Detritusphere
is
a
hotspot
of
carbon
cycling
in
terrestrial
ecosystems,
yet
the
mineralization
soil
organic
(SOC)
within
this
microregion
associated
with
reactive
oxygen
species
(ROS)
remains
unclear.
Herein,
we
investigated
ROS
production
and
distribution
detritusphere
six
representative
soils
evaluated
their
contributions
to
SOC
mineralization.
We
found
that
was
significantly
correlated
several
chemical
biological
factors,
including
pH,
water-soluble
phenols,
water-extractable
carbon,
phenol
oxidase
activity,
surface-bound
or
complexed
Fe(II)
low-crystalline
minerals,
highly
crystalline
Fe(II)-bearing
SOC.
These
factors
collectively
contributed
99.6%
variation
production,
as
revealed
by
redundancy
analyses.
Among
ROS,
hydroxyl
radicals
(•OH)
were
key
contributors
mineralization,
responsible
for
10.4%-38.7%
CO2
emissions
quenching
experiments.
Inhibiting
•OH
decreased
C-degrading
enzyme
activities,
indicating
stimulates
increasing
activity.
Structural
equation
modeling
further
demonstrated
promotes
activities
degrading
phenols
unlock
"enzyme
latch"
availability
upregulate
gene
expression.
pathways
equally
exceeded
its
direct
effect.
findings
provide
detailed
insight
into
mechanistic
•OH-mediated
dynamics
detritusphere.
Eco-Environment & Health,
Journal Year:
2024,
Volume and Issue:
3(1), P. 59 - 76
Published: Jan. 3, 2024
Soil,
the
largest
terrestrial
carbon
reservoir,
is
central
to
climate
change
and
relevant
feedback
environmental
health.
Minerals
are
essential
components
that
contribute
over
60%
of
soil
storage.
However,
how
interactions
between
minerals
organic
shape
transformation
stability
remains
poorly
understood.
Herein,
we
critically
review
primary
mechanisms,
including
sorption,
redox
reaction,
co-precipitation,
dissolution,
polymerization,
catalytic
reaction.
These
interactions,
highly
complex
with
combination
multiple
processes,
greatly
affect
through
following
processes:
(1)
formation
or
deconstruction
mineral-organic
association;
(2)
oxidative
minerals;
(3)
polymerization
(4)
varying
association
according
mineral
transformation.
Several
pieces
evidence
related
turnover
during
interaction
in
real
eco-environment
then
demonstrated.
We
also
highlight
current
research
gaps
outline
priorities,
which
may
map
future
directions
for
a
deeper
mechanisms-based
understanding
storage
capacity
considering
its
minerals.
Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(17), P. 7403 - 7414
Published: April 17, 2024
Photochemically
generated
reactive
oxygen
species
(ROS)
are
widespread
on
the
earth's
surface
under
sunlight
irradiation.
However,
nonphotochemical
ROS
generation
in
water
(e.g.,
paddy
overlying
water)
has
been
largely
neglected.
This
work
elucidated
drivers
of
and
its
spatial
distribution
undisturbed
water,
by
combining
imaging
technology
with
situ
monitoring.
It
was
found
that
H2O2
concentrations
formed
three
waters
could
reach
0.03–16.9
μM,
profiles
exhibited
heterogeneity.
The
O2
planar-optode
indicated
redox
interfaces
were
not
always
at
soil–water
interface
but
also
possibly
layer,
depending
soil
properties.
facilitated
a
rapid
turnover
reducing
oxidizing
substances,
creating
an
ideal
environment
for
ROS.
Additionally,
electron-donating
capacities
increased
4.5–8.4
times
compared
to
top
layers.
Importantly,
field
investigation
results
confirmed
sustainable
•OH
through
pathways
constituted
significant
proportion
total
daily
production
(>50%),
suggesting
comparable
or
even
greater
role
than
photochemical
generation.
In
summary,
process
reported
this
study
greatly
enhances
understanding
natural
processes
soils.
This
study
quantifies
the
contribution
of
H2O2-dependent
pathway
to
hydroxyl
radical
(•OH)
production
from
photolysis
dissolved
organic
matter
(DOM).
•OH
formation
rates
were
cross-validated
using
benzoate
and
terephthalate
as
probe
compounds
for
diverse
DOM
sources
(reference
isolates
whole
waters).
Catalase
addition
revealed
that
accounts
10-20%
total
in
isolate
materials,
but
no
significant
correlation
was
observed
between
ambient
iron
(Fe)
concentrations
formation.
lack
likely
due
lower
Fe
levels
isolated
thus
limiting
concentration
photochemically
produced
Fe(II)
available
reaction
with
H2O2.
Notably,
contributed
11
±
3%
Pony
Lake
fulvic
acid,
which
had
lowest
content,
implicating
additional
H2O2-driven
mechanisms
independent
Fe.
Experiments
model
acetophenone
p-benzoquinone
indicated
triplet
reactions
However,
rate
increased
6-fold
when
H2O2
reduced
by
ketyl
radicals
formed
excited
2,4,6-trimethylphenol.
advances
knowledge
photolysis,
providing
insight
into
role
aquatic
photochemical
processes.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
57(47), P. 18550 - 18562
Published: Dec. 7, 2022
The
efficient
and
selective
removal
of
refractory
antibiotics
from
high-strength
antibiotic
production
wastewater
is
crucial
but
remains
a
substantial
challenge.
In
this
study,
novel
ozone
micronano-bubble
(MNB)-enhanced
treatment
system
was
constructed
for
treatment.
Compared
with
conventional
ozone,
MNBs
exhibit
excellent
efficiency
oxytetracycline
(OTC)
degradation
toxicity
decrease.
Notably,
study
identifies
the
overlooked
singlet
oxygen
(1O2)
first
time
as
active
species
in
MNB
through
probe
electron
paramagnetic
resonance
methods.
Subsequently,
oxidation
mechanisms
OTC
by
are
systematically
investigated.
Owing
to
high
reactivity
toward
1O2,
enhance
anti-interference
performance
raw
complex
matrixes.
This
provides
insights
into
mechanism
MNB-enhanced
pollutant
new
perspective
high-concentration
industrial
using
MNBs.
addition,
presents
promising
technology
scientific
guidance
wastewater.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(18), P. 13408 - 13418
Published: Sept. 5, 2022
Hydrogen
peroxide
(H2O2)
and
hydroxyl
radical
(•OH)
production
during
oxygenation
of
reduced
iron
(Fe(II))
natural
organic
matter
(NOM)
in
the
subsurface
has
been
increasingly
discovered,
whereas
effect
C/Fe
molar
ratio
Fe(II)
NOM
coexisting
systems
remains
poorly
understood.
In
this
study,
aqueous
humic
acid
(HAred)
mixture
at
different
ratios
(0-20)
were
oxygenated.
Results
show
that
both
H2O2
•OH
accumulation
increased
almost
linearly
with
increase
ratio,
a
more
prominent
high
ratios.
At
low
(C/Fe
≤
1.6),
electrons
mainly
transferred
from
dissolved
inorganic
Fe(II),
surface-adsorbed
proportion
HA-complexed
to
O2;
level
≥
5),
main
electron
source
turned
free
HAred.
The
changes
transfer
pathway
yield
relative
H2O2.
This
study
highlights
important
role
controlling
therefore
accurately
evaluating
associated
environmental
impacts.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(22), P. 16483 - 16493
Published: Nov. 3, 2022
Reactive
oxygen
species
(ROS)
play
key
roles
in
soil
biogeochemical
processes,
yet
the
occurrence
and
accumulation
of
ROS
rhizosphere
are
poorly
documented.
Herein,
we
first
developed
a
ROS-trapping
membrane
to
situ
determine
ryegrass
then
quantified
temporal
spatial
variations
representative
(i.e.,
O2•─,
H2O2,
•OH).
Fluorescence
imaging
clearly
visualized
production
rhizosphere.
Both
O2•─
H2O2
content
increased
declined
throughout
life
cycle
ryegrass,
while
•OH
concentration
decreased
continuously.
Spatially,
contents
remained
at
relatively
high
level
0-5
mm
descended
with
increasing
distance.
The
concentrations
different
soils
followed
order
black
>
latosol
yellow-brown
tier
∼
red
soil.
Analysis
properties
suggested
that
both
biotic
factors
(microbial
community)
abiotic
(Fe(II)
water-soluble
phenols)
played
critical
production.
combined
including
Fe(II)
phenol-mediated
electron
transfer,
microbial
community-driven
extracellular
release,
Fe(II)/Fe(III)
cycling,
may
be
responsible
for
These
findings
provide
insights
into
ROS-associated
effects
inspiration
phytoremediation
pollutants
element
cycling.
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(43), P. 16340 - 16347
Published: Oct. 19, 2023
Frequent
cycles
of
flooding
and
drainage
in
paddy
soils
lead
to
the
reductive
dissolution
iron
(Fe)
minerals
reoxidation
Fe(II)
species,
all
while
generating
a
robust
consistent
output
reactive
oxygen
species
(ROS).
In
this
study,
we
present
comprehensive
assessment
temporal
spatial
variations
Fe
ROS
during
flooding-drainage
process
representative
soil.
Our
laboratory
column
experiments
showed
that
decrease
dissolved
O2
concentration
led
rapid
reduction
below
water-soil
interface,
aqueous
was
transformed
into
solid
phases
over
an
extended
time.
As
result,
•OH
production
capacity
liquid
reduced
improved.
The
increased
from
227-271
μmol
kg-1
(within
1-11
cm
depth)
500-577
499-902
after
50
day,
3
month,
1
year
incubation,
respectively.
During
drainage,
dynamic
triggered
by
consumption
oxidation.
ROS-trapping
film
situ
capture
revealed
soil
surface
active
zone
for
intense
H2O2
production,
limited
observed
deeper
layers
(>5
cm)
due
penetration.
These
findings
provide
more
insights
complex
interplay
between
cycling
redox
transition
zones
fields.