methylfuran,
2,5-dimethylfuran)
four
(naphthalene,
acenaphthylene,
fluorene,
phenanthrene).
were
an
flow
reactor
between
hydroxyl
(OH;
0.1–20
equivalent
aging
days)
or
NO3
(0.05–6
nights
14
h)
single
PAH.
The
ρeff,
α,
MAC
varied
depending
on
precursor
oxidant
considered.
ρeff
OH
tended
to
increase
particle
size
before
reaching
a
“plateau”.
This
was
evident
for
nighttime
chemistry
experiments
(1.2
1.6
average
particles
>
100
nm).
Such
results
highlighted
potential
differences
chemical
composition
SOA,
well
probably
their
morphology,
according
size.
Three
times
lower
yields
obtained
OH.
PAH
(18
76
%)
5
6
higher
than
furans
(3–12
%).
While
showed
low
negligible
found
have
significant
impact
UV-Visible
region,
implying
contribution
atmospheric
brown
carbon
(BrC).
No
values
observed
processes,
due
nitrogen-containing
chromophores
through
homogeneous
gas
phase
processes
only
(without
NOx).
Overall,
this
work
demonstrated
that
both,
day-
substantial
aerosol
properties
so
climate.