Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(14), P. 9845 - 9853
Published: June 30, 2021
Most
of
the
cadmium
(Cd)
accumulated
in
rice
grains
is
derived
from
its
remobilization
soils
during
grain
filling
period
when
paddy
water
drained.
The
factors
affecting
Cd
upon
drainage
remain
poorly
understood.
Here,
we
show
that
free
radical
effect
produced
oxidation
ferrous
sulfides
an
important
mechanism
oxidative
soil
drainage.
When
were
flooded,
microbial
sulfate
reduction
results
formation
various
metal
including
CdS
and
FeS.
Upon
drainage,
FeS
considerable
amounts
hydroxyl
radicals
(OH•),
which
could
oxidize
directly
thereby
promote
dissolution
increase
mobilization
soils.
also
form
a
within-sulfide
voltaic
cell,
with
protecting
due
to
lower
electrochemical
potential
former.
However,
this
was
short-lived
surpassed
by
effect.
composition
formed
flooding
vary
soils,
affected
both
effects
offered
different
sulfides.
These
are
applicable
biogeochemistry
other
chalcophile
trace
elements
coupled
sulfur
iron
redox
cycles
anoxic-oxic
transition
many
environments.
Chemical Reviews,
Journal Year:
2021,
Volume and Issue:
121(13), P. 8161 - 8233
Published: June 18, 2021
Iron
(Fe)
is
the
fourth
most
abundant
element
in
earth's
crust
and
plays
important
roles
both
biological
chemical
processes.
The
redox
reactivity
of
various
Fe(II)
forms
has
gained
increasing
attention
over
recent
decades
areas
(bio)
geochemistry,
environmental
chemistry
engineering,
material
sciences.
goal
this
paper
to
review
these
advances
current
state
knowledge
environment.
Specifically,
comprehensive
focuses
on
four
types
species
including
aqueous
Fe(II),
complexed
with
ligands,
minerals
bearing
structural
sorbed
mineral
oxide
surfaces.
formation
pathways,
factors
governing
reactivity,
insights
into
potential
mechanisms,
comparison,
characterization
techniques
are
discussed
reference
breakthroughs
field
where
possible.
We
also
cover
applications
zerovalent
iron,
microbial
processes,
biogeochemical
cycling
carbon
nutrients,
their
abiotic
oxidation
related
processes
natural
engineered
systems.
National Science Review,
Journal Year:
2022,
Volume and Issue:
9(10)
Published: July 4, 2022
Mineral–microbe
interactions
play
important
roles
in
environmental
change,
biogeochemical
cycling
of
elements
and
formation
ore
deposits.
Minerals
provide
both
beneficial
(physical
chemical
protection,
nutrients,
energy)
detrimental
(toxic
substances
oxidative
pressure)
effects
to
microbes,
resulting
mineral-specific
microbial
colonization.
Microbes
impact
dissolution,
transformation
precipitation
minerals
through
their
activity,
either
genetically
controlled
or
metabolism-induced
biomineralization.
Through
these
interactions,
microbes
co-evolve
Earth
history.
typically
occur
at
microscopic
scale
but
the
effect
is
often
manifested
global
scale.
Despite
advances
achieved
decades
research,
major
questions
remain.
Four
areas
are
identified
for
future
research:
integrating
mineral
ecology,
establishing
biosignatures,
linking
laboratory
mechanistic
investigation
field
observation,
manipulating
mineral–microbe
benefit
humankind.
Environmental Science & Technology,
Journal Year:
2021,
Volume and Issue:
55(18), P. 12136 - 12152
Published: Sept. 1, 2021
Manganese
(Mn)
is
a
biologically
important
and
redox-active
metal
that
may
exert
poorly
recognized
control
on
carbon
(C)
cycling
in
terrestrial
ecosystems.
influences
ecosystem
C
dynamics
by
mediating
biochemical
pathways
include
photosynthesis,
serving
as
reactive
intermediate
the
breakdown
of
organic
molecules,
binding
and/or
oxidizing
molecules
through
organo-mineral
associations.
However,
potential
for
Mn
to
influence
storage
remains
unresolved.
Although
substantial
research
has
demonstrated
ability
Fe-
Al-oxides
stabilize
matter,
there
scarcity
similar
information
regarding
Mn-oxides.
Furthermore,
Mn-mediated
reactions
regulate
litter
decomposition
pathways,
but
these
processes
are
constrained
across
diverse
Here,
we
discuss
ecological
roles
environments
synthesize
existing
knowledge
multiple
which
biogeochemical
intersect.
We
demonstrate
high
degrade
abiotic
microbially
mediated
oxidation
at
least
temporarily,
outline
priorities
needed
advance
understanding
Mn-C
interactions,
highlighting
gaps
address
key
uncertainties
soil
predictions.
Nature Communications,
Journal Year:
2020,
Volume and Issue:
11(1)
Published: Dec. 10, 2020
Abstract
It
has
been
shown
that
reactive
soil
minerals,
specifically
iron(III)
(oxyhydr)oxides,
can
trap
organic
carbon
in
soils
overlying
intact
permafrost,
and
may
limit
mobilization
degradation
as
it
is
observed
other
environments.
However,
the
use
of
iron(III)-bearing
minerals
terminal
electron
acceptors
permafrost
environments,
thus
their
stability
capacity
to
prevent
during
thaw,
poorly
understood.
We
have
followed
dynamic
interactions
between
iron
using
a
space-for-time
approach
across
thaw
gradient
Abisko
(Sweden),
where
wetlands
are
expanding
rapidly
due
thaw.
show
through
bulk
(selective
extractions,
EXAFS)
nanoscale
analysis
(correlative
SEM
nanoSIMS)
bound
Fe
primarily
transition
mineral
horizons
palsa
underlain
by
(41.8
±
10.8
mg
per
g
soil,
9.9
14.8%
total
carbon).
During
water-logging
O
2
limitation
lead
reducing
conditions
an
increase
abundance
Fe(III)-reducing
bacteria
which
favor
dissolution
drive
both
along
gradient.
By
providing
acceptor,
this
rusty
sink
effectively
destroyed
cannot
release
with
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(6), P. 3386 - 3396
Published: March 1, 2022
Hydroxyl
radical
(•OH)
is
an
active
species
widely
reported
in
studies
across
many
scientific
fields,
and
hence,
its
reliable
analysis
vitally
important.
Currently,
alcohols
are
commonly
used
as
scavengers
for
•OH
determination.
However,
the
impacts
of
on
reliability
detection
remain
unknown.
In
this
study,
we
found
that
adding
different
types
amounts
water
samples
treated
with
ultraviolet
irradiation
undesirably
produced
substantial
hydrogen
peroxide
(H2O2),
which
a
known
precursor.
This
means
conventional
determination
method
using
likely
unreliable
or
even
misleading.
Through
careful
investigation,
revealed
overlooked
reaction
pathway
during
H2O2
transformations.
Varying
oxygen
concentrations,
pHs,
alcohol
dosages,
altered
formation,
can
affect
accuracy.
Among
alcohols,
n-butanol
best
scavenger
because
it
quenches
rapidly
but
re-forms
little
H2O2.
Global Change Biology,
Journal Year:
2021,
Volume and Issue:
28(3), P. 1178 - 1196
Published: Dec. 4, 2021
Understanding
the
controls
on
amount
and
persistence
of
soil
organic
carbon
(C)
is
essential
for
predicting
its
sensitivity
to
global
change.
The
response
may
depend
whether
C
unprotected,
isolated
within
aggregates,
or
protected
from
decomposition
by
mineral
associations.
Here,
we
present
a
synthesis
relative
influence
environmental
factors
partitioning
among
pools,
abundance
in
each
pool
(mg
g-1
soil),
(as
approximated
radiocarbon
abundance)
relatively
unprotected
particulate
mineral-bound
pools.
We
show
that
mineral-associated
pools
consistently
differed
one
another
degree
relationship
factors.
Soil
depth
was
best
predictor
persistence,
though
it
accounted
more
variance
persistence.
Persistence
all
decreased
with
increasing
mean
annual
temperature
(MAT)
throughout
profile,
whereas
increased
wetness
index
(MAP/PET)
subsurface
soils
(30-176
cm).
soil)
climate
varied
depth.
Mineral-associated
surface
(<30
cm)
strongly
than
free
C,
but
both
showed
attenuated
responses
at
Overall,
these
relationships
suggest
strong
properties,
potential
loss
areas
decreasing
wetness.
Relative
significantly
land
cover
types
parent
material
lithologies.
This
variability
pool's
suggests
not
equally
vulnerable
Therefore,
projections
future
based
patterns
bulk
be
misleading.