Ecological Applications,
Год журнала:
2021,
Номер
31(7)
Опубликована: Июль 7, 2021
Abstract
Soil
fertility
in
organic
agriculture
relies
on
microbial
cycling
of
nutrient
inputs
from
legume
cover
crops
and
animal
manure.
However,
large
quantities
labile
carbon
(C)
nitrogen
(N)
these
amendments
may
promote
the
production
emission
nitrous
oxide
(N
2
O)
soils.
Better
ecological
understanding
N
O
controls
lead
to
new
management
strategies
reduce
emissions.
We
measured
soil
for
two
growing
seasons
four
corn–soybean–winter
grain
rotations
with
tillage,
crop,
manure
variations
typical
temperate
humid
North
America.
To
identify
pathways
mitigation
opportunities,
we
supplemented
flux
measurements
determinations
isotopomer
composition
microbiological
genomic
DNA
abundances
microplots
where
manipulated
crop
additions.
The
input
legume‐rich
prior
corn
planting
made
phase
main
source
emissions,
averaging
9.8
kg/ha
O‐N
representing
80%
3‐yr
rotations’
total
Nitrous
emissions
increased
sharply
when
exceeded
1.8
4
Mg/ha
(dry
matter),
respectively.
Removing
aboveground
biomass
before
prevent
co‐location
fresh
decreased
by
60%
during
phase.
co‐occurrence
peak
high
dioxide
suggests
that
oxygen
(O
)
consumption
likely
caused
hypoxia
bacterial
denitrification.
This
interpretation
is
supported
site
preference
values
trending
towards
denitrification
limited
reduction,
as
revealed
δ
15
18
decrease
clade
I
nosZ
gene
abundance
following
incorporation
Thus,
accelerated
seems
be
a
critical
control
systems
additions
decomposable
C
substrates.
Because
many
agricultural
rely
combined
legumes
manures,
our
research
controlling
rate
timing
additions,
well
preventing
manure,
could
mitigate
Frontiers in Microbiology,
Год журнала:
2023,
Номер
13
Опубликована: Янв. 12, 2023
Biogenic
nitrous
oxide
(N2O)
from
nitrification
and
denitrification
in
agricultural
soils
is
a
major
source
of
N2O
the
atmosphere,
its
flux
changes
significantly
with
soil
moisture
condition.
However,
quantitative
relationship
between
production
different
pathways
(i.e.,
vs.
denitrification)
content
remains
elusive,
limiting
our
ability
predicting
future
emissions
under
changing
environment.
This
study
quantified
rates
various
conditions
using
laboratory
incubation
combined
literature
synthesis.
15N
labeling
approach
was
used
to
differentiate
eight
contents
ranging
40
120%
water-filled
pore
space
(WFPS)
study,
while
80
groups
data
17
studies
across
global
were
collected
Results
showed
that
as
increased,
first
increased
then
decreased,
peak
occurring
95%
WFPS.
By
contrast,
dominant
pathway
switched
60
70%
Furthermore,
synthetic
elucidated
driver
controlling
relative
contributions
production,
NH4
+
NO3
-
concentrations
mainly
determined
each
pathway.
The
treatments
broad
narrow
gradient
required
capture
comprehensive
response
rate
change,
essential
for
accurately
emission
climate
change
scenarios.
Biogeosciences,
Год журнала:
2016,
Номер
13(16), С. 4789 - 4809
Опубликована: Авг. 29, 2016
Abstract.
This
paper
summarizes
currently
available
data
on
greenhouse
gas
(GHG)
emissions
from
African
natural
ecosystems
and
agricultural
lands.
The
are
used
to
synthesize
current
understanding
of
the
drivers
change
in
GHG
emissions,
outline
knowledge
gaps,
suggest
future
directions
strategies
for
emission
research.
were
collected
75
studies
conducted
22
countries
(n
=
244)
sub-Saharan
Africa
(SSA).
Carbon
dioxide
(CO2)
by
far
largest
contributor
global
warming
potential
(GWP)
SSA
terrestrial
systems.
CO2
ranged
3.3
57.0
Mg
ha−1
yr−1,
methane
(CH4)
−4.8
3.5
kg
yr−1
(−0.16
0.12
equivalent
(eq.)
yr−1),
nitrous
oxide
(N2O)
−0.1
13.7
(−0.03
4.1
eq.
yr−1).
Soil
physical
chemical
properties,
rewetting,
vegetation
type,
forest
management,
land-use
changes
all
found
be
important
factors
affecting
soil
In
aquatic
systems,
was
total
ranging
5.7
232.0
followed
−26.3
2741.9
CH4
(−0.89
93.2
yr−1)
0.2
N2O
(0.06
1.0
Rates
systems
affected
location,
hydrological
characteristics,
water
quality.
croplands,
also
dominated
CO2,
1.7
141.2
with
−1.3
66.7
(−0.04
2.3
0.05
112.0
(0.015
33.4
(EFs)
0.01
%.
Incorporation
crop
residues
or
manure
inorganic
fertilizers
invariably
resulted
significant
but
results
inconsistent
as
magnitude
direction
differed
gas.
vegetable
gardens
73.3
132.0
53.4
177.6
(15.9
52.9
EFs
3
4
agroforestry
38.6
26.7
8.0
respectively.
Improving
fallow
nitrogen
(N)-fixing
trees
led
increased
compared
conventional
croplands.
type
quality
plant
residue
is
an
control
how
affected.
Throughout
lands,
slowly
N
inputs
below
150
exponentially
application
rates
up
300
yr−1.
lowest
yield-scaled
reported
between
100
ha−1.
Overall,
lands
56.9
±
12.7
×
109
contributing
76.3
23.7
%,
Additional
measurements
urgently
required
reduce
uncertainty
annual
different
land
uses
identify
major
mitigation
options
low-emission
development.
A
common
strategy
addressing
this
gap
may
include
identifying
priorities
acquisition,
utilizing
appropriate
technologies,
involving
international
networks
collaboration.
Environmental Research Letters,
Год журнала:
2020,
Номер
16(2), С. 024004 - 024004
Опубликована: Дек. 12, 2020
The
potent
greenhouse
gas
nitrous
oxide
(N2O)
is
accumulating
in
the
atmosphere
at
unprecedented
rates
largely
due
to
agricultural
intensification,
and
cultivated
soils
contribute
∼60%
of
flux.
Empirical
models
N2O
fluxes
for
intensively
managed
cropping
systems
are
confounded
by
highly
variable
limited
geographic
coverage;
process-based
biogeochemical
rarely
able
predict
daily
monthly
emissions
with
>20%
accuracy
even
site-specific
calibration.
Here
we
show
promise
machine
learning
(ML)
significantly
improve
field-level
flux
predictions,
especially
when
coupled
a
model
simulate
unmeasured
soil
parameters.
We
used
sub-daily
data
from
six
years
automated
chambers
installed
continuous
corn
rotation
site
upper
US
Midwest
(∼3000
observations),
supplemented
weekly
biweekly
manual
chamber
measurements
(∼1100
fluxes),
train
an
ML
that
explained
65%–89%
variance
very
few
input
variables—soil
moisture,
days
after
fertilization,
texture,
air
temperature,
carbon,
precipitation,
nitrogen
(N)
fertilizer
rate.
When
applied
long-term
test
not
model,
38%
variation
observed
corn,
51%
upon
coupling
predicted
N
availability.
This
represents
two
three
times
improvement
over
conventional
substantially
fewer
requirements.
approach
offers
better
predictions
thus
more
precise
global
effective
mitigation
interventions.
Global Change Biology,
Год журнала:
2018,
Номер
24(5), С. 1843 - 1872
Опубликована: Фев. 5, 2018
Central
European
grasslands
are
characterized
by
a
wide
range
of
different
management
practices
in
close
geographical
proximity.
Site-specific
strategies
strongly
affect
the
biosphere-atmosphere
exchange
three
greenhouse
gases
(GHG)
carbon
dioxide
(CO2
),
nitrous
oxide
(N2
O),
and
methane
(CH4
).
The
evaluation
environmental
impacts
at
site
level
is
challenging,
because
most
situ
measurements
focus
on
quantification
CO2
exchange,
while
long-term
N2
O
CH4
flux
ecosystem
scale
remain
scarce.
Here,
we
synthesized
,
O,
fluxes
from
14
managed
grassland
sites,
quantified
eddy
covariance
or
chamber
techniques.
We
found
that
were
average
sink
(-1,783
to
-91
g
m-2
year-1
but
source
(18-638
-eq.
either
(-9
488
net
GHG
balance
(NGB)
nine
sites
where
all
GHGs
available
was
between
-2,761
-58
with
emissions
offsetting
concurrent
uptake
21
±
6%
across
sites.
only
positive
NGB
for
one
during
restoration
year
ploughing.
predictive
power
soil
parameters
generally
low
varied
considerably
within
years.
However,
after
site-specific
data
normalization,
identified
conditions
indicated
enhanced
source/sink
activity
("sweet
spots")
gave
good
prediction
normalized
overall
application
animal
slurry
increased
emissions.
O-N
emission
factor
1.8
0.5%,
among
years
(0.1%-8.6%).
Although
led
emissions,
strength
dominant
component
annual
budget.
Proceedings of the National Academy of Sciences,
Год журнала:
2021,
Номер
118(46)
Опубликована: Ноя. 8, 2021
Agricultural
landscapes
are
the
largest
source
of
anthropogenic
nitrous
oxide
(N2O)
emissions,
but
their
specific
sources
and
magnitudes
remain
contested.
In
US
Corn
Belt,
a
globally
important
N2O
source,
in-field
soil
emissions
were
reportedly
too
small
to
account
for
measured
in
regional
atmosphere,
disproportionately
high
from
intermittent
streams
have
been
invoked
explain
discrepancy.
We
collected
3
y
high-frequency
(4-h)
measurements
across
topographic
gradient,
including
very
poorly
drained
(intermittently
flooded)
depression
adjacent
upland
soils.
Mean
annual
this
corn-soybean
rotation
(7.8
kg
N2O-N
ha-1⋅y-1)
similar
previous
top-down
estimate,
regardless
landscape
position.
Synthesizing
other
Belt
studies,
we
found
mean
5.6
ha-1⋅y-1
soils
with
drainage
our
transect
(moderately
well-drained
drained),
which
collectively
comprise
60%
corn-soybean-cultivated
contrast,
strictly
averaged
only
2.3
Our
results
imply
that
moderately
severely
impaired
values
not
representative
broader
Belt.
On
basis
carbon
dioxide
equivalents,
warming
effect
direct
was
twofold
greater
than
optimistic
gains
achievable
agricultural
practice
changes.
Despite
recent
focus
on
sequestration,
addressing
wet
may
leverage
achieving
climate
sustainability.
Abstract
To
investigate
the
effect
of
nitrification
inhibitors
(NIs)
3,4-dimethylpyrazole
phosphate
(DMPP)
and
3-methylpyrazole
1,2,4-triazole
(3MP
+
TZ),
on
N
2
O
emissions
yield
from
a
typical
vegetable
rotation
in
sub-tropical
Australia
we
monitored
soil
fluxes
continuously
over
an
entire
year
using
automated
greenhouse
gas
measurement
system.
The
temporal
variation
showed
only
low
cropping
phases,
but
significantly
higher
were
observed
post-harvest
accounting
for
50–70%
annual
emissions.
NIs
reduced
by
20–60%
phases;
however,
this
mitigation
was
offset
elevated
treatments
fallow
period.
Annual
conventional
fertiliser,
DMPP
treatment,
3MP
TZ
treatment
1.3,
1.1
1.6
(sem
=
0.2)
kg-N
ha
−1
,
respectively.
This
study
highlights
that
use
systems
can
lead
to
storing
profile
is
available
microbes
during
decomposition
residues.
Hence
has
be
treated
carefully
fertiliser
rates
need
adjusted
avoid
oversupply
phase.
Global Change Biology,
Год журнала:
2016,
Номер
22(11), С. 3594 - 3607
Опубликована: Авг. 11, 2016
Differences
in
soil
nitrous
oxide
(N2
O)
fluxes
among
ecosystems
are
often
difficult
to
evaluate
and
predict
due
high
spatial
temporal
variabilities
few
direct
experimental
comparisons.
For
20
years,
we
measured
N2
O
11
southwest
Michigan
USA:
four
annual
grain
crops
(corn-soybean-wheat
rotations)
managed
with
conventional,
no-till,
reduced
input,
or
biologically
based/organic
inputs;
three
perennial
(alfalfa,
poplar,
conifers);
unmanaged
of
different
successional
age
including
mature
forest.
Average
emissions
were
higher
from
N-fixing
cropping
systems
than
nonleguminous
low
across
ecosystems.
Among
full-rotation
indistinguishable
one
another
but
rotation
phase
mattered.
example,
those
cover
fertilizer
N
emitted
more
during
the
corn
soybean
phases,
wheat
~40%
lower.
Likewise,
no-till
did
not
differ
conventional
tillage
over
entire
~20%
increased
30-80%
phases.
Greenhouse
gas
intensity
for
(flux
per
unit
yield)
was
lowest
soybeans
produced
under
management,
while
other
crop
×
management
combinations
intensities
similar
another.
fertilized
systems,
ranged
0.30
1.33
kg
O-N
ha-1
yr-1
best
predicted
by
IPCC
Tier
1
ΔEF
emission
factor
approaches.
Annual
cumulative
explained
NO3-
pools
(r2
=
0.72)
so
crops,
where
differences
overrode
simple
correlations.
Daily
poorly
any
variables.
Overall,
long-term
measurements
reveal
lower
nonlegume
vegetation
and,
conservatively
overriding
influence
on
fluxes.