Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(24), P. 10664 - 10674
Published: June 8, 2024
New
particle
formation
(NPF)
is
a
major
source
of
atmospheric
aerosol
particles,
including
cloud
condensation
nuclei
(CCN),
by
number
globally.
Previous
research
has
highlighted
that
NPF
less
frequent
but
more
intense
at
roadsides
compared
to
urban
background.
Here,
we
closely
examine
both
background
and
roadside
sites
in
Central
Europe.
We
show
the
concentration
oxygenated
organic
molecules
(OOMs)
greater
roadside,
OOMs
along
with
sulfuric
acid
onto
new
particles
sufficient
explain
growth
sites.
identify
hitherto
unreported
traffic-related
OOM
contributing
29%
16%
total
background,
respectively.
Critically,
this
undiscovered
an
essential
component
NPF.
Without
their
contribution
rates
subsequent
enhancements
survival,
>50
nm
produced
would
be
reduced
factor
21
site.
Reductions
hydrocarbon
emissions
from
road
traffic
may
thereby
reduce
numbers
CCN
counts.
Chemical Reviews,
Journal Year:
2023,
Volume and Issue:
123(4), P. 1635 - 1679
Published: Jan. 11, 2023
Organic
peroxides
(POs)
are
organic
molecules
with
one
or
more
peroxide
(−O–O−)
functional
groups.
POs
commonly
regarded
as
chemically
labile
termination
products
from
gas-phase
radical
chemistry
and
therefore
serve
temporary
reservoirs
for
oxidative
radicals
(HOx
ROx)
in
the
atmosphere.
Owing
to
their
ubiquity,
active
gas-particle
partitioning
behavior,
reactivity,
key
reactive
intermediates
atmospheric
multiphase
processes
determining
life
cycle
(formation,
growth,
aging),
climate,
health
impacts
of
aerosol.
However,
there
remain
substantial
gaps
origin,
molecular
diversity,
fate
due
complex
nature
dynamic
behavior.
Here,
we
summarize
current
understanding
on
POs,
a
focus
identification
quantification,
state-of-the-art
analytical
developments,
molecular-level
formation
mechanisms,
chemical
transformation
pathways,
well
environmental
impacts.
We
find
that
interactions
SO2
transition
metal
ions
generally
fast
PO
pathways
liquid
water,
lifetimes
estimated
be
minutes
hours,
while
hydrolysis
is
particularly
important
α-substituted
hydroperoxides.
Meanwhile,
photolysis
thermolysis
likely
minor
sinks
POs.
These
distinctly
different
fates,
such
reaction
OH
radicals,
which
highlights
need
understand
By
summarizing
advances
remaining
challenges
investigation
propose
future
research
priorities
regarding
fate,
Environmental Science & Technology,
Journal Year:
2020,
Volume and Issue:
54(13), P. 7911 - 7921
Published: June 9, 2020
To
better
understand
the
role
of
aromatic
hydrocarbons
in
new-particle
formation,
we
measured
particle-phase
abundance
and
volatility
oxidation
products
following
reaction
with
OH
radicals.
For
this
used
thermal
desorption
an
iodide-adduct
Time-of-Flight
Chemical-Ionization
Mass
Spectrometer
equipped
a
Filter
Inlet
for
Gases
AEROsols
(FIGAERO-ToF-CIMS).
The
measurements
confirm
that
toluene
naphthalene
can
contribute
to
initial
growth
newly
formed
particles.
Toluene-derived
(C7)
have
similar
distribution
α-pinene-derived
(C10)
products,
while
naphthalene-derived
are
much
less
volatile
than
those
from
or
α-pinene;
they
thus
stronger
contributors
growth.
Rapid
progression
through
multiple
generations
is
more
pronounced
α-pinene,
resulting
but
also
favoring
functional
groups
lower
per
added
oxygen
atom,
such
as
hydroxyl
carboxylic
instead
hydroperoxide
groups.
Under
conditions
typical
polluted
urban
settings,
may
well
nucleation
smallest
particles,
whereas
abundant
alkyl
benzenes
overtake
once
particles
grown
beyond
point
where
Kelvin
effect
strongly
influences
condensation
driving
force.
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:
2020,
Volume and Issue:
20(2), P. 649 - 669
Published: Jan. 20, 2020
Abstract.
Secondary
organic
aerosol
(SOA)
forms
a
major
part
of
the
tropospheric
submicron
aerosol.
Still,
exact
formation
mechanisms
SOA
have
remained
elusive.
Recently,
newly
discovered
group
oxidation
products
volatile
compounds
(VOCs),
highly
oxygenated
molecules
(HOMs),
been
proposed
to
be
responsible
for
large
fraction
formation.
To
assess
potential
HOMs
form
and
even
take
in
new
particle
formation,
knowledge
their
volatilities
is
essential.
However,
due
exotic,
partially
unknown,
structures,
estimating
volatility
challenging.
In
this
study,
we
performed
set
continuous
flow
chamber
experiments,
supported
by
box
modelling,
study
HOMs,
along
with
some
less
compounds,
formed
ozonolysis
α-pinene,
an
abundant
VOC
emitted
boreal
forests.
Along
gaseous
precursors,
periodically
injected
inorganic
seed
into
vary
condensation
sink
(CS)
low-volatility
vapours.
We
monitored
decrease
gas
phase
response
increasing
CS,
were
able
relate
responses
compounds.
found
that
HOM
monomers
are
mainly
low
volatility,
small
being
semi-volatile.
dimers
all
at
least
but
probably
extremely
volatility;
however,
our
method
not
directly
distinguish
between
two.
model
terms
carbon,
hydrogen,
oxygen
nitrogen
numbers.
levels
oxygenation
correspond
lower
volatilities,
as
expected,
steep
than
would
expected
based
on
many
existing
models
such
SIMPOL.
The
hydrogen
number
compound
also
predicted
its
independently
carbon
number,
higher
numbers
corresponding
volatilities.
This
can
explained
functional
groups
making
up
molecule:
high
associated
with,
e.g.
hydroxy
groups,
which
more
than,
carbonyls,
number.
presented
should
applicable
systems
other
α-pinene
ozonolysis,
different
loadings,
order
ranges.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(15), P. 9563 - 9579
Published: Aug. 14, 2020
Abstract.
Gas-phase
oxidation
pathways
and
products
of
anthropogenic
volatile
organic
compounds
(VOCs),
mainly
aromatics,
are
the
subject
intensive
research,
with
attention
paid
to
their
contributions
secondary
aerosol
(SOA)
formation
potentially
new
particle
(NPF)
in
urban
atmosphere.
In
this
study,
a
series
OH-initiated
experiments
trimethylbenzene
(TMB,
C9H12)
including
1,2,4-TMB,
1,3,5-TMB,
1,2,3-TMB,
1,2,4-(methyl-D3)-TMBs
(C9H9D3)
were
investigated
an
flow
reactor
(OFR)
absence
presence
NOx.
Products
measured
using
suite
state-of-the-art
instruments,
i.e.
nitrate-based
chemical
ionization–atmospheric
pressure
interface
time-of-flight
mass
spectrometer
(nitrate
CI-APi-TOF),
iodide-adduct
ionization
(iodide
CI-TOF)
equipped
Filter
Inlet
for
Gases
AEROsols
(FIGAERO),
Vocus
proton-transfer-reaction
(Vocus
PTR).
A
large
number
C9
1–11
oxygen
atoms
C18
presumably
formed
from
dimerization
peroxy
radicals
observed,
hinting
at
extensive
existence
autoxidation
accretion
reaction
reactions
TMBs.
Oxidation
deuterium
different
methyl
substituents
then
used
as
molecular
basis
propose
potential
pathways.
Accretion
is
most
significant
aromatics
meta-substituents
least
ortho-substituents
if
size
substituted
groups
identical.
The
NOx
would
suppress
highly
oxygenated
molecules
(HOMs)
enhance
organonitrates
even
dinitrate
compounds.
Our
results
show
that
TMB
much
more
diverse
could
be
than
current
mechanisms
predict.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(20), P. 13646 - 13656
Published: Sept. 29, 2021
Gas-phase
oxygenated
organic
molecules
(OOMs)
can
contribute
substantially
to
the
growth
of
newly
formed
particles.
However,
characteristics
OOMs
and
their
contributions
particle
rate
are
not
well
understood
in
urban
areas,
which
have
complex
anthropogenic
emissions
atmospheric
conditions.
We
performed
long-term
measurement
gas-phase
Beijing
during
2018–2019
using
nitrate-based
chemical
ionization
mass
spectrometry.
OOM
concentrations
showed
clear
seasonal
variations,
with
highest
summer
lowest
winter.
Correspondingly,
calculated
rates
due
condensation
were
summer,
followed
by
spring,
autumn,
One
prominent
feature
this
environment
was
a
high
fraction
(∼75%)
nitrogen-containing
OOMs.
These
contributed
only
50–60%
total
led
condensation,
owing
slightly
higher
volatility
than
non-nitrate
By
comparing
observed
rates,
we
that
sulfuric
acid
its
clusters
main
contributors
sub-3
nm
particles,
significantly
promoting
3–25
In
wintertime
Beijing,
however,
there
missing
particles
above
3
nm,
remain
be
further
investigated.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(14), P. 8511 - 8532
Published: July 22, 2020
Abstract.
Particles
in
smoke
emitted
from
biomass
combustion
have
a
large
impact
on
global
climate
and
urban
air
quality.
There
is
limited
understanding
of
how
particle
optical
properties
–
especially
the
contributions
black
carbon
(BC)
brown
(BrC)
evolve
with
photochemical
aging
smoke.
We
analyze
evolution
chemical
composition
particles
produced
wide
variety
fuels,
largely
western
United
States.
The
photochemically
aged
reaction
chamber
over
atmospheric-equivalent
timescales
ranging
0.25
to
8
d.
Various
aerosol
(e.g.,
single-scatter
albedo,
wavelength
dependence
absorption,
BC
mass
absorption
coefficient,
MACBC)
evolved
aging,
specific
dependent
initial
conditions.
coatings
(the
so-called
lensing
effect)
was
small,
even
after
aging.
BrC
absorptivity
(MACBrC)
varied
between
individual
burns
but
decreased
consistently
at
longer
times;
generally
increased
observed
changes
result
combination
secondary
organic
(SOA)
production
heterogeneous
oxidation
primary
OA
mass,
SOA
being
major
driver
changes.
time,
reflecting
both
formation
precursors
having
range
lifetimes
respect
OH
evolving
environment
within
chamber.
Although
decreases
dilution-corrected
may
actually
increase
SOA.
These
experimental
results
provide
context
for
interpretation
ambient
observations
biomass-combustion-derived
plumes.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(16), P. 9783 - 9803
Published: Aug. 21, 2020
Abstract.
Aromatic
volatile
organic
compounds
(VOCs)
are
key
anthropogenic
pollutants
emitted
to
the
atmosphere
and
important
for
both
ozone
secondary
aerosol
(SOA)
formation
in
urban
areas.
Recent
studies
have
indicated
that
aromatic
hydrocarbons
may
follow
previously
unknown
oxidation
chemistry
pathways,
including
autoxidation
can
lead
of
highly
oxidised
products.
In
this
study
we
evaluate
gas-
particle-phase
ions
measured
by
online
mass
spectrometry
during
hydroxyl
radical
substituted
C9-aromatic
isomers
(1,3,5-trimethylbenzene,
1,2,4-trimethylbenzene,
propylbenzene
isopropylbenzene)
a
polyaromatic
hydrocarbon
(1-methylnaphthalene)
under
low-
medium-NOx
conditions.
A
time-of-flight
chemical
ionisation
spectrometer
(ToF-CIMS)
with
iodide–anion
was
used
filter
inlet
gases
aerosols
(FIGAERO)
detection
products
particle
phase,
while
Vocus
proton-transfer-reaction
(Vocus-PTR-MS)
gas
phase.
The
signal
product
observed
spectra
were
compared
different
precursors
experimental
majority
spectral
phases
comes
from
which
common
all
precursors,
though
distributions
distinct
VOCs.
Gas-
composition
one
another.
Ions
corresponding
contained
near-explicit
phase
Master
Chemical
Mechanism
(MCM
version
3.3.1)
utilised
as
benchmark
current
scientific
understanding,
comparison
these
observations
shows
MCM
is
missing
range
its
mechanism.
bulk
ring
scission
ions,
large
proportion
more
than
reported
undergone
further
form
oxygenated
molecules
(HOMs).
Under
perturbation
OH
increased
NOx,
contribution
HOM-ion
signals
remains
elevated
precursors.
Up
43
%
ring-retaining
HOMs;
most
aromatics.
Unique
minor
component
systems,
many
dominant
ion
formulae
concurrent
other
highlighting
challenges
utilising
marker
SOA.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(13), P. 8592 - 8603
Published: June 17, 2021
Photooxidation
of
volatile
organic
compounds
(VOCs)
produces
secondary
aerosol
(SOA)
and
light-absorbing
brown
carbon
(BrC)
via
multiple
reaction
steps/pathways,
reflecting
significant
chemical
complexity
relevant
to
gaseous
oxidation
subsequent
gas-to-particle
conversion.
Toluene
is
an
important
VOC
under
urban
conditions,
but
the
fundamental
mechanism
leading
SOA
formation
remains
uncertain.
Here,
we
elucidate
multigeneration
production
from
toluene
by
simultaneously
tracking
evolutions
gas-phase
in
a
chamber.
Large
size
increase
browning
monodisperse
sub-micrometer
seed
particles
occur
shortly
after
initiating
hydroxyl
radical
(OH)
at
10–90%
relative
humidity
(RH).
The
evolution
products
properties
(size/density/optical
properties)
speciation
aerosol-phase
indicate
that
growth
result
earlier
generation
consisting
dominantly
dicarbonyl
carboxylic
functional
groups.
While
dicarbonyls
engage
aqueous
reactions
yield
nonvolatile
oligomers
nitrogen
heterocycles/heterochains
(in
presence
NH3)
high
RH,
acids
contribute
carboxylates
ionic
dissociation
or
acid–base
wide
RH
range.
We
conclude
contributes
importantly
SOA/BrC
because
their
prompt
yields
photooxidation
unique
functionalities
for
participation
reactions.