Reduced accrual of mineral-associated organic matter after two years of enhanced rock weathering in cropland soils, though no net losses of soil organic carbon
Biogeochemistry,
Journal Year:
2024,
Volume and Issue:
167(8), P. 989 - 1005
Published: July 23, 2024
Abstract
Enhanced
rock
weathering
(ERW),
the
application
of
crushed
silicate
to
soil,
can
remove
atmospheric
carbon
dioxide
by
converting
it
(bi)
carbonate
ions
or
solid
minerals.
However,
few
studies
have
empirically
evaluated
ERW
in
field
settings.
A
critical
question
remains
as
whether
additions
might
positively
negatively
affect
soil
organic
matter
(SOM)—Earth’s
largest
terrestrial
(C)
pool
and
a
massive
reservoir
nitrogen
(N).
Here,
three
irrigated
cropland
trials
California,
USA,
we
investigated
effect
meta-basalt
on
different
pools
(i.e.,
mineral-associated
matter,
MAOM,
particulate
POM),
active
microbial
biomass,
community
composition.
After
2
years
additions,
MAOM
stocks
were
lower
upper
surface
(0–10
cm)
plots
with
compared
unamended
control
plots.
At
sites
where
baseline
pre-treatment
data
available,
neither
total
SOC
nor
SON
decreased
over
study
accrual
rate
MAOM-C
MAOM-N
at
0–10
cm
was
vs.
controls.
Before
is
deployed
large
scales,
our
results
suggest
that
should
assess
effects
SOM
pools,
especially
multi-year
time
scales
environmental
contexts,
accurately
changes
net
C
understand
mechanisms
driving
interactions
between
cycling.
Language: Английский
Parameters of labile organic carbon as the indicators of the stability of soil organic matter under different land use
Soil and Water Research,
Journal Year:
2025,
Volume and Issue:
unknown
Published: Jan. 3, 2025
The
labile
fractions
of
organic
carbon
(OC),
which
are
a
reflection
the
properties
soil
and
its
use,
appear
to
be
suitable
parameters
for
their
use
as
indicators.
aim
this
study
was
determine
reliable
relatively
simple
indicators
detecting
chemical
physical
stabilizations
OC,
would
respond
sensitively
land
use.
includes
forest
ecosystem
(FE)
agroecosystem
(AE)
with
different
tillage
intensities
(reduced
tillage,
RT
conventional
CT)
on
real
farms.
Parameters
C
N
were
tested.
For
depth
<
0.1
m
in
FE,
hot
water
extractable
(HWEOC)
stabilization
nitrogen
(NL)
most
Higher
values
HWEOC
indicate
OC
by
decreasing
decomposition,
pH
or
increasing
carbonates,
recalcitrant
fractions,
higher
NL
incorporation
into
silt
fraction
larger
macro-aggregates.
In
AE
RT,
these
pool
index
(CPI)
lability
(LIC)
stabilization.
CPI
LIC
formation
size-optimal
dry-sieved
(DSA;
1–3
mm)
wet-sieved
(WSA;
1–2
aggregates.
CT,
it
NL.
Its
point
through
alkaline
cations,
size-fraction
>
0.01
mm
DSA
(1–3
mm).
0.3
AE,
CL
(for
RT),
value
points
clay
CT),
indicates
conditions
acidification.
Language: Английский
Impact of long-term drip irrigation on soil organic carbon and nutrient stocks in arid oasis farmlands
Weihao Sun,
No information about this author
Zhibin He,
No information about this author
Bing Liu
No information about this author
et al.
CATENA,
Journal Year:
2025,
Volume and Issue:
252, P. 108895 - 108895
Published: March 5, 2025
Language: Английский
Terracing stabilizes and enhances soil organic carbon sequestration benefits of revegetation on the Loess Plateau, China
Hui Cheng,
No information about this author
Hao Feng,
No information about this author
Xiaoping Zhang
No information about this author
et al.
CATENA,
Journal Year:
2025,
Volume and Issue:
255, P. 109018 - 109018
Published: April 9, 2025
Language: Английский
Reduced accrual of mineral-associated organic matter after two years of enhanced rock weathering in cropland soils, though no net losses of soil organic carbon
bioRxiv (Cold Spring Harbor Laboratory),
Journal Year:
2024,
Volume and Issue:
unknown
Published: June 27, 2024
Abstract
Enhanced
rock
weathering
(ERW),
the
application
of
crushed
silicate
to
soil,
can
remove
atmospheric
carbon
dioxide
by
converting
it
(bi)carbonate
ions
or
solid
carbonate
minerals.
However,
few
field
studies
have
empirically
evaluated
ERW
in
settings.
A
critical
question
remains
as
whether
additions
might
positively
negatively
affect
soil
organic
matter
(SOM)
–
Earth’s
largest
terrestrial
(C)
pool
and
a
massive
reservoir
nitrogen
(N).
Here,
three
irrigated
cropland
sites
California,
USA,
we
investigated
effect
meta-basalt
on
different
pools
(i.e.,
mineral-associated
particulate
matter),
active
microbial
biomass,
community
composition.
After
two
years
additions,
(MAOM)
stocks
were
lower
upper
surface
(0-10
cm)
compared
unamended
controls.
At
where
baseline
pre-treatment
data
available,
neither
total
SOC
nor
SON
decreased
over
study
control
plots.
accrual
rate
MAOM-C
MAOM-N
at
0-10
cm
was
plots
with
vs.
Before
is
deployed
large
scales,
our
results
suggest
that
trials
should
assess
effects
SOM
pools,
especially
multi-year
time
accurately
changes
net
C
understand
mechanisms
driving
interactions
between
cycling.
Language: Английский
Biochar affects soil properties over 1 m depth in an alkaline soil of north China Plain
Xiongxiong Bai,
No information about this author
Jiao Tang,
No information about this author
Qingwei Lin
No information about this author
et al.
Journal of Environmental Management,
Journal Year:
2024,
Volume and Issue:
370, P. 123097 - 123097
Published: Oct. 30, 2024
Language: Английский
Ecosystem Carbon Stock in Iron-Metamorphic Soils with Different Types of Land Use in South Karelia
Eurasian Soil Science,
Journal Year:
2024,
Volume and Issue:
57(10), P. 1567 - 1578
Published: Oct. 1, 2024
Language: Английский
Geographic Distribution Pattern Determines Soil Microbial Community Assembly Process in Acanthopanax senticosus Rhizosphere Soil
Mingyu Wang,
No information about this author
Xiangyu Xing,
No information about this author
Youjia Zhang
No information about this author
et al.
Microorganisms,
Journal Year:
2024,
Volume and Issue:
12(12), P. 2506 - 2506
Published: Dec. 4, 2024
The
geographic
distribution
patterns
of
soil
microbial
communities
associated
with
cultivated
Acanthopanax
senticosus
plants
in
Northeast
China
were
investigated.
High-throughput
sequencing
revealed
that
the
diversity
and
community
assembly
bacterial
fungal
inter-root
varied
significantly
location.
study
found
predominantly
assembled
through
stochastic
processes
at
most
sites,
while
showed
greater
variation,
both
deterministic
involved.
complexity
bacterial-fungal
co-occurrence
networks
also
longitude
latitude,
demonstrating
positive
negative
interactions.
PICRUSt
2.0
FUNGuild
used
to
predict
potential
functions
microbiota,
respectively,
during
different
land
use
patterns.
average
taxonomic
distinctness
(AVD)
index
indicated
varying
degrees
stability
across
sites.
Key
taxa
contributing
variability
identified
Random
Forest
modeling,
Bacteriap25
Sutterellaceae
standing
out
among
bacteria,
Archaeorhizomyces
Clavaria
fungi.
Soil
chemical
properties,
including
pH,
TN,
TP,
EC,
SOC,
correlated
diversity,
composition,
networks.
Structural
equation
modeling
directly
indirectly
influenced
properties
communities.
Overall,
provides
insights
into
A.
highlights
need
for
further
research
underlying
mechanisms
shaping
these
Language: Английский