Elucidating
the
response
of
soil
gross
nitrogen
(N)
transformations
to
fires
could
improve
our
understanding
how
fire
affects
N
availability
and
loss.
Yet,
internal
transformation
rates
respond
remains
unexplored
globally.
Here,
we
investigate
general
its
consequences
for
The
results
showed
that
increased
mineralization
rate
(GNM;
+38%)
ammonium
concentration
(+47%)
as
a
result
decreased
C/N
ratio
but
microbial
nitrate
immobilization
(
Forests,
Journal Year:
2023,
Volume and Issue:
14(8), P. 1531 - 1531
Published: July 27, 2023
Global
warming
has
a
significant
impact
on
soil
carbon
dioxide
(CO2)
and
methane
(CH4)
fluxes
in
temperate
forests.
However,
due
to
lack
of
field
observations,
limited
information
is
available
about
the
responses
CO2
CH4
changes
temperature
during
non-growing
season
throughout
year
The
broadleaf
Korean
pine
mixed
mature
forest
(MF)
adjacent
secondary
white
birch
(BF)
at
different
succession
stages
Changbai
mountain
region
northeastern
China
were
selected,
study
effect
situ
column
translocation
On
average,
air
5
cm
depth
under
BF
stands
from
October
2018
2022
increased
by
0.64
0.42
°C
0.49
0.43
year,
respectively,
compared
with
those
MF
stands.
Based
multi-year
measurements
experiments,
it
was
shown
that
season,
columns
ranged
0.004
1.175
0.015
1.401
(averages
0.321
0.387)
μmol
m−2
s−1,
−1.003
0.048
−1.037
−0.013
−0.179
−0.250)
nmol
accounting
for
approximately
20.8%
25.3%,
48.8%
69.1%
corresponding
average
growing
season.
When
undisturbed
transferred
stand,
simulate
warming,
cumulative
emissions
uptake
23.5%
15.3%
9.5%
16.3%
across
respectively.
when
cooling,
decreased
16.9%
0.1%
Upon
21.8%
but
15.4%
year.
moisture
could
explain
84–86%
variability
16–51%
two
measurement
period.
results
experiments
highlight
small
climate
nature
can
increase
forests
China,
particularly
which
should
be
considered
predicting
C
global
scenarios.
Biogeosciences,
Journal Year:
2024,
Volume and Issue:
21(8), P. 2005 - 2028
Published: April 24, 2024
Abstract.
Forest
ecosystems
play
an
important
role
in
the
global
carbon
(C)
budget
by
sequestering
a
large
fraction
of
anthropogenic
dioxide
(CO2)
emissions
and
acting
as
methane
(CH4)
sinks.
The
forest-floor
greenhouse
gas
(GHG;
CO2,
CH4,
nitrous
oxide
(N2O))
flux,
i.e.,
from
soil
understory
vegetation,
is
one
major
components
to
consider
when
determining
C
or
GHG
forests.
Although
winter
fluxes
are
essential
determine
annual
budget,
only
very
few
studies
have
examined
long-term,
year-round
fluxes.
Thus,
we
aimed
(i)
quantify
seasonal
variations
fluxes;
(ii)
evaluate
their
drivers,
including
effects
snow
cover,
timing,
amount
snowmelt;
(iii)
calculate
budgets
for
subalpine
spruce
forest
Switzerland.
We
measured
during
4
years
with
four
automatic
chambers
at
ICOS
Class
1
Ecosystem
station
Davos
(CH-Dav).
applied
random
models
investigate
environmental
drivers
gap-fill
flux
time
series.
floor
emitted
2336
g
CO2
m−2
yr−1
(average
over
years).
Annual
respiration
responded
most
strongly
temperature
depth.
No
response
leaf
area
index
photosynthetic
photon
density
was
observed,
suggesting
strong
direct
control
factors
weak,
even
lacking,
indirect
canopy
biology.
Furthermore,
consistent
CH4
sink
(−0.71
yr−1),
driven
mainly
Winter
were
less
(6.0
%–7.3
%),
while
contributed
substantially
(14.4
%–18.4
%).
N2O
low
(0.007
negligible
our
site.
In
2022,
warmest
year
on
record
below-average
precipitation
site,
observed
substantial
increase
compared
other
years.
mean
indicated
2319
±
200
eq.
(mean
standard
deviation
(SD)
all
years),
dominating
offsetting
small
proportion
(0.8
%)
emissions.
Due
relevance
recommend
measurements
high
temporal
resolution.
future
increasing
temperatures
cover
due
climate
change,
expect
increased
this
site
modulating
ecosystem.
Elucidating
the
response
of
soil
gross
nitrogen
(N)
transformations
to
fires
could
improve
our
understanding
how
fire
affects
N
availability
and
loss.
Yet,
internal
transformation
rates
respond
remains
unexplored
globally.
Here,
we
investigate
general
its
consequences
for
The
results
showed
that
increased
mineralization
rate
(GNM;
+38%)
ammonium
concentration
(+47%)
as
a
result
decreased
C/N
ratio
but
microbial
nitrate
immobilization
(