The Science of The Total Environment,
Год журнала:
2023,
Номер
905, С. 166921 - 166921
Опубликована: Сен. 12, 2023
Future
global
climate
changes
are
expected
to
increase
soil
organic
carbon
(SOC)
decomposition.
However,
the
combined
effect
of
C
inputs,
land
use
changes,
and
on
SOC
turnover
is
still
unclear.
Exploring
this
SOC-climate-land
interaction
allows
us
understand
stabilization
mechanisms
examine
whether
can
act
as
a
source
or
sink
for
CO2.
The
current
study
estimates
sequestration
potential
in
topsoil
layer
Danish
agricultural
lands
by
2038,
considering
change
future
scenarios
using
Rothamsted
Carbon
(RothC)
model.
Additionally,
we
quantified
loss
vulnerability
existing
projected
based
capacity
stabilize
OC.
We
used
quantile
random
forest
model
estimate
initial
stock
2018,
simulated
with
RothC
business-as-usual
(BAU)
scenario
crop
rotation
(LUC)
under
conditions
2038.
compared
stocks
saturation
deficit.
ranged
from
10
181
Mg
ha-1
different
parts
country.
projections
showed
8.1
BAU
6
after
LUC
adoption.
This
was
strongly
influenced
warmer
temperatures
clay
content.
proposed
became
mitigation
measure
against
negative
accumulation,
especially
sandy
soils
high
livestock
density.
A
accumulation
C-saturated
suggests
an
non-complexed
SOC,
which
vulnerable
being
lost
into
atmosphere
With
these
results,
provide
information
prioritize
areas
where
management
practices
be
adopted
enhance
stable
forms
preserve
labile-existing
stocks.
SOIL,
Год журнала:
2025,
Номер
11(1), С. 149 - 174
Опубликована: Фев. 5, 2025
Abstract.
Land
planning
projects
aiming
to
maximize
soil
organic
carbon
(SOC)
stocks
are
increasing
in
number
and
scope,
often
line
with
the
objective
reach
neutrality
by
2050.
In
response,
a
rising
of
studies
assesses
where
additional
SOC
could
be
stored
over
regional
global
spatial
scales.
order
provide
realistic
values
transferrable
beyond
scientific
community,
providing
targets
accrual
should
consider
timescales
needed
them,
taking
into
consideration
effects
C
inputs,
type,
depth
on
dynamics.
This
research
was
conducted
320
km2
territory
north-eastern
France,
eight
contrasted
types
have
been
identified,
characterized,
mapped
thanks
high
density
fully
described
profiles.
Continuous
profiles
were
interpolated
for
each
type
land
use
(cropland,
grassland,
or
forest).
We
defined
potential
using
percentile
boundary
lines
used
linear
model
depth-dependent
dynamics
explore
inputs
necessary
those
within
25
years.
also
from
literature
input
scenarios
provided
maps
stocks,
maximum
accrual,
highly
heterogenous
region
study.
Median
range
78–333
tC
ha−1.
Maximum
varies
19
ha−1
forested
Leptosols
197
grassland
Gleysols.
The
simulated
years
whole
study
one-fifth
accrual.
Further
different
is
therefore
storage
relevant
public
policies
approach
Soil Security,
Год журнала:
2021,
Номер
5, С. 100018 - 100018
Опубликована: Окт. 13, 2021
Soil
Security
includes
dimensions,
soil
capability,
condition,
capital,
connectivity
and
codification
(the
"five
C's").
This
article
provides
a
short
review
on
how
mapping,
digital
mapping
monitoring
systems
(SM,
DSM
SMS)
over
large
areas
contribute
to
these
five
C's
at
scales
ranging
from
country
globe.
Changes
the
evolution
in
aims
of
SM,
SMS
were
driven
both
by
main
issues
related
policy
priorities
associated
advances
science
technology.
shows
that
can
provide
basis
for
assessing
capability
condition
areas,
especially
if
we
assume
mainly
depends
rather
stable
attributes.
Repeated
or
are
appropriated
tool
monitor
changes
scales.
They
may
even
allow
capability.
However,
broad-scale
have
not
yet
fully
achieved
provision
information
concerning
delivery
some
functions
soil-based
ecosystem
services.
Although
significant
progress
estimating
capital
dimension
security
has
been
achieved,
there
is
need
capital.
Broad-scale
great
potential
increase
connectivity.
The
challenge
adapting
our
language
communication
target
audience.
There
encouraging
initiatives
enhance
codification.
Codification
largely
political
agenda,
still
an
urgent
connectivity,
towards
citizens,
NGOs
policy-makers.
Outlook on Agriculture,
Год журнала:
2022,
Номер
51(1), С. 91 - 104
Опубликована: Фев. 21, 2022
Clearing
natural
vegetation
to
establish
arable
agriculture
(cropland)
almost
invariably
causes
a
loss
of
soil
organic
carbon
(SOC).
Is
it
possible
restore
that
continues
in
the
pre-clearance
SOC
level
through
modified
management
practices?
To
address
this
question
we
reviewed
evidence
from
long-term
experiments
at
Rothamsted
Research,
UK,
Bad
Lauchstädt,
Germany,
Sanborn
Field,
USA
and
Brazil
both
surveys
farmers’
fields
Ethiopia,
Australia,
Zimbabwe,
UK
Chile.
In
most
cases
content
under
cropping
was
range
38–67%
values.
Returning
crop
residues,
adding
manures
or
including
periods
pasture
within
rotations
increased
this,
often
60–70%
initial
Under
tropical
climatic
conditions
after
clearance
particularly
rapid,
e.g.
>50%
less
than
10
years
smallholder
Zimbabwe.
If
larger
yielding
crops
were
grown,
using
fertilizers,
maize
stover
returned
instead
being
grazed
by
cattle,
reduced.
An
important
exception
general
trend
clearing
Cerrado
on
highly
weathered
acidic
soils
conversion
with
soybean.
Other
exceptions
unrealistically
large
annual
applications
manure
long
SOC-retentive
volcanic
soil.
Also,
introducing
irrigated
low
rainfall
region
can
increase
beyond
value
due
plant
biomass
production.
For
reasons
sustainability
health
is
maintain
as
high
practically
soils,
but
conclude
vast
majority
situations
unrealistic
expect
global
stocks
consider
more
reduce
current
rates
land
sustainably
produce
necessary
food
existing
agricultural
land.
Biogeosciences,
Год журнала:
2023,
Номер
20(8), С. 1559 - 1586
Опубликована: Апрель 19, 2023
Abstract.
Soil
organic
carbon
(SOC)
is
the
largest
terrestrial
pool.
SOC
composed
of
a
continuous
set
compounds
with
different
chemical
compositions,
origins,
and
susceptibilities
to
decomposition
that
are
commonly
separated
into
pools
characterised
by
responses
anthropogenic
environmental
disturbance.
Here
we
map
contribution
three
fractions
total
content
Australia's
soils.
The
fractions,
mineral-associated
(MAOC),
particulate
(POC),
pyrogenic
(PyOC),
represent
composition
distinct
turnover
rates,
chemistry,
pathway
formation.
Data
for
MAOC,
POC,
PyOC
were
obtained
near-
mid-infrared
spectral
models
calibrated
measured
fractions.
We
transformed
data
using
an
isometric-log-ratio
(ilr)
transformation
account
closed
compositional
nature
resulting
back-transformed
ilr
components
mapped
across
Australia.
fraction
stocks
0–30
cm
derived
maps
concentration,
bulk
density,
coarse
fragments,
soil
thickness.
Mapping
was
done
quantile
regression
forest
fitted
ilr-transformed
large
variables
as
predictors.
along
quantified
uncertainty
show
unique
spatial
pattern
in
MAOC
dominated
average
59
%
±
17
%,
whereas
28
13
11
POC.
allocation
(TOC)
increased
depth.
vulnerability
(i.e.
POC/[MAOC+PyOC])
greater
areas
Mediterranean
temperate
climates.
TOC
distribution
among
most
influential
uncertainty.
Further,
diversity
climatic
pedological
conditions
suggests
mechanisms
will
control
stabilisation
dynamics
continent,
shown
model
covariates'
importance
metric.
estimated
(0–30
cm)
be
Pg
2
5
PyOC,
which
consistent
previous
estimates.
their
can
used
modelling
forecasting
changes
response
land
use
change,
management,
climate
change.
Biogeosciences,
Год журнала:
2021,
Номер
18(13), С. 3981 - 4004
Опубликована: Июль 2, 2021
Abstract.
The
4
per
1000
initiative
aims
to
maintain
and
increase
soil
organic
carbon
(SOC)
stocks
for
fertility,
food
security,
climate
change
adaptation
mitigation.
One
way
enhance
SOC
is
(C)
inputs
the
soil.
In
this
study,
we
assessed
amount
of
C
that
are
necessary
reach
a
target
by
‰
yr−1
on
average,
30
years,
at
14
long-term
agricultural
sites
in
Europe.
We
used
Century
model
simulate
required
level
additional
these
sites.
Then,
analyzed
how
would
under
future
scenarios
temperature
increase.
Initial
were
simulated
assuming
steady
state.
compared
modeled
different
treatments
experimental
(exogenous
matter
addition
one
treatment
with
crop
rotations).
was
calibrated
fit
control
plots,
i.e.
conventional
management
without
from
exogenous
or
changes
rotations,
able
reproduce
stock
dynamics.
found
that,
average
among
selected
sites,
annual
will
have
43.15
±
5.05
%,
which
0.66
0.23
MgCha-1yr-1
(mean
standard
error),
respect
initial
treatment.
input
lower
than
similar
actually
majority
experiments.
However,
might
be
overestimating
effect
stocks.
At
increasing
0.25
%
average.
This
means
much
higher.
Furthermore,
estimated
even
more
due
warming,
54
120
1
5
∘C
respectively.
showed
depended
linearly
stocks,
raising
concern
feasibility
objective
soils
higher
potential
contribution
sequestration,
high
Our
work
highlights
challenge
large
scale
warmer
climate.
Agriculture,
Год журнала:
2022,
Номер
12(2), С. 170 - 170
Опубликована: Янв. 25, 2022
Carbon
sequestration
has
been
proposed
as
a
way
to
mitigate
the
impact
of
CO2
on
climate.
At
COP21,
‘4
per
1000
Soils
for
Food
Security
and
Climate’
initiative
was
launched
with
goal
increase
global
soil
organic
carbon
(SOC)
stocks
by
4‰
year.
The
Thyrow
long-term
field
experiment
DIV.2
chosen
determine
feasibility
this
4
under
dry
sandy
conditions
in
Eastern
Germany.
effects
different
fertilizing
regimes
SOC
contents
winter
rye
yields
were
investigated.
Winter
is
representative
crop
region
grown
monoculture
experiment.
achieved
all
treatments
including
unfertilized
control,
although
ploughing
takes
place
straw
removed
every
highest
up
0.5
t
ha−1
a−1
provided
combination
mineral
manure
fertilization.
In
three
out
four
years,
no
yield
difference
observed
between
mineral-only
fertilization
(120
kg
N)
N
(97.4
plant
available
Yields
increased
over
years
treatment
pure
decreased
other
treatments.
European Journal of Soil Science,
Год журнала:
2022,
Номер
73(6)
Опубликована: Ноя. 1, 2022
Abstract
Soils
store
vast
amounts
of
carbon
(C)
on
land,
and
increasing
soil
organic
(
SOC
)
stocks
in
already
managed
soils
such
as
croplands
may
be
one
way
to
remove
C
from
the
atmosphere,
thereby
limiting
subsequent
warming.
The
main
objective
this
study
was
estimate
amount
additional
input
needed
annually
increase
by
4‰
at
16
long‐term
agricultural
experiments
Europe,
including
exogenous
matter
EOM
additions.
We
used
an
ensemble
six
models
ran
them
under
two
configurations:
(1)
with
default
parametrization
(2)
parameters
calibrated
site‐by‐site
fit
evolution
control
treatments
(without
).
compared
model
simulations
analysed
factors
generating
variability
across
models.
able
reproduce
stock
unfertilised
treatments.
found
that,
average,
experimental
sites
1.5
±
1.2
Mg
ha
−1
year
per
over
30
years,
(multi‐model
median
standard
deviation
sites).
That
is,
a
119%
control.
While
mean
annual
temperature,
initial
had
significant
effect
predicted
configuration
(i.e.,
relative
mean),
only
water‐related
variables
precipitation
potential
evapotranspiration)
explained
divergence
between
when
calibrated.
Our
work
highlights
challenge
agriculture
accentuates
need
increasingly
lean
multi‐model
ensembles
predicting
trends
related
processes.
To
reliability
future
climate
change,
we
suggest
developers
better
constrain
decomposition.
Highlights
feasibility
target
studied
experiments.
An
uncertainty
predictions.
On
average
sites,
conditions.
High
mainly
driven
variables.
Crop Science,
Год журнала:
2023,
Номер
63(3), С. 990 - 1018
Опубликована: Янв. 31, 2023
Abstract
There
is
interest
in
harnessing
cropland
C
storage
potential
at
a
large
scale
to
mitigate
climate
change
and
improve
land
productivity.
While
the
effects
of
soil
management
practices
on
have
been
studied
extensively,
opportunities
select
for
sequestration
traits
crop
plants
remain
largely
unexplored.
This
review
describes
how
genetic
improvement
major
US
crops
may
altered
stocks
historically
identifies
plant
breeding
increase
stocks.
Through
quantitative
literature
review,
we
find
that
has
led
an
aboveground
residue
inputs
corn
(
Zea
mays
L.)
soybeans
Glycine
max
(L.)
Merr)
decrease
wheat
Triticum
aestivum
L.
turgidum
L.).
Breeding
not
root:shoot
ratio
these
crops.
Given
there
limited
further
improvements
harvest
index,
high
grain
yields
necessitate
increasing
biomass
production
future.
Crop
root
quality
influence
stabilization
crop‐derived
soil,
but
uncertainty
regarding
historical
changes
due
breeding,
magnitude
their
effect
organic
stocks,
tradeoffs
or
synergies
with
yield.
Nevertheless,
such
as
suberin
content,
rhizodeposition,
mycorrhizal
association,
depth
emerge
targets
more
efficient
stabilization.
also
opportunity
enhance
performance
cover
crops,
double
perennial
grains,
groundcovers,
which
can
annual
by
occupying
fallow
periods.
Our
reveals
are
many
fix
cropping
systems
its
meet
goals
sustainable
intensification
capture.