Environmental Science & Technology,
Journal Year:
2013,
Volume and Issue:
47(6), P. 2998 - 3005
Published: Feb. 18, 2013
Air
pollutants
from
residential
solid
fuel
combustion
are
attracting
growing
public
concern.
Field
measured
emission
factors
(EFs)
of
various
air
for
fuels
close
to
the
reality
and
urgently
needed
better
estimations.
In
this
study,
particulate
matter
(PM),
organic
carbon
(OC),
elemental
(EC),
polycyclic
aromatic
hydrocarbons
(PAHs)
combustions
coal
briquette,
cake,
wood
were
in
rural
Heshun
County,
China.
The
EFs
PM,
OC,
EC
8.1-8.5,
2.2-3.6,
0.91-1.6
g/kg
burnt
a
simple
metal
stove,
0.54-0.64,
0.13-0.14,
0.040-0.0041
briquette
burned
an
improved
stove
with
chimney,
3.2-8.5,
0.38-0.58,
0.022-0.052
homemade
cake
combusted
brick
flue,
respectively.
28
parent
PAHs,
4
oxygenated
9
nitro-PAHs
182-297,
7.8-10,
0.14-0.55
mg/kg
wood,
14-16,
1.7-2.6,
0.64-0.83
168-223,
4.7-9.5,
0.16-2.4
Emissions
much
higher
than
those
especially
true
high
molecular
weight
PAHs.
Most
field
under
laboratory
conditions.
Atmospheric chemistry and physics,
Journal Year:
2011,
Volume and Issue:
11(9), P. 4039 - 4072
Published: May 3, 2011
Abstract.
Biomass
burning
(BB)
is
the
second
largest
source
of
trace
gases
and
primary
fine
carbonaceous
particles
in
global
troposphere.
Many
recent
BB
studies
have
provided
new
emission
factor
(EF)
measurements.
This
especially
true
for
non-methane
organic
compounds
(NMOC),
which
influence
secondary
aerosol
(SOA)
ozone
formation.
New
EF
should
improve
regional
to
emissions
estimates
therefore,
input
atmospheric
models.
In
this
work
we
present
an
up-to-date,
comprehensive
tabulation
known
pyrogenic
species
based
on
measurements
made
smoke
that
has
cooled
ambient
temperature,
but
not
yet
undergone
significant
photochemical
processing.
All
EFs
are
converted
one
standard
form
(g
compound
emitted
per
kg
dry
biomass
burned)
using
carbon
mass
balance
method
they
categorized
into
14
fuel
or
vegetation
types.
terminology
defined
promote
consistency.
We
compile
a
large
number
consumption
unit
area
important
fire
types
summarize
several
by
major
burning.
Post
processes
discussed
provide
context
concept
within
overall
chemistry
also
highlight
potential
rapid
changes
relative
scale
some
models
remote
sensing
products.
Recent
shows
individual
fires
emit
significantly
more
gas-phase
NMOC
than
previously
thought
including
additional
can
model
performance.
A
detailed
estimate
suggests
emits
at
least
400
Tg
yr−1
NMOC,
almost
3
times
larger
most
previous
estimates.
Selected
results
(e.g.
HONO
tracers
HCN
CH3CN)
highlighted
key
areas
requiring
future
research
briefly
discussed.
The Science of The Total Environment,
Journal Year:
2016,
Volume and Issue:
579, P. 1000 - 1034
Published: Nov. 29, 2016
Biomass
burning
(BB)
is
a
significant
air
pollution
source,
with
global,
regional
and
local
impacts
on
quality,
public
health
climate.
Worldwide
an
extensive
range
of
studies
has
been
conducted
almost
all
the
aspects
BB,
including
its
specific
types,
quantification
emissions
assessing
various
impacts.
China
one
countries
where
significance
BB
recognized,
lot
research
efforts
devoted
to
investigate
it,
however,
so
far
no
systematic
reviews
were
synthesize
information
which
emerging.
Therefore
aim
this
work
was
comprehensively
review
most
published
topic
in
China,
literature
concerning
field
measurements,
laboratory
indoors
outdoors
China.
In
addition,
provides
insights
into
role
wildfire
anthropogenic
quality
globally.
Further,
we
attempted
provide
basis
for
formulation
policies
regulations
by
policy
makers
Atmospheric chemistry and physics,
Journal Year:
2011,
Volume and Issue:
11(23), P. 12049 - 12064
Published: Dec. 5, 2011
Abstract.
Biomass
burning
(BB)
is
a
large
source
of
primary
and
secondary
organic
aerosols
(POA
SOA).
This
study
addresses
the
physical
chemical
evolution
BB
aerosols.
Firstly,
lifetime
POA
SOA
signatures
observed
with
Aerodyne
Aerosol
Mass
Spectrometer
are
investigated,
focusing
on
measurements
at
high-latitudes
acquired
during
2008
NASA
ARCTAS
mission,
in
comparison
to
data
from
other
field
studies
laboratory
aging
experiments.
The
parameter
f60,
ratio
integrated
signal
m/z
60
total
component
mass
spectrum,
used
as
marker
rate
oxidation
fate
POA.
A
background
level
f60~0.3%
±
0.06%
for
SOA-dominated
ambient
OA
shown
be
an
appropriate
this
tracer.
Using
also
f44
tracer
aged
surrogate
O:C,
novel
graphical
method
presented
characterise
plumes.
Similar
trends
decreasing
f60
increasing
most
lab
studies.
At
least
some
very
plumes
retain
clear
signature.
statistically
significant
difference
between
highly-oxygenated
non-BB
origin
using
tracer,
consistent
substantial
contribution
BBOA
springtime
Arctic
aerosol
burden
2008.
Secondly,
summary
results
net
enhancement
plumes,
which
shows
variability.
estimates
gain
range
ΔOA/ΔCO(mass)
=
−0.01
~0.05,
mean
ΔOA/POA
~19%.
With
these
ratios
global
inventories
CO
due
~8
7
Tg
yr−1
estimated,
order
5
%
recent
estimates.
Further
following
plume
advection
should
focus
future
research
better
constrain
potentially
important
burden.
Atmospheric chemistry and physics,
Journal Year:
2012,
Volume and Issue:
12(2), P. 615 - 634
Published: Jan. 16, 2012
Abstract.
We
discuss
the
use
of
a
two-dimensional
volatility-oxidation
space
(2-D-VBS)
to
describe
organic-aerosol
chemical
evolution.
The
is
built
around
two
coordinates,
volatility
and
degree
oxidation,
both
which
can
be
constrained
observationally
or
specified
for
known
molecules.
Earlier
work
presented
thermodynamics
organics
forming
foundation
this
2-D-VBS,
allowing
us
define
average
composition
(C,
H,
O)
organics,
including
organic
aerosol
(OA)
based
on
oxidation
state.
Here
we
how
analyze
experimental
data,
using
2-D-VBS
gain
fundamental
insight
into
chemistry.
first
present
well-understood
"traditional"
secondary
(SOA)
system
–
SOA
from
α-pinene
+
ozone,
then
turn
examples
"non-traditional"
formation
wood
smoke
dilute
diesel-engine
emissions.
Finally,
broader
implications
analysis.
Atmospheric chemistry and physics,
Journal Year:
2010,
Volume and Issue:
10(13), P. 6363 - 6370
Published: July 13, 2010
Abstract.
We
report
the
direct
observation
of
laboratory
production
spherical,
carbonaceous
particles
–
"tar
balls"
from
smoldering
combustion
two
commonly
occurring
dry
mid-latitude
fuels.
Real-time
measurements
spectrally
varying
absorption
Ångström
coefficients
(AAC)
indicate
that
a
class
light
absorbing
organic
carbon
(OC)
with
wavelength
dependent
imaginary
part
its
refractive
index
optically
defined
as
"brown
carbon"
is
an
important
component
tar
balls.
The
spectrum
parts
their
complex
indices
can
be
described
Lorentzian-like
model
effective
resonance
in
ultraviolet
(UV)
spectral
region.
Sensitivity
calculations
for
aerosols
containing
traditional
OC
(no
at
visible
and
UV
wavelengths)
brown
suggest
accounting
near-UV
by
leads
to
increase
aerosol
radiative
forcing
efficiency
increased
absorption.
Since
account
nearly
three-fourths
total
mass
emitted
globally,
inclusion
optical
properties
balls
into
models
has
significance
Earth's
radiation
budget,
remote
sensing,
understanding
anomalous
troposphere.