Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(1), P. 61 - 83
Published: Jan. 3, 2023
Abstract.
Isoprene
and
monoterpene
emissions
to
the
atmosphere
are
generally
dominated
by
biogenic
sources.
The
oxidation
of
these
compounds
can
lead
production
secondary
organic
aerosol;
however
impact
this
chemistry
in
polluted
urban
settings
has
been
poorly
studied.
monoterpenes
form
aerosol
(SOA)
heterogeneously
via
anthropogenic–biogenic
interactions,
resulting
formation
organosulfate
(OS)
nitrooxy-organosulfate
(NOS)
species.
Delhi,
India,
is
one
most
cities
world,
but
little
known
about
volatile
(VOCs)
or
sources
SOA.
As
part
DELHI-FLUX
project,
gas-phase
mixing
ratios
isoprene
speciated
were
measured
during
pre-
post-monsoon
measurement
campaigns
central
Delhi.
Nocturnal
VOCs
substantially
higher
(isoprene:
(0.65±0.43)
ppbv;
limonene:
(0.59±0.11)
α-pinene:
(0.13±0.12)
ppbv)
than
pre-monsoon
(0.13±0.18)
0.011±0.025
(ppbv);
0.033±0.009)
period.
At
night,
concentrations
correlated
strongly
with
CO
Filter
samples
particulate
matter
less
2.5
µm
diameter
(PM2.5)
collected
OS
NOS
content
analysed
using
ultra-high-performance
liquid
chromatography
tandem
mass
spectrometry
(UHPLC-MS2).
Inorganic
sulfate
was
shown
facilitate
species
across
both
campaigns.
Sulfate
contained
within
contribute
significantly
signal
AMS.
Strong
nocturnal
enhancements
observed
total
concentration
contributed
an
average
(2.0±0.9)
%
(1.8±1.4)
oxidized
up
a
maximum
4.2
6.6
periods,
respectively.
Overall,
study
provides
first
molecular-level
measurements
SOA
derived
from
Delhi
demonstrates
that
anthropogenic
be
important
areas.
ACS Earth and Space Chemistry,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 26, 2025
The
nitrate
radical
(NO3)
oxidation
of
isoprene
is
an
important
contributor
to
secondary
organic
aerosol
(SOA).
Isoprene
has
two
double
bonds
which
allow
for
multigeneration
occur.
effects
chemistry
on
the
gas-
and
particle-phase
product
distributions
+
NO3
system
are
not
fully
understood.
In
this
study,
we
conduct
chamber
experiments
by
varying
ratio
N2O5
(precursor
NO3)
concentration
from
1:1
14:1
investigate
formation
products
in
both
phases
under
different
levels.
Multigeneration
leads
gas-phase
then
partition
into
particle
phase
depending
volatility;
first-generation
(15–36%
total
SOA)
such
as
C5H9NO5
C10H16N2O9
have
volatility
(log10C*
=
1.0–3.0
using
partitioning
method
log10C*
2.6–4.5
formula
method)
1–5
orders
magnitude
higher
than
second-generation
(37–57%
SOA,
−0.8–2.1
−3.7–1.8
C5H8,10N2O8,
C5H9N3O10,
C10H17N3O13.
fast
reaction
rate
constants
(estimated
be
order
10–13
cm3
molecules–1
s–1
at
295
K)
lower
result
increased
SOA
yields
when
availability
increases
enhanced.
Specifically,
increase
up
300%
yield
observed
N2O5/isoprene
3:1;
5.7%
(organic
mass
concentration,
ΔMo
4.2
μg/m3)
16.3%
(ΔMo
11.9
reacted
25
ppb
3.1%
1.2
12.4%
5.4
15
ppb.
maximum
occurs
greater
or
equal
3:1
a
combined
peroxy
radicals
(RO2)
fate.
We
encourage
future
studies
consider
factors,
can
vary
laboratory
ambient
conditions,
comparing
better
understand
any
differences
observed.
Our
results
highlight
that
updated
parameters
including
distribution
should
considered
enable
more
comprehensive
representation
prediction
atmospheric
models.
Accounts of Chemical Research,
Journal Year:
2020,
Volume and Issue:
53(8), P. 1415 - 1426
Published: July 10, 2020
ConspectusThe
complex
array
of
sources
and
transformations
organic
carbonaceous
material
that
comprises
an
important
fraction
atmospheric
fine
particle
mass,
known
as
aerosol,
has
presented
a
long
running
challenge
for
accurate
predictions
its
abundance,
distribution,
sensitivity
to
anthropogenic
activities.
Uncertainties
about
changes
in
aerosol
abundance
over
time
translate
uncertainties
their
impact
on
Earth's
climate
response
air
quality
policy.
One
limitation
our
understanding
been
lack
comprehensive
measurements
molecular
composition
volatility,
which
can
elucidate
processes
affecting
abundance.
Herein
we
describe
advances
the
development
application
Filter
Inlet
Gases
Aerosols
(FIGAERO)
coupled
field-deployable
High-Resolution
Time-of-Flight
Chemical
Ionization
Mass
Spectrometers
(HRToF-CIMS).
The
FIGAERO
HRToFCIMS
combination
broadly
probes
gas
particulate
OA
by
using
programmed
thermal
desorption
particles
collected
Teflon
filter
with
subsequent
detection
speciation
desorbed
vapors
inherently
quantitative
selected-ion
chemical
ionization.
provides
means
obtain
insights
into
volatility
components
thus
physicochemical
nature
will
govern
evolution
atmosphere.In
this
Account,
discuss
design
operation
FIGAERO,
when
HRToF-CIMS,
characterization
molecular-level
effective
laboratory
field.
We
provide
example
gleaned
from
deployment,
improve
evolution.
Specifically,
connect
profiles
equilibrium
saturation
vapor
concentration
enthalpy
vaporization
detected
components.
also
show
how
HRToF-CIMS
environmental
simulation
chamber
experiments
field
new
constraints
mechanisms
governing
secondary
formation
dynamic
associated
challenges
decomposition
during
calibration
both
axis
signal.
illustrate
additional
through
isothermal
evaporation
well
ultrafine
composition.
conclude
description
future
opportunities
needs
ability
further
science.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(14), P. 8421 - 8440
Published: July 17, 2020
Abstract.
The
formation
and
evolution
of
secondary
organic
aerosol
(SOA)
were
investigated
at
Yorkville,
GA,
in
late
summer
(mid-August
to
mid-October
2016).
(OA)
composition
was
measured
using
two
online
mass
spectrometry
instruments,
the
high-resolution
time-of-flight
spectrometer
(AMS)
Filter
Inlet
for
Gases
AEROsols
coupled
a
iodide-adduct
chemical
ionization
(FIGAERO-CIMS).
Through
analysis
speciated
organics
data
from
FIGAERO-CIMS
factorization
obtained
both
we
observed
notable
SOA
isoprene
monoterpenes
during
day
night.
Specifically,
addition
epoxydiol
(IEPOX)
uptake,
identified
non-IEPOX
pathways
nitrate
via
photooxidation
presence
NOx
radical
oxidation.
Monoterpenes
found
be
most
important
precursors
We
significant
contributions
highly
oxidized
acid-like
compounds
aged
OA
factor
FIGAERO-CIMS.
Taken
together,
our
results
showed
that
measurements
are
complementary
extensively
used
AMS
analysis,
together
they
provide
more
comprehensive
insights
into
sources
composition.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(5), P. 2878 - 2889
Published: Feb. 17, 2021
Nighttime
oxidation
of
biogenic
volatile
organic
compounds
(BVOCs)
by
nitrate
radicals
(NO3·)
represents
one
the
most
important
interactions
between
anthropogenic
and
natural
emissions,
leading
to
substantial
secondary
aerosol
(SOA)
formation.
The
direct
climatic
effect
such
SOA
cannot
be
quantified
because
its
optical
properties
atmospheric
fate
are
poorly
understood.
In
this
study,
we
generated
from
NO3·
a
series
BVOCs
including
isoprene,
monoterpenes,
sesquiterpenes.
were
subjected
comprehensive
online
offline
chemical
composition
analysis
using
high-resolution
mass
spectrometry
measurements
novel
broadband
(315–650
nm)
cavity-enhanced
spectrometer,
which
covers
wavelength
range
needed
understand
potential
contribution
radiative
forcing.
contained
significant
fraction
oxygenated
nitrates
(ONs),
consisting
monomers
oligomers
that
responsible
for
detected
light
absorption
in
315–400
nm
range.
created
β-pinene
α-humulene
was
further
photochemically
aged
an
flow
reactor.
has
photochemical
bleaching
lifetime
>6.2
h,
indicating
some
ONs
may
serve
as
atmosphere-stable
nitrogen
oxide
sinks
or
reservoirs
will
absorb
scatter
incoming
solar
radiation
during
daytime.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(17), P. 10125 - 10147
Published: Sept. 1, 2020
Abstract.
The
formation
of
organic
nitrates
(ONs)
in
the
gas
phase
and
their
impact
on
mass
secondary
aerosol
(SOA)
was
investigated
a
laboratory
study
for
α-pinene
β-pinene
photooxidation.
Focus
elucidation
those
mechanisms
that
cause
often
observed
suppression
SOA
by
NOx,
therein
role
highly
oxygenated
multifunctional
molecules
(HOMs).
We
with
increasing
NOx
concentration
(a)
portion
HOM
(HOM-ONs)
increased,
(b)
fraction
accretion
products
(HOM-ACCs)
decreased,
(c)
HOM-ACCs
contained
average
smaller
carbon
numbers.
Specifically,
we
(HOM-ONs),
arising
from
termination
reactions
peroxy
radicals
permutation
(HOM-PPs),
such
as
ketones,
alcohols,
or
hydroperoxides,
formed
other
reactions.
Effective
uptake
coefficients
γeff
HOMs
particles
were
determined.
more
than
six
O
atoms
efficiently
condensed
(γeff>0.5
average),
containing
eight
atoms,
every
collision
led
to
loss.
There
no
systematic
difference
HOM-ONs
HOM-PPs
same
radicals.
This
similarity
is
attributed
character
HOMs:
functional
groups
precursor
radical
are
identical,
vapor
pressures
should
not
strongly
depend
final
group.
As
consequence,
suppressing
effect
cannot
be
simply
explained
replacement
terminal
nitrate
groups.
According
all
will
contribute
bound
(OrgNO3)
particulate
phase.
However,
OrgNO3
stored
condensable
molecular
masses
>
230
Da
appeared
substantially
higher
spectrometry.
result
suggests
losses
particles,
probably
due
hydrolysis
releases
HNO3
into
but
leaves
behind
rest
loss
alone
could
explain
particle
β-pinene.
Instead
can
attribute
most
reduction
yields
significant
HOM-ACCs,
which
have
high
potentially
important
at
low-NOx
conditions.
Atmospheric chemistry and physics,
Journal Year:
2020,
Volume and Issue:
20(6), P. 3739 - 3776
Published: March 30, 2020
Abstract.
Ozone
is
a
greenhouse
gas
and
air
pollutant
that
harmful
to
human
health
plants.
During
the
summer
in
southeastern
US,
many
regional
global
models
are
biased
high
for
surface
ozone
compared
observations.
Past
studies
have
suggested
different
solutions
including
need
updates
model
representation
of
clouds,
chemistry,
deposition,
emissions
nitrogen
oxides
(NOx)
or
biogenic
hydrocarbons.
Here,
due
more
comprehensive
updated
isoprene
terpene
chemistry
added
into
CESM/CAM-chem
(Community
Earth
System
Model/Community
Atmosphere
Model
with
full
chemistry)
evaluate
impact
on
simulated
ozone.
Comparisons
results
data
collected
during
Studies
Emissions
Atmospheric
Composition,
Clouds
Climate
Coupling
by
Regional
Surveys
(SEAC4RS)
field
campaign
from
US
EPA
(Environmental
Protection
Agency)
CASTNET
(Clean
Air
Status
Trends
Network)
monitoring
stations
confirm
improves
ozone,
precursors,
NOx
reservoir
compounds.
The
reduce
bias
daily
maximum
8
h
average
(MDA8)
up
7
ppb.
In
past,
oxidation
particular
has
been
ignored
heavily
reduced
chemical
schemes
used
models,
this
study
demonstrates
needed
biases.
Sensitivity
tests
were
performed
order
lingering
uncertainties
Results
suggest
even
though
higher
than
remaining
similar
impacts
lower
oxidation.
Additionally,
identifies
further
constraints
aerosol
uptake
organic
nitrates
derived
terpenes
uncertainty
Although
greatly
CAM-chem,
large
remains.
Evaluation
against
SEAC4RS
suggests
future
improvements
horizontal
resolution
cloud
parameterizations
CAM-chem
may
be
particularly
important
reducing
bias.
Environmental Science & Technology Letters,
Journal Year:
2020,
Volume and Issue:
7(2), P. 60 - 69
Published: Jan. 13, 2020
Organic
aerosol
(OA)
is
a
complex
mixture
of
compounds
with
diverse
elemental
and
structural
features,
its
composition
affects
health
environmental
impacts.
A
detailed
speciation
the
functional
group
distribution
in
OA
important
for
constraining
atmospheric
reaction
pathways
products,
evaluating
chemical
mechanisms
models,
understanding
We
used
high-resolution
tandem
mass
spectrometry
to
perform
nontargeted
analysis
groups
from
three
ambient
sites
across
times
day
seasons.
observed
range
oxygen-,
nitrogen-,
and/or
sulfur-containing
groups,
including
oxygenates
such
as
hydroxyls
(29–69%)
carboxylic
acids
(19–59%),
that
dominated
may
participate
hydrogen
bonding
thus
impact
physical
properties
(percentages
indicate
average
ion
abundance
contributions
campaigns).
also
esters
(7–39%)
ethers
(13–42%)
suggest
importance
oligomerization.
On
average,
organonitrates
represented
only
12%
identified
nitrogen-containing
organosulfates
21%
while
we
many
other
nitrogen-
structures
were
contributors
(e.g.,
amines,
imines,
nitrophenols,
sulfides).
Most
(81%)
multifunctional
likely
multigenerational
oxidation
which
typically
contained
two
five
total.
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(23), P. 15658 - 15671
Published: Nov. 22, 2021
The
reactions
of
biogenic
volatile
organic
compounds
(BVOC)
with
the
nitrate
radicals
(NO3)
are
major
night-time
sources
nitrates
and
secondary
aerosols
(SOA)
in
regions
influenced
by
BVOC
anthropogenic
emissions.
In
this
study,
formation
gas-phase
highly
oxygenated
molecules-organic
(HOM-ON)
from
NO3-initiated
oxidation
a
representative
monoterpene,
β-pinene,
was
investigated
SAPHIR
chamber
(Simulation
Atmosphere
PHotochemistry
large
Reaction
chamber).
Six
monomer
(C
=
7–10,
N
1–2,
O
6–16)
five
accretion
product
17–20,
2–4,
9–22)
families
were
identified
further
classified
into
first-
or
second-generation
products
based
on
their
temporal
behavior.
time
lag
observed
peak
concentrations
between
peroxy
containing
odd
even
number
oxygen
atoms,
as
well
corresponding
termination
products,
provided
constraints
HOM-ON
mechanism.
can
be
explained
unimolecular
bimolecular
radicals.
A
dominant
portion
carbonylnitrates
detected,
highlighting
significance
intramolecular
H-shift
for
HOM-ON.
mean
molar
yield
estimated
to
4.8%
(−2.6%/+5.6%),
suggesting
significant
contributions
SOA
formation.
Atmospheric chemistry and physics,
Journal Year:
2021,
Volume and Issue:
21(12), P. 9681 - 9704
Published: June 29, 2021
Abstract.
Highly
oxygenated
organic
molecules
(HOM)
are
found
to
play
an
important
role
in
the
formation
and
growth
of
secondary
aerosol
(SOA).
SOA
is
type
with
significant
impact
on
air
quality
climate.
Compared
oxidation
volatile
compounds
by
ozone
(O3)
hydroxyl
radical
(OH),
HOM
nitrate
(NO3),
oxidant
at
nighttime
dawn,
has
received
less
attention.
In
this
study,
reaction
isoprene
NO3
was
investigated
SAPHIR
chamber
(Simulation
Atmospheric
PHotochemistry
a
large
Reaction
chamber).
A
number
HOM,
including
monomers
(C5),
dimers
(C10),
trimers
(C15),
both
closed-shell
open-shell
peroxy
radicals
(RO2),
were
identified
classified
into
various
series
according
their
formula.
Their
pathways
proposed
based
observed
known
mechanisms
literature,
which
further
constrained
time
profiles
after
sequential
addition
differentiate
first-
second-generation
products.
containing
one
three
N
atoms
(1–3N-monomers)
formed,
starting
carbon
double
bond,
forming
radicals,
followed
autoxidation.
1N-monomers
formed
direct
first-generation
2N-monomers
(e.g.,
C5H8N2On(n=7–13),
C5H10N2On(n=8–14))
likely
termination
products
C5H9N2On⚫,
C5-hydroxynitrate
(C5H9NO4),
product
bond.
2N-monomers,
products,
dominated
accounted
for
∼34
%
all
indicating
+
under
our
experimental
conditions.
H
shift
alkoxy
form
subsequent
autoxidation
(“alkoxy–peroxy”
pathway)
be
pathway
formation.
mostly
accretion
monomer
RO2
via
reactions
dimer
possibly
C5–RO2
isoprene.
RO2.
The
concentrations
different
showed
distinct
during
reaction,
linked
pathway.
either
typical
profile
or
combination
both,
multiple
and/or
isomers.
Total
molar
yield
estimated
1.2
%-0.7%+1.3%,
corresponded
∼3.6
assuming
molecular
weight
C5H9NO6
as
lower
limit.
This
suggests
that
may
contribute
fraction
NO3.