Journal of Plant Nutrition and Soil Science,
Journal Year:
2022,
Volume and Issue:
185(1), P. 44 - 59
Published: Jan. 22, 2022
Abstract
Background
Knowledge
of
the
stabilizing
mechanisms
soil
organic
matter
(SOM)
is
extremely
important
for
numerous
functions.
For
this,
insight
into
nature
through
appropriate
model
concepts
are
crucial.
Aims
several
years,
a
heated
debate
has
emerged
on
transformation
and
stabilization
SOM.
In
present
work,
we
try
to
contribute
this
using
molecular
modeling
providing
comprehensive
overview
history
application
tools
developing
structural
Methods
Molecular
methods
based
quantum
and/or
classical
mechanics
were
used
SOM
related
properties
including
interactions
with
reactive
surfaces
minerals.
Results
Modeling
aggregates
revealed
that
hydrogen
bonds
cation
bridges
main
factors
in
solution,
whereas
pH
modifies
stability.
The
modeled
supramolecular
exhibit
physicochemical
properties,
similar
those
humic
substances
(HS)
described
literature.
HS
models
kaolinite
nanopores
led
partial
disintegration
individual
molecules
smaller
subaggregates.
Conclusions
From
point
view,
microaggregate
stable
solution.
However,
their
binding
mineral
constituents
can
be
also
form
or
Thus,
stability
relative,
depending
interacting
environment.
This
reconciles
two
points
view
HS:
either
as
small
structures.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(12), P. 9123 - 9132
Published: June 8, 2022
Fe(II)
has
been
extensively
studied
due
to
its
importance
as
a
reductant
in
biogeochemical
processes
and
contaminant
attenuation.
Previous
studies
have
shown
that
ligands
can
alter
aqueous
redox
reactivity
but
their
data
interpretation
is
constrained
by
the
use
of
probe
compounds.
Here,
we
employed
mediated
electrochemical
oxidation
(MEO)
an
approach
directly
quantify
extent
absence
presence
three
model
organic
(citrate,
nitrilotriacetic
acid,
ferrozine)
across
range
potentials
(EH)
pH,
thereby
manipulating
over
broad
fixed
thermodynamic
conditions.
Fe(III)-stabilizing
enhanced
thermodynamically
unfavorable
regions
(i.e.,
low
pH
EH)
while
stabilizing
ligand
(ferrozine)
prevented
all
regions.
We
experimentally
derived
apparent
standard
potentials,
EHϕ,
for
these
other
(oxalate,
oxalate2,
NTA2,
EDTA,
OH2)
Fe-ligand
couples
via
oxidative
current
integration.
Preferential
stabilization
Fe(III)
decreased
EHϕ
values,
Nernstian
correlation
between
log(KFe(III)/KFe(II))
exists
wide
stability
constants.
used
this
estimate
natural
matter
isolate,
demonstrating
MEO
be
measure
iron
constant
ratios
unknown
ligands.
Environmental Science & Technology,
Journal Year:
2022,
Volume and Issue:
56(13), P. 9806 - 9815
Published: June 20, 2022
Birnessite
(δ-MnO2)
is
a
layered
manganese
oxide
widely
present
in
the
environment
and
actively
participates
transformation
of
natural
organic
matter
(NOM)
biogeochemical
processes.
However,
effect
oxygen
on
dynamic
interface
processes
NOM
δ-MnO2
remains
unclear.
This
study
systematically
investigated
interactions
between
fulvic
acid
(FA)
under
both
aerobic
anaerobic
conditions.
FA
was
transformed
by
via
direct
electron
transfer
generated
reactive
species
(ROS).
During
32-day
reaction,
79.8%
total
carbon
(TOC)
solution
removed
conditions,
unexpectedly
higher
than
that
conditions
(69.8%),
suggesting
limitation
more
conducive
to
oxidative
δ-MnO2.
The
vacancies
(OV)
surface
were
exposed
thus
promoting
adsorption
as
well
regeneration
active
sites.
Additionally,
reaction
with
weakened
strongly
bonded
lattice
(Olatt),
released
Olatt
an
important
source
ROS.
Interestingly,
part
(OC)
preserved
forming
MnCO3,
which
might
be
novel
mechanism
for
preservation.
These
findings
contribute
improved
understanding
MnO2
provide
new
insights
into
effects
cycling
preservation
OC.
Environmental Science & Technology,
Journal Year:
2023,
Volume and Issue:
57(14), P. 5988 - 5998
Published: March 30, 2023
Methylmercury
(MeHg)
is
a
potent
neurotoxin
and
has
great
adverse
health
impacts
on
humans.
Organisms
sunlight-mediated
demethylation
are
well-known
detoxification
pathways
of
MeHg,
yet
whether
abiotic
environmental
components
contribute
to
MeHg
degradation
remains
poorly
known.
Here,
we
report
that
can
be
degraded
by
trivalent
manganese
(Mn(III)),
naturally
occurring
widespread
oxidant.
We
found
28
±
4%
could
Mn(III)
located
synthesized
Mn
dioxide
(MnO2–x)
surfaces
during
the
reaction
0.91
μg·L–1
5
g·L–1
mineral
at
an
initial
pH
6.0
for
12
h
in
10
mM
NaNO3
25
°C.
The
presence
low-molecular-weight
organic
acids
(e.g.,
oxalate
citrate)
substantially
enhances
MnO2–x
via
formation
soluble
Mn(III)-ligand
complexes,
leading
cleavage
carbon–Hg
bond.
also
reactions
with
Mn(III)-pyrophosphate
apparent
rate
constants
comparable
those
biotic
photolytic
degradation.
Thiol
ligands
(cysteine
glutathione)
show
negligible
effects
Mn(III).
This
research
demonstrates
potential
roles
degrading
natural
environments,
which
may
further
explored
remediating
heavily
polluted
soils
engineered
systems
containing
MeHg.
Soil Biology and Biochemistry,
Journal Year:
2023,
Volume and Issue:
178, P. 108962 - 108962
Published: Jan. 19, 2023
Wetlands
host
∼20%
of
terrestrial
organic
carbon
and
serve
as
a
major
sink
for
atmospheric
carbon.
Anoxic
soils
sediments
accrue
soil
(SOC)
partly
by
hampering
the
activity
extracellular
oxidative
enzymes
that
break
down
phenolic
polymers.
Upon
aeration,
fungal-driven
enzymatic
depolymerization
microbial
respiration
released
monomers
ensue.
Redox-active
metals
can
simultaneously
catalyze
abiotic
nonspecific
oxidation
SOC,
notable
examples
including
Mn(III)
or
Fe(II)
through
Fenton-like,
hydrogen
peroxide-catalyzed
radical
production.
However,
extent
reactive
metal
contributions
to
biotic
SOC
degradation
is
not
understood
in
context
natural
environments
with
diverse
redox
chemistry.
We
tested
relative
fungi,
substrate
(L-DOPA)
floodplain
representing
range
transient
conditions
driven
permanent
vs.
periodic
flooding.
Phenol
potential
was
highest
permanently
flooded
fewer
fungal
taxa
known
observed
(per)oxidase
instead
correlated
HCl-extractable
Fe(II),
Fe(total)
Fe(II)/Fe(total),
suggesting
specific
role
Fe(II).
additions
enhanced
phenol
sterilized
non-sterilized
presence
peroxide,
indicating
Fe-mediated
chemistry
could
significantly
enhance
wetland
throughout
redox-active
soils.
Fungal
community
composition
did
correlate
overall
only
more
oxic
adjacent
river
communities
showed
declining
after
sterilization.
addition
across
all
soils,
although
it
appeared
drive
fungal-mediated
most
aerated
Understanding
how
mediate
oxidants
microbially-harnessed
enzyme
cofactors
substrates
under
variable
hydrologic
controls
will
improve
our
ability
represent
models
other
frequently
saturated
Soil Biology and Biochemistry,
Journal Year:
2024,
Volume and Issue:
195, P. 109449 - 109449
Published: April 27, 2024
Given
the
increasingly
recognised
importance
of
microbial
biomass
(MB)
in
soil
organic
carbon
(SOC)
sequestration,
knowledge
ionome
beyond
(C),
nitrogen
(N)
and
phosphorus
(P)
becomes
crucial.
The
could
indicate
nutritional
restrictions
related
to
MB
growth
necromass
C
(MN-C)
accumulation.
In
this
study,
soils
receiving
different
combinations
mineral
N,
P
potassium
(K)
were
sampled
Askov
long-term
field
experiment,
Denmark,
analysed
for
elemental
composition
including
P,
K,
magnesium
(Mg),
manganese
(Mn)
zinc
(Zn)
using
fumigation-extraction
ICP-OES.
Furthermore,
bacterial,
archaeal
fungal
gene
abundance
was
determined
by
qPCR
as
community
shifts
may
relate
shifts.
MN-C
amino
sugar
analysis.
MB-C
unaffected
fertiliser
treatments
not
correlated
with
MN-C.
N
fertilisation
increased
K
additions
plant-derived
SOC,
indicating
SOC
Availability
MB-P
MB-K,
respectively,
reduced
MB-C:P
ratio
but
MB-C:K.
pH
Mn
availability
which
MB-Mn
MB-C:Mn.
ITS1
copies
responded
positively
availability.
A
MB-C:Mn
associated
a
relative
increase
copy
abundance.
This
linked
an
positive
link
between
availability,
level,
yet
reflected
accumulation,
accumulation
possibly
due
plant
turnover.
Biogeosciences,
Journal Year:
2022,
Volume and Issue:
19(9), P. 2333 - 2351
Published: May 5, 2022
Abstract.
Arctic
warming
and
permafrost
degradation
are
modifying
northern
ecosystems
through
changes
in
microtopography,
soil
water
dynamics,
nutrient
availability,
vegetation
succession.
Upon
degradation,
the
release
of
deep
stores
nutrients,
such
as
nitrogen
phosphorus,
from
newly
thawed
stimulates
production.
More
specifically,
wetter
lowlands
show
an
increase
sedges
(as
part
graminoids),
whereas
drier
uplands
favor
shrub
expansion.
These
shifts
composition
may
influence
local
mineral
element
cycling
litter
In
this
study,
we
evaluate
on
foliar
stocks
potential
annual
fluxes
upon
litterfall.
We
measured
elemental
(Al,
Ca,
Fe,
K,
Mn,
P,
S,
Si,
Zn)
∼
500
samples
typical
tundra
plant
species
two
contrasting
Alaskan
sites,
i.e.,
experimental
sedge-dominated
site
(Carbon
Permafrost
Experimental
Heating
Research,
CiPEHR)
natural
shrub-dominated
(Gradient).
The
concentration
these
elements
was
specific,
with
sedge
leaves
having
relatively
high
Si
Ca
Mn
concentrations.
Therefore,
biomass
response
to
thaw
expected
be
main
factors
that
dictate
maximum
observed
litterfall
fluxes,
increasing
expansion
sites
(CiPEHR),
Consequently,
expect
will
lead
therefore
affect
across
sub-Arctic
implications
for
further
Biogeochemistry,
Journal Year:
2023,
Volume and Issue:
165(1), P. 91 - 111
Published: July 7, 2023
Organo-mineral
and
organo-metal
associations
play
an
important
role
in
the
retention
accumulation
of
soil
organic
carbon
(SOC).
Recent
studies
have
demonstrated
a
positive
correlation
between
calcium
(Ca)
SOC
content
range
types.
However,
most
these
focused
on
soils
that
contain
carbonate
(pH
>
6).
To
assess
importance
Ca-SOC
lower
pH
soils,
we
investigated
their
physical
chemical
interaction
grassland
Point
Reyes
National
Seashore
(CA,
USA)
at
spatial
scales.
Multivariate
analyses
our
bulk
characterisation
dataset
showed
strong
exchangeable
Ca
(Ca