Environmental Science Nano,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Jan. 1, 2024
An
optimum
application
of
NPs
can
mitigate
biotic
and
abiotic
stresses,
but
overuse
cause
phytotoxicity.
Research
on
the
use
for
plant
stress
is
demonstrating
promising
benefits.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(18), P. 4077 - 4098
Published: Sept. 19, 2024
Abstract.
Understanding
the
mechanisms
of
plant-derived
carbon
(C)
and
nitrogen
(N)
transformation
stabilization
in
soil
is
fundamental
for
predicting
capacity
to
mitigate
climate
change
support
other
functions.
The
decomposition
plant
residues
particulate
organic
matter
(POM)
contributes
formation
mineral-associated
(on
average
more
stable)
(MAOM)
soil.
MAOM
formed
from
binding
dissolved
(ex
vivo
pathway)
or
microbial
necromass
bioproducts
(in
minerals
metal
colloids.
Which
these
two
(SOM)
pathways
important
under
which
conditions
remains
an
open
question.
To
address
this
question,
we
propose
a
novel
diagnostic
model
describe
C
N
dynamics
as
function
POM
decomposition.
Focusing
on
relations
among
compartments
(i.e.,
modeling
phase
space)
rather
than
time
trajectories
allows
isolating
processes
underlying
stabilization.
Using
combination
with
database
36
studies
residue
were
tracked
into
MAOM,
found
that
predominantly
fueled
by
produced
microbes
decomposing
POM.
relevance
pathway
higher
clayey
soils
but
lower
C-rich
N-poor
added
residues.
Overall,
our
space
proved
be
sound
tool
mechanistic
investigation
supported
current
understanding
critical
role
both
mineral
soils.
Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(4)
Published: Feb. 12, 2025
Abstract
Despite
the
importance
of
microbial
soil
organic
matter
(SOM)
respiration
in
regulating
flux
carbon
between
soils
and
atmosphere,
cycling
models
remain
primarily
based
on
climate
properties,
leading
to
large
uncertainty
predictions.
To
address
this
knowledge
gap,
we
analyzed
high‐resolution
water‐extractable
SOM
profiles
from
cores
collected
across
United
States
by
1,000
Soils
Pilot
Molecular
Observation
Network.
Our
innovation
lies
using
machine
learning
distill
thousands
formula
into
tractable
units;
it
enables
integrating
data
molecular
measurements
models.
In
surface
soils,
chemistry
provided
better
estimates
potential
than
physicochemistry,
them
combined
yielded
best
prediction.
Overall,
identify
specific
subsets
molecules
that
may
improve
predictions
global
create
a
strong
basis
for
developing
new
representations
process‐based
Sustainability,
Journal Year:
2024,
Volume and Issue:
16(1), P. 444 - 444
Published: Jan. 4, 2024
Understanding
the
spatial
distribution
of
soil
properties
is
essential
for
comprehending
fertility,
predicting
ecosystem
productivity,
enhancing
environmental
quality,
promoting
sustainable
agriculture,
and
addressing
global
climate
change.
This
study
focuses
on
investigating
influencing
factors
carbon
(C)
nitrogen
(N)
in
Danjiangkou
Reservoir
area,
a
vital
water
source
South-to-North
Water
Transfer
Project.
Utilizing
both
geostatistical
traditional
statistical
methods,
this
research
explores
impact
various
land-use
types—such
as
orchards,
drylands,
paddy
fields,
Hydro-Fluctuation
Belts
(HF
belts)—on
C
N
content.
The
findings
reveal
predominantly
low
levels
organic
(SOC)
(ranging
from
2.95
to
21.50
g·kg−1),
total
(TN)
0.27
2.44
available
(AN)
18.20
170.45
mg·kg−1),
mostly
falling
into
deficient
categories.
Notably,
variability
observed,
especially
agriculturally
developed
regions,
leading
areas
enrichment.
Paddy
fields
HF
belts
are
identified
influential
contributors
increased
SOC
content
compared
orchards
drylands.
Correlation
stepwise
regression
analyses
unveil
intricate
interactions
among
SOC,
TN,
AN,
factors,
underscoring
necessity
holistic
approach
management.
emphasizes
critical
role
adopting
rational
types
agricultural
practices
effective
management
area.
Journal of Geophysical Research Biogeosciences,
Journal Year:
2024,
Volume and Issue:
129(5)
Published: May 1, 2024
Abstract
Manganese
(Mn)
is
a
redox‐active
micronutrient
that
has
been
shown
to
accelerate
plant
litter
decomposition;
however,
the
effect
of
Mn‐promoted
decomposition
on
soil
C
storage
unclear.
We
present
novel
biogeochemical
model
simulating
how
Mn
bioavailability
influences
organic
(SOC)
stocks
in
profile
(<50
cm)
within
temperate
forest.
In
our
model,
foliar
increased
response
increasing
soluble
released
through
Mn‐oxide
(birnessite)
dissolution
mineral
layers.
The
ensuing
enrichment
leaf
redistributed
surface
forest
floor
layer,
promoted
enzymatic
oxidation
lignin,
and
decreased
SOC
stocks.
Total
loss
was
partially
mitigated
by
accumulation
lignin‐oxidation
products
as
mineral‐associated
C.
also
explored
Mn‐driven
changes
interacted
with
effects
N
deposition
warming.
Nitrogen
inhibited
Mn‐dependent
lignin
degradation,
weakening
their
dependence
bioavailability.
Warming
stimulated
reduced
but
less
effective
at
low
Our
results
suggest
are
sensitive
because
uptake
redistributes
soils
where
it
can
enhance
decomposition.
Based
simulations,
we
predict
becomes
limiting
poorly
soluble.
Depletion
bioavailable
or
other
cofactors
critical
could
limit
warming
over
time,
quantitative
projections
role
regulating
requires
additional
measurements
constrain
uncertainties.
Abstract.
Understanding
the
mechanisms
of
plant-derived
carbon
(C)
and
nitrogen
(N)
transformation
stabilization
in
soil
is
fundamental
for
predicting
capacity
to
mitigate
climate
change
support
other
functions.
The
decomposition
plant
residues
particulate
organic
matter
(POM)
contributes
formation
mineral
associated
(on
average
more
stable)
(MAOM)
soil.
MAOM
formed
from
binding
dissolved
(ex
vivo
pathway)
or
microbial
necromass
bioproducts
(in
minerals
metal
colloids.
Which
these
two
(SOM)
pathways
important
under
which
conditions
remains
an
open
question.
To
address
this
question,
we
propose
a
novel
diagnostic
model
describe
C
N
dynamics
as
function
POM
decomposition.
Focusing
on
relations
among
compartments
(i.e.,
modelling
phase
space)
rather
than
time
trajectories
allows
isolating
processes
underlying
stabilization.
Using
combination
with
database
~
40
studies
residue
were
tracked
into
MAOM,
found
that
predominantly
fuelled
by
produced
microbes
decomposing
POM—the
so-called
‘in
vivo’
pathway
relevance
higher
clayey
soils,
but
lower
rich
soils
poor
added
residues.
Overall,
our
space
proved
be
sound
tool
mechanistic
investigation
supported
current
understanding
critical
role
both
soils.
Generalized
model
including
dissolved
organic
matter
dynamicsC
and
N
are
transferred
between
POM
MAOM
compartments
partly
via
(DOM),
which
is
only
considered
implicitly
in
the
presented
main
text
(Fig.
1).In
this
appendix,
we
present
a
more
general
DOM
compartment,
show
simplifications
lead
to
used
text.To
construct
model,
assume
that
fraction
of
depolymerized
products
from
locally
by
respective
microbial
communities
(fractions
1
-
,
respectively)
'shared'
compartment
respectively).DOM
then
taken
up
both
according
rates
equilibrium
(i.e.,
⁄
≈
0)
because
it
small
C
with
relatively
fast
turnover
rates.Mathematically,
means
+
allows
simplifying
Eq.
(
1)-(
5)
obtain
described
(after
re-naming
=
).
EarthArXiv (California Digital Library),
Journal Year:
2024,
Volume and Issue:
unknown
Published: Feb. 13, 2024
Despite
the
importance
of
microbial
respiration
soil
organic
matter
(SOM)
in
regulating
carbon
flux
between
soils
and
atmosphere,
cycling
models
remain
primarily
based
on
climate
properties,
leading
to
large
uncertainty
predictions.
With
data
from
1000
Soils
Pilot
Molecular
Observation
Network
(MONet),
we
analyzed
high
resolution
water-extractable
SOM
profiles
standardized
cores
across
United
States
address
this
knowledge
gap.
Our
innovation
lies
using
machine
learning
distill
thousands
formula
into
tractable
units;
it
enables
integrating
molecular
measurements
models.
In
surface
soils,
chemistry
provided
better
estimates
potential
than
physicochemistry,
them
combined
yielded
best
prediction.
Overall,
identify
specific
subsets
molecules
that
may
improve
predictions
global
create
a
strong
basis
for
developing
new
representations
process-based