Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(28), P. 12430 - 12440
Published: July 5, 2024
Soil
organic
carbon
(SOC)
is
pivotal
for
both
agricultural
activities
and
climate
change
mitigation,
biochar
stands
as
a
promising
tool
bolstering
SOC
curtailing
soil
dioxide
(CO2)
emissions.
However,
the
involvement
of
in
dynamics
underlying
interactions
among
biochar,
microbes,
iron
minerals,
fresh
matter
(FOM,
such
plant
debris)
remain
largely
unknown,
especially
soils
after
long-term
amendment.
We
therefore
introduced
FOM
to
with
without
decade-long
history
amendment,
performed
microcosm
incubations,
evaluated
well
microbial
properties.
Biochar
amendment
resulted
2-fold
accrual
over
decade
attenuated
FOM-induced
CO2
emissions
by
approximately
11%
during
56-day
incubation
through
diverse
pathways.
Notably,
facilitated
microbially
driven
reduction
subsequent
Fenton-like
reactions,
potentially
having
enhanced
extracellular
electron
transfer
use
efficiency
long
run.
Throughout
cycling
processes,
physical
protection
minerals
could
contribute
accumulation
debris
preservation,
alongside
direct
adsorption
occlusion
particles.
Furthermore,
slurry
experiments,
sterilization
ferrous
stimulation
controls,
confirmed
role
microbes
hydroxyl
radical
generation
biotic
sequestration
biochar-amended
soils.
Overall,
our
study
sheds
light
on
intricate
abiotic
mechanisms
governing
upland
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.
Nature Communications,
Journal Year:
2023,
Volume and Issue:
14(1)
Published: April 13, 2023
Ice-rich
Pleistocene-age
permafrost
is
particularly
vulnerable
to
rapid
thaw,
which
may
quickly
expose
a
large
pool
of
sedimentary
organic
matter
(OM)
microbial
degradation
and
lead
emissions
climate-sensitive
greenhouse
gases.
Protective
physico-chemical
mechanisms
may,
however,
restrict
accessibility
reduce
OM
decomposition;
that
be
influenced
by
changing
environmental
conditions
during
sediment
deposition.
Here
we
study
different
fractions
in
Siberian
deposited
colder
warmer
periods
the
past
55,000
years.
Among
known
stabilization
mechanisms,
occlusion
aggregates
minor
importance,
while
33-74%
carbon
associated
with
small,
<6.3
µm
mineral
particles.
Preservation
mineral-associated
enhanced
reactive
iron
minerals
cold
dry
climate,
reflected
low
CO2
production
incubation
experiments.
Warmer
wetter
stabilization,
shown
more
decomposed
up
30%
higher
production.
This
shows
considering
stability
bioavailability
important
for
predicting
future
climate-carbon
feedback.
Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(24), P. 10623 - 10631
Published: May 23, 2024
Iron
minerals
are
widespread
in
earth's
surface
water
and
soil.
Recent
studies
have
revealed
that
under
sunlight
irradiation,
iron
photoactive
on
producing
reactive
oxygen
species
(ROS),
a
group
of
key
regulating
elemental
cycling,
microbe
inactivation,
pollutant
degradation.
In
nature,
exhibit
varying
crystallinity
different
hydrogeological
conditions.
While
is
known
parameter
determining
the
overall
activity
minerals,
impact
mineral
photochemical
ROS
production
remains
unknown.
Here,
we
assessed
from
ferrihydrites
with
degrees
crystallinity.
All
examined
demonstrated
photoactivity
resulting
generation
hydrogen
peroxide
(H2O2)
hydroxyl
radical
(•OH).
The
increased
decreasing
ferrihydrite
crystallinity-dependent
•OH
was
primarily
attributed
to
conduction
band
reduction
reactions,
O2
by
electrons
being
rate-limiting
process.
Conversely,
had
negligible
influence
photon-to-electron
conversion
efficiency
or
Fenton-like
activity.
difference
productions
led
discrepant
degradation
organic
pollutants
surfaces.
Our
study
provides
valuable
insights
into
natural
systems,
emphasizing
significance
photochemistry
sites
abundant
lower-crystallinity
such
as
wetland
soils.
Abstract
Climate
change
in
the
Arctic
is
altering
watershed
hydrologic
processes
and
biogeochemistry.
Here,
we
present
an
emergent
threat
to
watersheds
based
on
observations
from
75
streams
Alaska’s
Brooks
Range
that
recently
turned
orange,
reflecting
increased
loading
of
iron
toxic
metals.
Using
remote
sensing,
constrain
timing
stream
discoloration
last
10
years,
a
period
rapid
warming
snowfall,
suggesting
impairment
likely
due
permafrost
thaw.
Thawing
can
foster
chemical
weathering
minerals,
microbial
reduction
soil
iron,
groundwater
transport
metals
streams.
Compared
clear
reference
streams,
orange
have
lower
pH,
higher
turbidity,
sulfate,
trace
metal
concentrations,
supporting
sulfide
mineral
as
primary
mobilization
process.
Stream
was
associated
with
dramatic
declines
macroinvertebrate
diversity
fish
abundance.
These
findings
considerable
implications
for
drinking
water
supplies
subsistence
fisheries
rural
Alaska.
Environmental Science & Technology,
Journal Year:
2024,
Volume and Issue:
58(28), P. 12430 - 12440
Published: July 5, 2024
Soil
organic
carbon
(SOC)
is
pivotal
for
both
agricultural
activities
and
climate
change
mitigation,
biochar
stands
as
a
promising
tool
bolstering
SOC
curtailing
soil
dioxide
(CO2)
emissions.
However,
the
involvement
of
in
dynamics
underlying
interactions
among
biochar,
microbes,
iron
minerals,
fresh
matter
(FOM,
such
plant
debris)
remain
largely
unknown,
especially
soils
after
long-term
amendment.
We
therefore
introduced
FOM
to
with
without
decade-long
history
amendment,
performed
microcosm
incubations,
evaluated
well
microbial
properties.
Biochar
amendment
resulted
2-fold
accrual
over
decade
attenuated
FOM-induced
CO2
emissions
by
approximately
11%
during
56-day
incubation
through
diverse
pathways.
Notably,
facilitated
microbially
driven
reduction
subsequent
Fenton-like
reactions,
potentially
having
enhanced
extracellular
electron
transfer
use
efficiency
long
run.
Throughout
cycling
processes,
physical
protection
minerals
could
contribute
accumulation
debris
preservation,
alongside
direct
adsorption
occlusion
particles.
Furthermore,
slurry
experiments,
sterilization
ferrous
stimulation
controls,
confirmed
role
microbes
hydroxyl
radical
generation
biotic
sequestration
biochar-amended
soils.
Overall,
our
study
sheds
light
on
intricate
abiotic
mechanisms
governing
upland