Atmospheric chemistry and physics,
Journal Year:
2022,
Volume and Issue:
22(1), P. 505 - 533
Published: Jan. 13, 2022
Abstract.
We
present
here
the
results
obtained
during
an
intensive
field
campaign
conducted
in
framework
of
French
“BIO-MAÏDO”
(Bio-physico-chemistry
tropical
clouds
at
Maïdo
(Réunion
Island):
processes
and
impacts
on
secondary
organic
aerosols'
formation)
project.
This
study
integrates
exhaustive
chemical
microphysical
characterization
cloud
water
March–April
2019
Réunion
(Indian
Ocean).
Fourteen
samples
have
been
collected
along
slope
this
mountainous
island.
Comprehensive
these
is
performed,
including
inorganic
ions,
metals,
oxidants,
matter
(organic
acids,
sugars,
amino
carbonyls,
low-solubility
volatile
compounds,
VOCs).
Cloud
presents
high
molecular
complexity
with
elevated
water-soluble
content
partly
modulated
by
properties.
As
expected,
our
findings
show
presence
compounds
marine
origin
(e.g.
chloride,
sodium)
demonstrating
ocean–cloud
exchanges.
Indeed,
Na+
Cl−
dominate
composition
contributing
to
30
%
27
%,
respectively,
average
total
ion
content.
The
strong
correlations
between
species
(r2
=
0.87,
p
value:
<
0.0001)
suggest
similar
air
mass
origins.
However,
molar
Cl-/Na+
ratio
(0.85)
lower
than
sea-salt
one,
reflecting
a
chloride
depletion
possibly
associated
acids
such
as
HNO3
H2SO4.
Additionally,
non-sea-salt
fraction
sulfate
varies
38
91
indicating
other
sources.
Also,
for
first
time
waters
sugars
clearly
indicates
that
biological
activities
contribute
composition.
A
significant
variability
events
observed
dissolved
(25.5
±
18.4
mg
C
L−1),
levels
reaching
up
62
L−1.
was
not
all
measured
suggesting
dissimilar
emission
sources
or
production
mechanisms.
For
that,
statistical
analysis
performed
based
back-trajectory
calculations
using
CAT
(Computing
Atmospheric
Trajectory
Tool)
model
land
cover
registry.
These
investigations
reveal
origins
variables
do
fully
explain
composition,
highlighting
sources,
multiphasic
transfer,
processing
clouds.
Even
though
minor
contribution
VOCs
(oxygenated
VOCs)
carbon
(DOC)
(0.62
0.06
respectively)
has
observed,
biogenic
VOC
(20
180
nmol
L−1)
were
detected
aqueous
phase,
cloud-terrestrial
vegetation
exchange.
scavenging
assessed
measurements
both
gas
phases
deduced
experimental
gas-/aqueous-phase
partitioning
compared
Henry's
law
equilibrium
evaluate
potential
supersaturation
unsaturation
conditions.
evaluation
reveals
from
natural
anthropogenic
Our
depict
even
higher
terpenoids,
evidencing
deviation
thermodynamically
expected
aqueous-phase
chemistry
highly
impacted
area.
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:
2024,
Volume and Issue:
58(2), P. 1236 - 1243
Published: Jan. 3, 2024
Aqueous-phase
reactions
of
α-dicarbonyls
with
amines
or
ammonium
have
been
identified
as
important
sources
secondary
brown
carbon
(BrC).
However,
the
kinetics
BrC
formation
and
effects
pH
are
still
not
very
clear.
In
this
study,
by
aqueous
(glyoxal
methylglyoxal)
ammonium,
amino
acids,
alkylamines
in
bulk
solution
at
different
values
investigated.
Our
results
reveal
pH-parameterized
production
rate
constants,
kBrCII
(m–1
[M]−2
s–1),
based
on
light
absorption
between
300
500
nm:
log10(kBrCII)
=
(1.0
±
0.1)
×
–
(7.4
1.0)
for
glyoxal
(6.3
0.9)
methylglyoxal.
The
linear
slopes
closing
to
1.0
indicate
that
is
governed
nitrogen
nucleophilic
addition
pathway.
Consequently,
absorptivities
produced
increase
exponentially
pH.
from
methylglyoxal
higher
(≥6.5)
exhibits
optical
properties
comparable
biomass
burning
coal
combustion,
categorized
"weakly"
absorbing
BrC,
while
lower
(<6.0)
(pH
5.0–7.0)
falls
into
"very
weakly"
BrC.
pH-dependent
feature
significantly
affects
solar
ability
thus
atmospheric
photochemical
processes,
e.g.,
7.0
absorbs
14–16
times
more
power
compared
5.0,
which
turn
could
lead
a
decrease
1
order
magnitude
photolysis
constants
O3
NO2.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(12), P. 7771 - 7778
Published: May 24, 2022
There
is
a
large
gap
between
the
simulated
and
observed
sulfate
concentrations
during
winter
haze
events
in
North
China.
Although
multiphase
formation
mechanisms
have
been
proposed,
they
not
evaluated
using
chemical
transport
models.
In
this
study,
Weather
Research
Forecasting
model
coupled
with
Chemistry
(WRF-Chem)
was
used
to
apportion
formation.
It
found
that
Mn-catalyzed
oxidation
on
aerosol
surfaces
dominant
pathway,
accounting
for
92.3
±
3.5%
of
events.
Gas-phase
contributed
3.1
0.5%
due
low
OH
levels.
The
H2O2
water
accounted
4.2
3.6%
formation,
caused
by
rapid
consumption
H2O2.
contributions
O3,
NO2
oxidation,
transition
metal
ion-catalyzed
reactions
could
be
negligible
owing
content,
pH,
high
ionic
strength.
from
in-cloud
were
barrier
provided
stable
stratification
ACS Environmental Au,
Journal Year:
2022,
Volume and Issue:
2(4), P. 336 - 345
Published: April 29, 2022
Reactive
oxygen
species
(ROS)
play
a
critical
role
in
the
chemical
transformation
of
atmospheric
secondary
organic
aerosols
(SOA)
and
aerosol
health
effects
by
causing
oxidative
stress
vivo.
Acidity
is
an
important
physicochemical
property
aerosols,
but
its
on
ROS
formation
from
SOA
have
been
poorly
characterized.
By
applying
electron
paramagnetic
resonance
spin-trapping
technique
Diogenes
chemiluminescence
assay,
we
find
highly
distinct
radical
yields
composition
at
different
pH
values
range
1–7.4
generated
oxidation
isoprene,
α-terpineol,
α-pinene,
β-pinene,
toluene,
naphthalene.
We
observe
that
isoprene
has
substantial
hydroxyl
(•OH)
neutral
pH,
which
are
1.5–2
times
higher
compared
to
acidic
conditions
total
yields.
Superoxide
(O2•–)
found
be
dominant
all
types
SOAs
lower
pH.
At
α-terpineol
exhibits
yield
carbon-centered
radicals,
while
no
observed
aromatic
SOA.
Further
experiments
with
model
compounds
show
decomposition
peroxide
leading
may
suppressed
due
acid-catalyzed
rearrangement
peroxides.
also
1.5–3
molar
hydrogen
(H2O2)
biogenic
SOA,
likely
enhanced
α-hydroxyhydroperoxides
quinone
redox
cycling,
respectively.
These
findings
bridge
gap
understanding
mechanisms
kinetics
physiological
environments.
Journal of The Royal Society Interface,
Journal Year:
2023,
Volume and Issue:
20(203)
Published: June 1, 2023
The
mechanistic
factors
hypothesized
to
be
key
drivers
for
the
loss
of
infectivity
viruses
in
aerosol
phase
often
remain
speculative.
Using
a
next-generation
bioaerosol
technology,
we
report
measurements
aero-stability
several
SARS-CoV-2
variants
concern
droplets
well-defined
size
and
composition
at
high
(90%)
low
(40%)
relative
humidity
(RH)
upwards
40
min.
When
compared
with
ancestral
virus,
Delta
variant
displayed
different
decay
profiles.
At
RH,
viral
approximately
55%
was
observed
over
initial
5
s
both
variants.
Regardless
RH
variant,
greater
than
95%
lost
after
min
being
aerosolized.
Aero-stability
correlate
their
sensitivities
alkaline
pH.
Removal
all
acidic
vapours
dramatically
increased
rate
decay,
90%
2
min,
while
addition
nitric
acid
vapour
improved
aero-stability.
Similar
artificial
saliva
growth
medium
observed.
A
model
predict
is
proposed:
pH
exhaled
drives
loss;
salt
content
limits
infectivity.
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(33), P. 12351 - 12361
Published: Aug. 5, 2023
Aqueous-phase
reactions
of
α-dicarbonyls
with
ammonium
or
amines
have
been
identified
as
important
sources
secondary
brown
carbon
(BrC).
However,
the
identities
most
chromophores
in
these
and
effects
pH
remain
largely
unknown.
In
this
study,
chemical
structures,
formation
pathways,
optical
properties
individual
BrC
formed
through
aqueous
(glyoxal
methylglyoxal)
ammonium,
amino
acids,
methylamine
at
different
pH's
were
characterized
detail
by
liquid
chromatography-photodiode
array-high
resolution
tandem
mass
spectrometry.
total,
180
are
identified,
accounting
for
29-79%
light
absorption
bulk
reactions.
Thereinto,
155
newly
chromophores,
including
76
imidazoles,
57
pyrroles,
10
pyrazines,
9
pyridines,
3
imidazole-pyrroles,
explain
additionally
9-69%
absorption,
mainly
involve
four
previously
unrecognized
ammonia
methylglyoxal
dimer
pyrroles.
The
also
shows
remarkable
on
transformation
chromophores;
e.g.,
increase
from
5.0
to
7.0,
contributions
imidazoles
decrease
72%
65%,
while
pyrazines
5%
13%
+
reaction;
meanwhile,
more
small
nitrogen
heterocycles
transformed
into
oligomers
(e.g.,
C9
C12
pyrroles)
via
reaction
methylglyoxal.
These
proposed
pathways
instructive
future
field
studies
aqueous-phase
BrC.
Atmospheric chemistry and physics,
Journal Year:
2023,
Volume and Issue:
23(17), P. 9765 - 9785
Published: Sept. 4, 2023
Abstract.
Multiphase
chemistry
occurs
between
chemicals
in
different
atmospheric
phases,
typically
involving
gas–solid
and
gas–liquid
interactions.
The
importance
of
multiphase
has
long
been
recognized.
Its
central
role
extends
from
acid
precipitation
stratospheric
ozone
depletion
to
its
impact
on
the
oxidizing
capacity
troposphere
roles
that
aerosol
particles
play
driving
chemistry–climate
interactions
affecting
human
health.
This
opinion
article
briefly
introduces
subject
tracks
development
before
after
start
Atmospheric
Chemistry
Physics.
Most
focuses
research
opportunities
challenges
field.
Central
themes
are
a
fundamental
understanding
at
molecular
level
underpins
ability
accurately
predict
environmental
change
discipline
is
strongest
when
tightly
connected
modeling
field
observations.
Nature Communications,
Journal Year:
2024,
Volume and Issue:
15(1)
Published: May 30, 2024
Abstract
Traditional
atmospheric
chemistry
posits
that
sulfur
dioxide
(SO
2
)
can
be
oxidized
to
sulfate
4
2–
through
aqueous-phase
reactions
in
clouds
and
gas-phase
oxidation.
Despite
adequate
knowledge
of
traditional
mechanisms,
several
studies
have
highlighted
the
potential
for
SO
oxidation
within
aerosol
water.
Given
widespread
presence
tropospheric
aerosols,
2−
production
water
could
a
pervasive
global
impact.
Here,
we
quantify
contributions
aqueous
pathways
formation
based
on
GEOS-Chem
simulations
subsequent
theoretical
calculations.
Hydrogen
peroxide
(H
O
significantly
influences
continental
regions
both
horizontally
vertically.
Over
past
two
decades,
shifts
typical
cities
reveal
an
intriguing
trend:
despite
reductions
emissions,
increased
capacities,
like
rising
H
levels,
prevent
steady
decline
concentrations.
Abating
oxidants
would
facilitate
benefit
reduction
positive
feedback
mitigation.