Differential contributions of microbial necromass to humic acid during composting of organic wastes
Environmental Research,
Journal Year:
2025,
Volume and Issue:
unknown, P. 121036 - 121036
Published: Feb. 1, 2025
Language: Английский
Nitrogen-induced acidification increases soil organic carbon accrual by promoting particulate organic carbon and microbial necromass under long-term experiment in the paddy soils of East China
Zhaoming Chen,
No information about this author
Qiang Wang,
No information about this author
Jinchuan Ma
No information about this author
et al.
Research Square (Research Square),
Journal Year:
2025,
Volume and Issue:
unknown
Published: March 27, 2025
Abstract
Background
and
aims
Nitrogen
(N)
addition
can
substantially
affect
soil
carbon
cycling
in
agroecosystems.
Microbial
necromass
(MNC)
is
widely
recognized
as
a
key
contributor
to
organic
C
(SOC)
fractions.
However,
the
mechanisms
underlying
responses
of
MNC
SOC
fractions
N
fertilization
paddy
soils
remain
unclear.
Methods
A
field
experiment
with
four
rates,
namely,
0,
300,
450,
600
kg
ha
–1
yr
–1
was
conducted
determine
effects
on
fractions,
microbial
(MNC),
enzyme
activity,
biomass
rice–wheat
rotation.
Results
increased
POC
concentrations
by
2.88–8.41%
14.6–41.2%,
respectively,
but
did
not
MAOC.
The
ratio
MAOC
reduced
addition,
indicating
that
decreased
stability.
concentration
7.32–22.5%
its
contribution
4.14–13.7%.
activity
β-1,4-
N-acetyl-glucosaminidase
decreased,
while
activities
leucine
amino
peptidase
acid
phosphatase
were
under
P
addition.
Structural
equation
modeling
random
forest
revealed
N-induced
decrease
pH
promoted
accrual
increasing
root
biomass,
consequently
improving
POC.
Conclusions
likely
more
vulnerable
than
acidification
primary
driver
for
promoting
soils.
Language: Английский
Aggregate Size Mediated the Changes in Soil Microbial Communities After the Afforestation of a Former Dryland in Northwestern China
Diversity,
Journal Year:
2024,
Volume and Issue:
16(11), P. 696 - 696
Published: Nov. 13, 2024
Although
the
afforestation
of
former
arable
lands
is
a
common
global
land-use
conversion,
its
impact
on
soil
microbial
communities
at
aggregate
scale
has
not
been
adequately
addressed.
In
this
study,
samples
were
categorized
into
large
macroaggregates
(LM,
>2
mm),
small
(SM,
2–0.25
and
microaggregates
(MI,
<0.25
mm)
to
assess
changes
in
composition,
diversity,
network
complexity,
stability
within
aggregates
after
dryland
northwestern
China.
The
results
revealed
that
enhanced
relative
abundance
Actinobacteriota,
Chloroflexi,
Ascomycota,
Mortierellomycota
aggregates,
suggesting
these
phyla
may
have
greater
advantages
post-afforestation.
Shannon–Wiener
Pielou
indices
for
bacterial
showed
no
significant
differences
between
types
across
all
fractions.
However,
alpha
diversity
fungal
LM
SM
significantly
increased
afforestation.
Bray–Curtis
dissimilarity
altered
beta
MI
but
had
minimal
three
topological
features
cross-kingdom
co-occurrence
networks
generally
exhibited
decreasing
trend
post-afforestation,
indicating
simplification
community
structure.
reduced
robustness
fractions
implies
also
destabilized
structure
macroaggregates.
composition
correlated
closely
with
carbon
nitrogen
contents,
especially
two
macroaggregate
linkages
suggests
improved
resource
conditions
could
be
key
driver
behind
shifts
following
Our
findings
indicate
ecology
can
better
understood
by
fractionation.
Language: Английский