Geophysical Research Letters,
Journal Year:
2021,
Volume and Issue:
48(8)
Published: March 22, 2021
Abstract
Despite
the
recent
decrease
in
pollution
events
Chinese
urban
areas,
World
Health
Organization
air
quality
guideline
values
are
still
exceeded.
Observations
from
monitoring
networks
show
a
stronger
of
organic
aerosol
directly
emitted
to
atmosphere
relative
secondary
(SOA)
generated
oxidation
processes.
Here,
uptake
water‐soluble
gas‐phase
products
is
reported
as
major
SOA
contribution
particulate
Beijing,
triggered
by
increase
liquid
water.
In
episodes,
this
pathway
enough
explain
mass,
with
formaldehyde,
acetaldehyde,
glycolaldehyde,
formic
acid,
and
acetic
acid
alone
explaining
15%–25%
increase.
Future
mitigation
strategies
reduce
non‐methane
volatile
compound
emissions
should
be
considered
China.
Environmental Science & Technology,
Journal Year:
2020,
Volume and Issue:
54(14), P. 8568 - 8579
Published: June 19, 2020
Biomass
burning
is
the
largest
combustion-related
source
of
volatile
organic
compounds
(VOCs)
to
atmosphere.
We
describe
development
a
state-of-the-science
model
simulate
photochemical
formation
secondary
aerosol
(SOA)
from
biomass-burning
emissions
observed
in
dry
(RH
<20%)
environmental
chamber
experiments.
The
modeling
supported
by
(i)
new
oxidation
measurements,
(ii)
detailed
concurrent
measurements
SOA
precursors
emissions,
and
(iii)
parameters
for
heterocyclic
oxygenated
aromatic
based
on
historical
find
that
compounds,
including
phenols
methoxyphenols,
account
slightly
less
than
60%
formed
help
our
explain
variability
mass
(R2
=
0.68)
O/C
0.69)
enhancement
ratios
across
11
Despite
abundant
included
furans
contribute
∼20%
total
SOA.
use
pyrolysis-temperature-based
or
averaged
emission
profiles
represent
precursors,
rather
those
specific
each
fire,
provide
similar
results
within
20%.
Our
findings
demonstrate
necessity
accounting
aromatics
their
chemical
mechanisms.
Science Advances,
Journal Year:
2021,
Volume and Issue:
7(50)
Published: Dec. 8, 2021
Wildfires
are
a
substantial
but
poorly
quantified
source
of
tropospheric
ozone
(O3).
Here,
to
investigate
the
highly
variable
O3
chemistry
in
wildfire
plumes,
we
exploit
situ
chemical
characterization
western
wildfires
during
FIREX-AQ
flight
campaign
and
show
that
production
can
be
predicted
as
function
experimentally
constrained
OH
exposure,
volatile
organic
compound
(VOC)
reactivity,
fate
peroxy
radicals.
The
exhibits
rapid
transition
regimes.
Within
few
daylight
hours,
formation
substantially
slows
is
largely
limited
by
abundance
nitrogen
oxides
(NOx).
This
finding
supports
previous
observations
enhanced
when
VOC-rich
smoke
mixes
into
NOx-rich
urban
thereby
deteriorating
air
quality.
Last,
relate
underlying
fire
characteristics,
enabling
more
accurate
representation
atmospheric
models
used
study
quality
predict
climate.
Proceedings of the National Academy of Sciences,
Journal Year:
2021,
Volume and Issue:
118(52)
Published: Dec. 20, 2021
Significance
Understanding
the
sources
of
tropospheric
ozone
is
important
for
effective
air
quality
management
and
accurate
radiative
forcing
attribution.
Biomass
burning
emits
large
quantities
precursors
to
lower
atmosphere.
This
source
can
drive
regional-scale
production,
but
its
impact
on
global
poorly
constrained.
Here,
we
present
unique
in
situ
aircraft
observations
continental
pollution
tracers.
Ozone
enhancements
attributable
biomass
equal
or
exceed
those
from
urban
emissions,
a
result
that
not
predicted
by
current
chemical
transport
models.
These
findings
represent
potentially
major
shift
understanding
atmosphere
indicate
need
model
developments
improve
representation
ozone.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(23), P. 14769 - 14785
Published: Dec. 2, 2020
Abstract.
Volatile
organic
compounds
(VOCs)
play
important
roles
in
the
tropospheric
atmosphere.
In
this
study,
VOCs
were
measured
at
an
urban
site
Guangzhou,
one
of
megacities
Pearl
River
Delta
(PRD),
using
a
gas
chromatograph–mass
spectrometer/flame
ionization
detection
(GC–MS/FID)
and
proton
transfer
reaction
time-of-flight
mass
spectrometer
(PTR-ToF-MS).
Diurnal
profile
analyses
show
that
stronger
chemical
removal
by
OH
radicals
for
more
reactive
hydrocarbons
occurs
during
daytime,
which
is
used
to
estimate
daytime
average
radical
concentration.
comparison,
diurnal
profiles
oxygenated
volatile
(OVOCs)
indicate
evidence
contributions
from
secondary
formation.
Detailed
source
OVOCs,
photochemical
age-based
parameterization
method,
suggest
both
primary
emissions
formation
OVOCs.
During
campaign,
around
1700
ions
detected
PTR-ToF-MS
spectra,
among
there
462
with
noticeable
concentrations.
VOC
signals
these
are
quantified
based
on
sensitivities
available
species.
OVOC-related
dominated
contribution
73
%
±
9
%.
Combining
measurements
GC–MS/FID,
OVOCs
contribute
57
10
total
concentration
VOCs.
Using
concurrent
reactivity,
greatly
reactivity
(19
%).
account
21
11
reactivity.
Adding
up
inorganic
gases
(48
15
%),
∼
(range
0
%–19
%)
remains
`missing”,
well
within
combined
uncertainties
between
calculated
Our
results
demonstrate
emission
evolution
budget
Journal of Geophysical Research Atmospheres,
Journal Year:
2021,
Volume and Issue:
126(11)
Published: May 9, 2021
Abstract
We
present
emission
measurements
of
volatile
organic
compounds
(VOCs)
for
western
U.S.
wildland
fires
made
on
the
NSF/NCAR
C‐130
research
aircraft
during
Western
Wildfire
Experiment
Cloud
Chemistry,
Aerosol
Absorption,
and
Nitrogen
(WE‐CAN)
field
campaign
in
summer
2018.
VOCs
were
measured
with
complementary
instruments
onboard
C‐130,
including
a
proton‐transfer‐reaction
time‐of‐flight
mass
spectrometer
(PTR‐ToF‐MS)
two
gas
chromatography
(GC)‐based
methods.
Agreement
within
combined
instrument
uncertainties
(<60%)
was
observed
most
co‐measured
VOCs.
GC‐based
speciated
isomeric
contributions
to
selected
PTR‐ToF‐MS
ion
masses
generally
showed
little
fire‐to‐fire
variation.
report
ratios
(ERs)
factors
(EFs)
161
31
near‐fire
smoke
plume
transects
24
specific
individual
sampled
afternoon
when
burning
conditions
are
typically
active.
Modified
combustion
efficiency
(MCE)
ranged
from
0.85
0.94.
The
campaign‐average
total
VOC
EF
26.1
±
6.9
g
kg
−1
,
approximately
67%
which
is
accounted
by
oxygenated
10
abundantly
emitted
species
contributed
more
than
half
mass.
found
that
MCE
alone
explained
nearly
70%
variance
emissions
(
r
2
=
0.67)
>50%
57
EFs
representing
carbon
Finally,
we
variability
fraction
emissions,
suggesting
single
speciation
profile
can
describe
wildfires
coniferous
ecosystems
WE‐CAN.
Journal of Geophysical Research Atmospheres,
Journal Year:
2022,
Volume and Issue:
128(2)
Published: Dec. 30, 2022
Abstract
The
NOAA/NASA
Fire
Influence
on
Regional
to
Global
Environments
and
Air
Quality
(FIREX‐AQ)
experiment
was
a
multi‐agency,
inter‐disciplinary
research
effort
to:
(a)
obtain
detailed
measurements
of
trace
gas
aerosol
emissions
from
wildfires
prescribed
fires
using
aircraft,
satellites
ground‐based
instruments,
(b)
make
extensive
suborbital
remote
sensing
fire
dynamics,
(c)
assess
local,
regional,
global
modeling
fires,
(d)
strengthen
connections
observables
the
ground
such
as
fuels
fuel
consumption
satellite
products
burned
area
radiative
power.
From
Boise,
ID
western
were
studied
with
NASA
DC‐8
two
NOAA
Twin
Otter
aircraft.
high‐altitude
ER‐2
deployed
Palmdale,
CA
observe
some
these
in
conjunction
overpasses
other
Further
conducted
three
mobile
laboratories
sites,
17
different
forecast
analyses
for
fire,
air
quality
climate
implications.
Salina,
KS
investigated
87
smaller
Southeast
in‐situ
data
collection.
Sampling
by
all
platforms
designed
measure
gases
aerosols
multiple
transects
capture
chemical
transformation
perform
observations
smoke
plumes
under
day
night
conditions.
linked
consumed
power
orbital
collected
during
overflights
sampling
fuels.
Atmospheric chemistry and physics,
Journal Year:
2024,
Volume and Issue:
24(2), P. 929 - 956
Published: Jan. 23, 2024
Abstract.
Extensive
airborne
measurements
of
non-methane
organic
gases
(NMOGs),
methane,
nitrogen
oxides,
reduced
species,
and
aerosol
emissions
from
US
wild
prescribed
fires
were
conducted
during
the
2019
NOAA/NASA
Fire
Influence
on
Regional
to
Global
Environments
Air
Quality
campaign
(FIREX-AQ).
Here,
we
report
atmospheric
enhancement
ratios
(ERs)
inferred
emission
factors
(EFs)
for
compounds
measured
board
NASA
DC-8
research
aircraft
nine
wildfires
one
fire,
which
encompass
a
range
vegetation
types.
We
use
photochemical
proxies
identify
young
smoke
reduce
effects
chemical
degradation
our
calculations.
ERs
EFs
calculated
FIREX-AQ
observations
agree
within
factor
2,
with
values
reported
previous
laboratory
field
studies
more
than
80
%
carbon-
nitrogen-containing
species.
Wildfire
are
parameterized
based
correlations
sum
NMOGs
reactive
oxides
(NOy)
modified
combustion
efficiency
(MCE)
as
well
other
signatures
indicative
flaming/smoldering
combustion,
including
carbon
monoxide
(CO),
dioxide
(NO2),
black
aerosol.
The
primary
NMOG
correlates
MCE
an
R2
0.68
slope
−296
±
51
g
kg−1,
consistent
studies.
mixing
CO
0.98
137
4
ppbv
per
parts
million
by
volume
(ppmv)
CO,
demonstrating
that
can
be
estimated
CO.
Individual
species
correlate
better
NO2,
NOy,
More
half
NOy
in
fresh
plumes
is
NO2
0.95
ratio
0.55
0.05
ppbv−1,
highlighting
fast
photochemistry
had
already
occurred
sampled
fire
plumes.
follows
trends
observed
experiments
increases
exponentially
MCE,
due
increased
key
at
higher
flaming
combustion.
These
parameterizations
will
provide
accurate
boundary
conditions
modeling
satellite
plume
chemistry
evolution
predict
downwind
formation
secondary
pollutants,
ozone
Environmental Science & Technology,
Journal Year:
2020,
Volume and Issue:
54(21), P. 13467 - 13477
Published: Oct. 21, 2020
Emissions
of
aromatic
compounds
cause
air
pollution
and
detrimental
health
effects.
Here,
we
explore
the
reaction
kinetics
products
key
radicals
in
benzene
photo-oxidation.
After
initial
OH
addition
with
O2,
effective
production
rates
phenol
bicyclic
peroxy
radical
(BCP-peroxy)
are
experimentally
constrained
at
295
K
to
be
420
±
80
370
70
s–1,
respectively.
These
lead
approximately
53%
yield
for
47%
BCP-peroxy
under
atmospheric
conditions.
The
NO
produces
hydroxy
nitrate
a
branching
ratio
<0.2%,
indicating
efficient
NOx
recycling.
Similarly,
HO2
largely
recycles
HOx,
producing
corresponding
alkoxy
(BCP-oxy).
Because
presence
C–C
double
bonds
multiple
functional
groups,
chemistry
BCP-oxy
other
system
is
diverse.
Experimental
results
suggest
aldehydic
H-shift
ring-closure
produce
an
epoxide
functionality
could
competitive
classic
decomposition
radicals.
reactions
potential
sources
highly
oxygenated
molecules.
Finally,
despite
large
number
observed
our
study,
unable
account
∼20%
carbon
flow.
Atmospheric chemistry and physics,
Journal Year:
2019,
Volume and Issue:
19(19), P. 12797 - 12809
Published: Oct. 14, 2019
Abstract.
Biomass
burning
is
an
important
source
of
aerosol
and
trace
gases
to
the
atmosphere,
but
how
these
emissions
change
chemically
during
their
lifetimes
not
fully
understood.
As
part
Fire
Influence
on
Regional
Global
Environments
Experiment
(FIREX
2016),
we
investigated
effect
photochemical
aging
biomass
organic
(BBOA)
with
a
focus
fuels
from
western
United
States.
Emissions
were
sampled
into
small
(150
L)
environmental
chamber
photochemically
aged
via
addition
ozone
irradiation
by
254
nm
light.
While
some
fraction
species
undergoes
photolysis,
vast
majority
occurs
reaction
OH
radicals,
total
exposures
corresponding
equivalent
up
10
d
atmospheric
oxidation.
For
all
burned,
large
rapid
changes
are
seen
in
ensemble
chemical
composition
BBOA,
as
measured
mass
spectrometer
(AMS).
Secondary
(SOA)
formation
for
experiments
continues
grow
increasing
exposure,
magnitude
SOA
highly
variable
between
experiments.
This
variability
can
be
explained
well
combination
differences
exposure
concentration
non-methane
(NMOGs)
before
oxidation,
PTR-ToF-MS
(r2
values
0.64
0.83).
From
this
relationship,
calculate
carbon
NMOGs
that
converted
function
time,
yields
ranging
24±4
%
after
6
h
56±9
4
d.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(3), P. 1531 - 1547
Published: Feb. 7, 2020
Abstract.
Relationships
between
various
optical,
physical,
and
chemical
properties
of
biomass-combustion-derived
particles
are
characterized
for
produced
in
the
laboratory
from
a
wide
range
fuels
burn
conditions.
The
modified
combustion
efficiency
(MCE),
commonly
used
to
parameterize
biomass
particle
emissions
properties,
is
shown
generally
have
weak
predictive
capabilities,
especially
more
efficient
There
is,
however,
strong
relationship
many
intensive
optical
(e.g.,
single-scatter
albedo,
Ångström
absorption
exponent,
mass
efficiency)
organic
aerosol-to-black
carbon
([OA]
∕
[BC])
ratio
over
wider
than
previously
considered
(0.3
105).
brown
(BrC,
i.e.,
light-absorbing
carbon)
also
vary
with
[OA]
[BC].
Coating-induced
enhancements
(i.e.,
“lensing”
effects)
contribute
only
minor
amount
BC
all
burns
despite
some
producing
having
large
ensemble-average
coating-to-core
ratios.
BC–OA
mixing
state
varies
strongly
[BC];
fraction
OA
that
internally
mixed
decreases
[BC]
while
relative
coated
on
increases.
In
contrast,
there
little
bulk
[BC],
O
:
C
H
atomic
ratios
abundance
key
marker
ion
(m/z=60,
linked
levoglucosan)
showing
no
dependence
both
nitrate
volatility
do
depend
Neither
total
nor
BC-specific
size
distributions
exhibit
any
clear
conditions
or
although
perhaps
fuel
type.
Overall,
our
results
expand
existing
knowledge
new
understanding
emitted
combustion.