Carbon dioxide fluxes and carbon budget of a sugarcane ecosystem with crop residue returning in South China
Zhuoting Li,
Qiangsheng Xu,
Wenting Ning
и другие.
Field Crops Research,
Год журнала:
2025,
Номер
322, С. 109744 - 109744
Опубликована: Янв. 9, 2025
Язык: Английский
Refining snow-streamflow dynamics in a Tibetan Plateau basin by incorporating snow depth and topography
Journal of Hydrology,
Год журнала:
2025,
Номер
unknown, С. 133057 - 133057
Опубликована: Март 1, 2025
Язык: Английский
Influence of Groundwater Depth on Salt Migration and Maize Growth in the Typical Irrigation Area
Agronomy,
Год журнала:
2025,
Номер
15(5), С. 1021 - 1021
Опубликована: Апрель 24, 2025
Groundwater
depth
has
a
significant
impact
on
salinization
in
irrigated
areas.
In
this
study,
different
groundwater
depths
were
controlled
via
pit
tests
and
we
conducted
with
(DGWs)
to
investigate
the
relationship
between
irrigation
water
volume
salt
migration
during
crop
growth
period,
as
well
influence
of
DGW
maize
yield.
The
aim
study
was
determine
an
appropriate
for
Hetao
Irrigation
District,
largest
area
Asia,
under
dual
goals
conservation
control.
results
showed
that
upward
replenishment
179.60
mm,
139.17
119.98
68.62
48.38
mm
each
respective
DGW,
i.e.,
negatively
correlated
period.
Soil
electrical
conductivity
(EC)
exponentially
related
DGW.
For
DGWs
>
1.75
m,
surface
soil
EC
decreased
significantly
exhibited
less
variation
Moreover,
desalination
rate
after
improved
at
values
2.00
m
2.25
m.
Shallow
resulted
increased
evapotranspiration
intensified
stress,
which
reduced
use
efficiency.
To
reduce
resource
waste
stress
crops,
suggest
2.00~2.25
is
more
suitable
development.
These
provide
reference
determining
salinized
Язык: Английский
Stable isotopes reveal soil evaporation and its controlling factors in the Heihe River source area on the northeastern Qinghai-Tibetan Plateau
Journal of Hydrology Regional Studies,
Год журнала:
2024,
Номер
54, С. 101901 - 101901
Опубликована: Июль 29, 2024
The
Heihe
River
source
area
in
the
Northeastern
Qinghai-Tibetan
Plateau,
China.
Soil
evaporation,
which
is
a
key
process
soil
water
loss,
influenced
by
various
environmental
factors.
However,
identification
of
its
main
drivers
on
large
scale
alpine
mountains
remains
challenging
due
to
sampling
constraints.
This
study
examined
spatial
distribution
evaporation
and
control
factors
during
growing
season
area.
results
indicated
that
represented
lc-excess
values,
gradually
increased
from
southeast
northwest,
then
decreased,
reaching
depth
50
cm
below
surface.
Although
normalized
difference
vegetation
index
explained
54
%
variation
interaction
between
land
surface
temperature
content
(SWC)
provided
more
robust
explanation.
losses
exhibited
following
pattern:
cropland
>
grassland
forest
shrubland.
In
shrubland,
SWC
precipitation
68
73.3
variations
respectively.
Grassland
mainly
relied
SWC,
with
49.33
unexplained
variability
Meanwhile,
aridity
aspect
45
44.6
cropland.
These
findings
invaluable
information
for
advancing
our
understanding
ecohydrological
processes
mountains.
Язык: Английский
Eddy covariance measurements reveal a decreased carbon sequestration strength 2010–2022 in an African semiarid savanna
Global Change Biology,
Год журнала:
2024,
Номер
30(9)
Опубликована: Сен. 1, 2024
Abstract
Monitoring
the
changes
of
ecosystem
functioning
is
pivotal
for
understanding
global
carbon
cycle.
Despite
its
size
and
contribution
to
cycle,
Africa
largely
understudied
in
regard
ongoing
their
responses
climate
change.
One
reasons
lack
long‐term
situ
data.
Here,
we
use
eddy
covariance
quantify
net
exchange
(NEE)
components—gross
primary
production
(GPP)
respiration
(
R
eco
)
years
2010–2022
a
Sahelian
semiarid
savanna
study
trends
fluxes.
Significant
negative
were
found
NEE
(12.7
±
2.8
g
C
m
2
year
−1
),
GPP
(39.6
7.9
(32.2
8.9
).
We
that
decreased
by
60%
over
period,
this
decrease
was
mainly
caused
stronger
rainy
season
than
.
Additionally,
observed
strong
increasing
vapor
pressure
deficit,
but
no
rainfall
or
soil
water
content.
Thus,
proposed
explanation
sink
strength
atmospheric
dryness.
The
warming
Sahel,
coupled
with
evaporative
demand,
may
thus
lead
levels
across
biome,
lowering
CO
sequestration.
Язык: Английский