Abstract.
While
reforestation
in
water-limited
areas
has
increased
vegetation
coverage,
an
increasing
number
of
studies
have
reported
that
large-scale
plantations
are
suffering
from
tree
degradation,
which
is
characterized
by
short
trees,
small
size,
and
dieback.
Moreover,
the
changes
hydrological
processes
degraded
trees
within
soil-plant
system
remain
poorly
understood.
Here,
stable
isotope
method
(2H,
18O,
13C)
thermal
dissipation
technique
were
used
to
compare
soil
water
dynamics,
transpiration,
root
uptake
patterns,
intrinsic
water-use
efficiency
(WUEi)
Populus
simonii
under
different
degradation
degrees
(no
ND;
light
LD;
or
severe
SD)
2021
growing
season.
As
intensified,
weight
density
decreased
significantly
(P<0.05)
proportion
shallow
layer
(0–40
cm)
increased.
Influenced
precipitation
recharge,
volumetric
content
(SWC)
did
not
show
significant
differences
(P>0.05)
among
degrees.
The
SWC
middle
(40–80
deep
(80–200
layers
lower
ND
plot
than
LD
SD
plots.
Despite
SWC,
isotopic
characteristics
xylem
similar
ND,
LD,
Although
transpiration
plots
was
reduced
compared
plot,
main
depths
proportions
change.
P.
able
shift
source
process
wetting
drying.
healthy
WUEi
more
sensitive
SWC.
Our
study
shows
although
alleviate
exhaustion
reservoirs
some
extent,
sustainable
development
afforestation
ecosystems
requires
appropriate
stand
management
measures
maintain
balanced
forest-water
relationships.
Agricultural Water Management,
Год журнала:
2024,
Номер
296, С. 108799 - 108799
Опубликована: Март 28, 2024
Poplar
plantations
play
an
active
role
in
windbreak
and
sand-fixation
timber
production
water-limited
areas,
but
the
large-scale
are
experiencing
degradation,
characterized
by
short
trees,
small
size,
dieback.
Moreover,
potential
impacts
of
plantation
degradation
on
ecohydrological
processes
soil-plant
systems
remain
unclear.
We
continuously
measured
soil
water
content
(SWC),
hydrogen
oxygen
isotopic
compositions
plant
xylem
water,
carbon
leaf,
sap
flow
velocity
poplar
trees
under
various
degraded
(no
degraded,
ND;
lightly
LD;
severely
SD)
during
2021
growing
season
(May–September).
also
investigated
tree
root
at
a
depth
0–200
cm.
Our
results
showed
that
as
intensified,
weight
density
different
depths
decreased
proportion
shallow
layer
(0–40
cm)
increased.
Although
SWC
did
not
change
plantations,
SWCs
middle
(40–80
deep
(80–200
were
higher
LD
SD
than
ND
which
might
be
related
to
reduced
transpiration
plantations.
The
Bayesian
mixing
model
all
can
shift
source
from
layers
process
wetting
drying.
Evidence
leaf
isotopes
suggested
increased
sensitivity
intrinsic
water-use
efficiency
SWC.
findings
demonstrate
normal
growth
is
prone
desiccation
due
high
demand
alleviate
depletion
low
transpiration.
For
rain-fed
proper
thinning
measures
reducing
evaporation
may
necessary
avoid
excess
consumption
soils.