Atmospheric chemistry and physics,
Journal Year:
2025,
Volume and Issue:
25(2), P. 959 - 977
Published: Jan. 27, 2025
Abstract.
Reports
on
the
composition
of
ultrafine
particles
(<100
nm
in
diameter)
Amazon
are
scarce,
due
part
to
fact
that
new-particle
formation
has
rarely
been
observed
near
ground
level.
Ultrafine
surface
have
nevertheless
observed,
leaving
open
questions
regarding
sources
and
chemistry
their
growth,
particularly
as
these
vary
across
seasons.
Here,
we
present
measurements
collected
Tapajós
National
Forest
(2.857°
S,
54.959°
W)
during
three
different
seasonal
periods:
10–30
September
2016
(SEP),
18
November–23
December
(DEC),
22
May–21
June
2017
(JUN).
Size-selected
(5–70
nm)
were
daily
(for
h
each
day)
using
an
offline
sampler.
Samples
time
periods
compiled
analyzed
liquid
chromatography
coupled
with
Orbitrap
high-resolution
mass
spectrometry.
Our
findings
suggest
a
sustained
influence
isoprene
organosulfate
from
periods.
We
chemical
evidence
indicates
biological-spore
fragmentation
impacted
ultrafine-particle
late
wet
season
(JUN),
while
markers
for
biomass
burning
secondary
peaked
dry
(SEP
DEC).
Higher
oxidation
states
degrees
unsaturation
organics
DEC),
suggesting
greater
extents
aerosol
aging.
Finally,
applying
volatility
parameterization
compounds
suggests
organic
sulfur
species
likely
key
drivers
growth
region
low
compared
other
species.
Proceedings of the National Academy of Sciences,
Journal Year:
2024,
Volume and Issue:
121(31)
Published: July 24, 2024
New
particle
formation
(NPF)
substantially
affects
the
global
radiation
balance
and
climate.
Iodic
acid
(IA)
is
a
key
marine
NPF
driver
that
recently
has
also
been
detected
inland.
However,
its
impact
on
continental
nucleation
remains
unclear.
Here,
we
provide
molecular-level
evidence
IA
greatly
facilitates
clustering
of
two
typical
land-based
nucleating
precursors:
dimethylamine
(DMA)
sulfuric
(SA),
thereby
enhancing
nucleation.
Incorporating
this
mechanism
into
an
atmospheric
chemical
transport
model,
show
IA-induced
enhancement
could
realize
increase
over
20%
in
SA–DMA
rate
iodine-rich
regions
China.
With
declining
anthropogenic
pollution
driven
by
carbon
neutrality
clean
air
policies
China,
enhance
rates
1.5
to
50
times
2060.
Our
results
demonstrate
overlooked
role
highlight
necessity
for
considering
synergistic
SA-IA-DMA
modeling
correct
representation
climatic
impacts
aerosols.
Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(8), P. 5477 - 5494
Published: April 26, 2022
Abstract.
We
evaluate
monoterpene-derived
peroxy
radical
(MT-RO2)
unimolecular
autoxidation
and
self-
cross-reactions
with
other
RO2
species
in
the
GEOS-Chem
global
chemical
transport
model.
The
formation
of
associated
highly
oxygenated
organic
molecules
(HOMs)
accretion
products
are
tracked
competition
bimolecular
reactions.
Autoxidation
is
dominant
fate
up
to
6–8
km
for
first-generation
MT-RO2,
which
can
undergo
H
shifts.
Reaction
NO
be
a
more
common
H-shift
rate
constants
<
0.1
s−1
or
at
altitudes
higher
than
8
due
imposed
Arrhenius
temperature
dependence
For
MT-derived
HOM-RO2,
generated
by
multistep
reaction
predicted
major
throughout
most
boreal
tropical
forest
regions,
whereas
dominates
temperate
subtropical
forests
Northern
Hemisphere.
newly
added
reactions
result
an
approximate
4
%
average
decrease
HO2
RO2,
mainly
faster
self-/cross-reactions
but
impact
upon
HO2,
OH,
NOx
abundances
only
important
planetary
boundary
layer
(PBL)
over
portions
forests.
Predicted
HOM
concentrations
MT-rich
regions
seasons
exceed
total
aerosol
standard
version
model
depending
on
parameters
used.
Comparisons
observations
reveal
that
large
uncertainties
remain
key
processes,
especially
respect
photochemical
lifetime
volatility
HOMs
as
well
rates
branching
products.
Further
laboratory
studies
related
MT-RO2-derived
gas-phase
product
kinetics
–
their
atmospheric
fate,
such
gas–particle
partitioning,
multiphase
chemistry,
net
secondary
needed.
Reviews of Modern Physics,
Journal Year:
2023,
Volume and Issue:
95(4)
Published: Nov. 9, 2023
Atmospheric
nanoparticles
can
serve
as
nuclei
for
cloud
droplets,
thereby
inducing
significant
but
uncertain
effects
on
the
radiative
forcing
of
climate
system.
This
article
focuses
physicochemical
processes
that
govern
growth
these
particles
from
formation
molecular
clusters
until
reach
sizes
where
they
act
condensation
nuclei.
The
review
describes
latest
developments
in
measurement
and
modeling
connects
domains
to
large-scale
simulations
such
Earth
system
models.
authors
recommend
closer
coordination
among
laboratory
studies,
atmospheric
measurements,
understand
importance
ACS Earth and Space Chemistry,
Journal Year:
2023,
Volume and Issue:
7(3), P. 653 - 660
Published: March 7, 2023
Aerosol
nucleation
accounts
for
over
half
of
all
seed
particles
cloud
droplet
formation.
In
the
atmosphere,
sulfuric
acid
(SA)
nucleates
with
ammonia,
amines,
oxidized
organics,
and
many
more
compounds
to
form
particles.
Studies
have
also
shown
that
methanesulfonic
(MSA)
independently
amines
ammonia.
MSA
SA
are
produced
simultaneously
via
dimethyl
sulfide
oxidation
in
marine
atmosphere.
However,
limited
knowledge
exists
on
how
nucleate
together
presence
various
atmospherically
relevant
base
compounds,
which
is
critical
predicting
rates
accurately.
This
work
provides
experimental
evidence
react
SA-MSA-base
has
different
reaction
pathways
than
SA-base
nucleation.
Specifically,
formation
SA-MSA
heterodimer
creates
energetically
favorable
SA-MSA-methylamine
an
enhancement
rates.
SA-trimethylamine
suppressed
by
MSA,
likely
due
steric
hindrance
trimethylamine.
These
results
display
importance
including
reactions
between
SA,
predict
particle
One Earth,
Journal Year:
2024,
Volume and Issue:
7(6), P. 1029 - 1043
Published: June 1, 2024
New
particle
formation
(NPF)
in
fire
smoke
is
thought
to
be
unlikely
due
large
condensation
and
coagulation
sinks
that
scavenge
molecular
clusters.
We
analyze
aircraft
measurements
over
the
Amazon
find
fires
significantly
enhance
NPF
ultrafine
(UFP
<
50
nm
diameter)
numbers
compared
background
conditions,
contrary
previous
understanding.
identify
nucleation
of
dimethylamine
with
sulfuric
acid,
which
aided
by
extremely
low
volatility
organics
biomass-burning
smoke,
can
overcome
explain
observations.
show
freshly
formed
clusters
rapidly
grow
UFP
sizes
through
secondary
organic
aerosol
formation,
leading
a
10-fold
increase
number
concentrations.
contrasting
effect
UFPs
on
deep
convective
clouds
larger
particles
from
primary
emissions
for
case
investigated
here.
intensify
precipitation
increased
condensational
heating,
while
delay
reduce
precipitation.
Journal of Geophysical Research Atmospheres,
Journal Year:
2023,
Volume and Issue:
128(3)
Published: Jan. 20, 2023
Abstract
The
processes
of
new
particle
formation
(NPF)
and
growth
are
important
contributors
to
cloud
condensation
nuclei
(CCN)
concentrations,
CCN
for
climate
from
their
impact
on
planetary
radiative
forcing.
While
the
general
ubiquity
importance
NPF
is
understood,
vertical
extent
governing
mechanisms
in
lower
troposphere
uncertain.
We
present
an
analysis
four
events
two
non‐NPF
during
HI‐SCALE
field
campaign
at
Southern
Great
Plains
observatory
Oklahoma,
USA.
First,
we
analyzed
airborne
ground‐based
observations
aerosol
gas‐phase
properties.
Second,
used
a
column
chemistry
microphysics
model
probe
factors
that
influence
profile
NPF.
During
HI‐SCALE,
found
several
instances
enhanced
occurring
hundred
meters
above
surface;
however,
spatio‐temporal
characteristics
observed
made
comparisons
between
airborne‐
difficult.
represented
(or
lack
NPF)
surface
final
diameters
within
10
nm.
predicted
rates
upper
mixed
layer,
this
enhancement
primarily
due
temperature
dependence
schemes,
but
was
also
dependent
precursors
measured
HI‐SCALE.
mixing
either
or
suppressed
rates,
number
surface.
Finally,
our
provides
insights
future
campaigns
modeling
efforts
investigating
National Science Review,
Journal Year:
2023,
Volume and Issue:
11(1)
Published: May 15, 2023
New
particle
formation
(NPF)
in
the
tropical
free
troposphere
(FT)
is
a
globally
important
source
of
cloud
condensation
nuclei,
affecting
properties
and
climate.
Oxidized
organic
molecules
(OOMs)
produced
from
biogenic
volatile
compounds
are
believed
to
contribute
aerosol
FT,
but
without
direct
chemical
observations.
We
performed
situ
molecular-level
OOMs
measurements
at
Bolivian
station
Chacaltaya
5240
m
above
sea
level,
on
western
edge
Amazonia.
For
first
time,
we
demonstrate
presence
OOMs,
mainly
with
4-5
carbon
atoms,
both
gas-phase
particle-phase
(in
terms
mass
contribution)
FT
air
These
observations,
combined
history
analyses,
indicate
that
observed
linked
isoprene
emitted
rainforests
hundreds
kilometers
away.
Based
measurements,
find
these
can
NPF,
least
growth
newly
formed
nanoparticles,
continental
scale.
Thus,
our
study
fundamental
significant
step
understanding
process
FT.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(13), P. 7297 - 7319
Published: July 4, 2023
Abstract.
Highly
oxygenated
organic
molecules
(HOMs)
play
a
pivotal
role
in
the
formation
of
secondary
aerosol
(SOA).
Therefore,
distribution
and
yields
HOMs
are
fundamental
to
understand
their
fate
chemical
evolution
atmosphere,
it
is
conducive
ultimately
assess
impact
SOA
on
air
quality
climate
change.
In
this
study,
gas-phase
formed
from
reaction
limonene
with
OH
radicals
photooxidation
were
investigated
SAPHIR
(Simulation
Atmospheric
PHotochemistry
large
Reaction
chamber),
using
time-of-flight
ionization
mass
spectrometer
nitrate
reagent
ion
(NO3--CIMS).
A
number
HOMs,
including
monomers
(C9–10)
dimers
(C17–20),
detected
classified
into
various
families.
Both
closed-shell
products
open-shell
peroxy
(RO2)
identified
under
low
NO
(0.06–0.1
ppb)
high
conditions
(17
ppb).
C10
most
abundant
HOM
account
for
over
80
%
total
HOMs.
Closed-shell
two
radical
family,
C10H15Ox⚫
(x=6–15)
C10H17Ox⚫
(x=6–15),
respective
termination
reactions
NO,
RO2,
HO2.
While
likely
by
addition
C10H16,
dominant
initial
step
plus
OH,
C10H15Ox⚫,
via
H
abstraction
OH.
related
contributed
41
42
at
demonstrating
that
H-abstraction
pathways
significant
Combining
theoretical
kinetic
calculations,
structure–activity
relationships
(SARs),
data
literature,
observed
RO2
intensities,
we
proposed
tentative
mechanisms
both
pathways.
We
further
estimated
molar
be
1.97-1.06+2.52
0.29-0.16+0.38
respectively.
Our
study
highlights
importance
provides
yield
oxidation
simulate
formation.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(15), P. 8789 - 8804
Published: Aug. 9, 2023
Abstract.
Sulfuric
acid
(SA)
is
a
governing
gaseous
precursor
for
atmospheric
new
particle
formation
(NPF),
major
source
of
global
ultrafine
particles,
in
environments
studied
around
the
world.
In
polluted
urban
atmospheres
with
high
condensation
sinks
(CSs),
stable
SA–amine
clusters,
such
as
SA–dimethylamine
(DMA)
usually
initializes
intense
NPF
events.
Coagulation
scavenging
and
cluster
evaporation
are
dominant
sink
processes
clusters
atmospheres,
yet
these
loss
not
quantitatively
included
present
parameterizations
nucleation.
We
herein
report
parameterization
SA–DMA
nucleation,
based
on
dynamic
simulations
quantum
chemistry
calculations,
certain
simplifications
to
greatly
reduce
computational
costs.
Compared
previous
nucleation
parameterizations,
this
was
able
reproduce
dependences
rates
temperature
CSs.
then
incorporated
it
three-dimensional
(3-D)
chemical
transport
model
simulate
evolution
number
size
distributions.
Simulation
results
showed
good
consistency
observations
occurrence
events
distributions
wintertime
Beijing
represented
significant
improvement
compared
that
using
without
coagulation
scavenging.
Quantitative
analysis
shows
contributes
significantly
aerosol
population
during
3-D
(>99
%
>60
%,
respectively).
These
broaden
understanding
stress
necessity
including
effects
stability
simulating
simulations.
Representing
thus
likely
improve
performance
apportionment
quantification
air
quality,
human
health,
climate.