Geophysical Research Letters,
Journal Year:
2024,
Volume and Issue:
51(8)
Published: April 10, 2024
Abstract
Changes
are
projected
for
the
boreal
biome
with
complex
and
variable
effects
on
forest
vegetation
including
drought‐induced
tree
mortality
loss.
With
soil
atmospheric
conditions
governing
drought
intensity,
specific
drivers
of
trees
water
stress
can
be
difficult
to
disentangle
across
temporal
scales.
We
used
wavelet
analysis
causality
detection
identify
potential
environmental
controls
(evapotranspiration,
moisture,
rainfall,
vapor
pressure
deficit,
air
temperature
photosynthetically
active
radiation)
daily
deficit
longer
periods
dehydration
in
black
spruce
tamarack.
Daily
was
controlled
by
radiation,
temperature,
causing
greater
stand
evapotranspiration.
Prolonged
(multi‐day)
were
regulated
radiation
moisture.
provide
empirical
evidence
that
continued
warming
drying
will
cause
short‐term
increases
tamarack
transpiration,
but
reduced
availability.
Biogeosciences,
Journal Year:
2022,
Volume and Issue:
19(17), P. 4315 - 4329
Published: Sept. 12, 2022
Abstract.
Droughts
affect
terrestrial
ecosystems
directly
and
concurrently
can
additionally
induce
lagged
effects
in
subsequent
seasons
years.
Such
legacy
of
drought
on
vegetation
growth
state
have
been
widely
studied
tree
ring
records
satellite-based
greenness,
while
legacies
ecosystem
carbon
fluxes
are
still
poorly
quantified
understood.
Here,
we
focus
two
monitoring
sites
central
Germany
with
a
similar
climate
but
characterised
by
different
species
age
structures.
Using
eddy
covariance
measurements,
detect
gross
primary
productivity
(GPP)
calculating
the
difference
between
random
forest
model
estimates
potential
GPP
observed
GPP.
Our
results
showed
that,
at
both
sites,
droughts
caused
significant
seasonal
annual
timescales,
which
were
partly
explained
reduced
leaf
development.
The
reduction
due
to
is
comparable
magnitude
concurrent
differed
neighbouring
forests
divergent
methodology
proposed
here
allows
quantification
temporal
dynamics
sub-seasonal
scale
separation
from
uncertainties.
application
larger
range
will
help
us
quantify
whether
identified
lag
general
factors
they
may
depend.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(8), P. 2073 - 2092
Published: April 27, 2022
Abstract.
Root
water
uptake
(RWU)
is
an
important
critical
zone
process,
as
plants
can
tap
various
sources
and
transpire
these
back
into
the
atmosphere.
However,
knowledge
about
spatial
temporal
dynamics
of
RWU
associated
at
both
high
resolution
(e.g.
daily)
over
longer
time
periods
seasonal)
still
limited.
We
used
cavity
ring-down
spectroscopy
(CRDS)
for
continuous
in
situ
monitoring
stable
isotopes
soil
xylem
two
riparian
willow
(Salix
alba)
trees
growing
season
(May
to
October)
2020.
This
was
complemented
by
isotopic
sampling
local
precipitation,
groundwater,
stream
order
help
constrain
potential
RWU.
A
eddy
flux
tower,
together
with
sap
flow
monitoring,
moisture
measurements,
dendrometry,
also
provide
hydroclimatic
ecohydrological
contexts
isotope
monitoring.
In
addition,
respective
bulk
twig
samples
were
collected
corroborate
data.
The
period
characterised
frequent
inputs
interspersed
warm
dry
periods,
which
resulted
variable
storage
upper
20
cm
profile
dynamic
signatures.
variability
greatly
damped
40
cm,
composition
subsoil
groundwater
relatively
stable.
very
similar
those
soil,
analysis
using
a
Bayesian
mixing
model
inferred
that
overall
∼90
%
derived
from
profile.
while
signatures,
direct
equilibrium
method
showed
good
comparability
results,
water,
cryogenic
extractions
signatures
only
moderately
or
not
all
comparable.
Sap
dendrometry
data
indicated
availability
did
seriously
limit
transpiration
during
study
period,
though
it
seemed
deeper
(>40
cm)
provided
higher
proportion
(∼30
%)
drier
late
summer.
demonstrates
utility
prolonged
real-time
natural
abundance
soil–vegetation
systems,
has
great
further
understanding
partitioning
under
changing
conditions.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(1), P. 123 - 137
Published: Jan. 4, 2023
Abstract.
Stable
water
isotopes
have
been
used
extensively
to
study
the
use
strategy
of
plants
in
various
ecosystems.
In
deep
vadose
zone
(DVZ)
regions,
rooting
depth
trees
can
reach
several
meters
tens
meters.
However,
existence
roots
soils
does
not
necessarily
mean
occurrence
root
uptake,
which
usually
occurs
at
a
particular
time
during
growing
season.
Therefore,
quantifying
contribution
deep-layer
soil
(DLSW)
DVZ
regions
using
natural
abundance
stable
may
be
accurate
because
this
method
assumes
that
always
extract
shallow-
and
water.
We
propose
multi-step
for
addressing
issue.
First,
isotopic
labeling
layers
identifies
whether
absorb
DLSW
determines
layer
depths
from
derive
their
source.
Next,
we
calculate
sources
based
on
determined
above
quantify
trees.
also
compared
results
with
method.
The
11-
17-year-old
apple
were
taken
as
examples
analyses
China's
Loess
Plateau.
Isotopic
showed
uptake
11-year-old
reached
300
cm
blossom
young
fruit
(BYF)
stage
only
100
swelling
(FSW)
stage,
whereas
consumed
0–320
layer.
Overall,
absorbed
most
(>140
cm)
BYF
more
these
than
throughout
addition,
overestimated
DLSW,
especially
320–500
Our
findings
highlight
determining
helps
regions.
Ecohydrology,
Journal Year:
2024,
Volume and Issue:
17(2)
Published: Jan. 17, 2024
Abstract
In
ecohydrology,
water
isotopologues
are
used
to
assess
potential
sources
of
root
uptake
by
comparing
xylem
signatures
with
source
signatures.
Such
comparisons
affected
the
variability
and
uncertainty
isotope
plant
sources.
The
tree‐scale
stand‐scale
variabilities
in
stem
often
unknown
but
important
for
sampling
design
estimation
assessing
tree
uptake.
Here,
we
quantified
beech,
oak
spruce
trees
a
mature
forest
on
Swiss
plateau.
For
water,
sub‐daily
replicates
different
cardinal
directions
showed
no
systematic
differences,
found
differences
height.
observed
at
heights
along
suggests
that
residence
times
within
need
be
considered,
their
effects
compartments
(stem,
branches,
leaves).
Further,
concerning
hydrogen
signatures,
height‐
species‐specific
offsets
(SW‐excess
δ
2
H).
Stem
water's
was
similar
magnitude
its
smaller
than
branch
bulk
soil
around
each
tree.
Xylem
from
cores
close
ground,
therefore,
can
give
more
precise
estimate
isotopic
signal
most
recent
facilitate
accurate
attribution.
Hydrological Processes,
Journal Year:
2021,
Volume and Issue:
35(3)
Published: Feb. 6, 2021
Abstract
Source
water
apportionment
studies
using
the
dual
isotopes
of
oxygen
and
hydrogen
have
revolutionized
our
understanding
ecohydrology.
But
despite
these
developments—mostly
over
past
decade—many
technical
problems
still
exist
in
terms
linking
xylem
to
its
soil
groundwater
sources.
This
is
mainly
due
sampling
issues
possible
fractionation
water.
Here
we
explore
whether
or
not
leaf
alone
can
be
used
quantify
blend
rainfall
event
inputs
from
which
originates.
Leaf
has
historically
been
avoided
plant
uptake
extreme
processes
at
surface.
In
proof
concept
work
embrace
those
use
well‐known
Craig
Gordon
model
map
back
individual
precipitation
We
also
employ
a
Bayesian
uncertainty
estimation
approach
source
uncertainties.
show
this
controlled,
vegetated
lysimeter
experiment
where
were
able
correctly
identify
mean
seasonal
that
was
taken
up
by
plant,
with
an
typically
within
±
1‰
for
δ
18
O.
While
appropriate
all
studies,
shows
isotope
composition
may
provide
new,
relatively
un‐intrusive
method
addressing
questions
about
source.
Kastamonu University Journal of Forestry Faculty,
Journal Year:
2022,
Volume and Issue:
unknown, P. 1 - 16
Published: March 30, 2022
Aim
of
study:
Two-year-old
containerized
balsam
and
concolor
fir
one-year-old
Eastern
white
pine
transplants
were
grown
under
variable
watering
regimes
with
the
goal
identifying
plant
morphological
some
physiological
traits
water
stress.
Area
This
experiment
was
conducted
in
a
greenhouse
at
Tree
Research
Center
on
Michigan
State
University
campus,
East
Lansing,
Michigan.
Material
methods:
Relative
root
collar
diameter
(RRCD),
height
growth
(RHG),
length
(RRL)
measured
as
parameters.
Stem
potential
(Ψ),
stomatal
conductance
(gs),
net
photosynthetic
rate
(Anet),
intrinsic
use
efficiency
(iWUE=Anet/gs),
foliar
potassium
(K+),
calcium
(Ca+2)
concentration
traits.
Main
results:
Well-watered
had
significantly
higher
RRCD,
RHG,
RRL
species.
Balsam
Ψ
than
severe
Fir
species
Anet,
gs,
lower
iWUE
pine.
White
K+
concentration,
while
highest
Ca+2
concentration.
stress
due
to
their
ability
maintain
uptake
despite
reduced
soil
content.
Highlights:
It
is
concluded
that
has
better
drought
tolerance
because
withstand
through
mechanism
activities
growth,
minimize
loss,
increase
uptake.
One Earth,
Journal Year:
2023,
Volume and Issue:
6(3), P. 251 - 266
Published: March 1, 2023
Terrestrial
disturbances
are
increasing
in
frequency
and
severity,
perturbing
the
hydrologic
cycle
by
altering
vegetation-mediated
water
use
microclimate.
Here,
we
synthesize
literature
on
post-disturbance
ecohydrological
coupling,
including
mechanistic
relationship
between
vegetation
streamflow,
under
changing
disturbance
regimes,
atmospheric
CO2,
climate.
Disturbance
can
cause
decoupling
transpiration
streamflow
connectivity,
size,
availability,
spatial
distribution
of
their
source
pools.
Successional
trajectories
influence
dynamics
partitioning.
Changing
climate
regimes
alter
succession
prolong
decoupling.
Increasing
rates,
spread
along
with
warming
could
promote
greater
globally.
From
this
review
emerges
a
framework
testable
hypotheses
that
identify
critical
processes
regulating
coupling
provide
roadmap
for
future
research.
Accurate
prediction
requires
understanding
degree
hydraulic
connectivity
pools
response
to
regimes.
Water Resources Research,
Journal Year:
2025,
Volume and Issue:
61(1)
Published: Jan. 1, 2025
Abstract
Modeling
water
stable
isotope
transport
in
soil
is
crucial
to
sharpen
our
understanding
of
cycles
terrestrial
ecosystems.
Although
several
models
for
have
been
developed,
many
rely
on
a
semi‐coupled
numerical
approach,
solving
only
after
obtaining
solutions
from
and
heat
equations.
However,
this
approach
may
increase
instability
errors
model.
Here,
we
developed
an
algorithm
that
solves
one‐dimensional
water,
heat,
equations
with
fully
coupled
method
(MOIST).
Our
results
showed
MOIST
more
under
various
spatial
temporal
discretization
than
has
good
agreement
semi‐analytical
transport.
We
also
validated
long‐term
measurements
lysimeter
study
three
scenarios
hydraulic
parameters
calibrated
by
HYDRUS‐1D
the
first
two
last
scenario.
In
scenario
1,
overall
NSE
,
KGE
MAE
simulated
δ
18
O
0.47,
0.58,
0.92‰,
respectively,
compared
0.31,
0.60,
1.00‰
HYDRUS‐1D;
2,
these
indices
were
0.33,
0.52,
1.04‰,
0.19,
1.15‰
3,
exhibited
highest
(0.48)
(0.76),
smallest
(0.90)
among
all
scenarios.
These
findings
indicate
better
performance
simulating
flow
simplified
ecosystems
HYDRUS‐1D,
suggesting
great
potential
furthering
understandings
ecohydrological
processes
Frontiers in Forests and Global Change,
Journal Year:
2025,
Volume and Issue:
7
Published: Jan. 28, 2025
The
movement
of
water
between
xylem
and
inner
bark
(phloem
associated
tissues),
mostly
driven
by
potential
differences,
forms
a
key
part
the
diel
transpiration
cycle.
It
is
not
known
how
use
stored
in
at
cycle
may
influence
isotopic
composition
water.
Understanding
these
possible
effects
major
challenge
for
identification
tree
sources
interpretation
patterns
using
isotopes.
Here,
we
examined
variation
scale
assessed
this
varied
relation
to
traits
strategies
on
nine
species
tropical
rainforest
end
dry
season.
We
measured
δ
2
H
18
O
two
shallow
depths:
‘outer
xylem’
‘inner
(up
~0.5
cm
~
1
from
bark,
respectively)
collected
predawn,
morning
midday.
Considering
all
together,
average
outer
was
similar
predawn
midday,
suggesting
exchange
tissues
reflected
times,
but
differed
significantly
during
increased
transpiration.
Results
suggest
that
bark-xylem
throughout
affects
trees.
Furthermore,
variations
were
more
pronounced
deep-rooted,
isohydric
with
dense
wood
than
shallow-rooted,
anisohydric
low
density.
This
differences
related
hydraulic
reliance
bark-stored
across
buffer
changes
potential.
discuss
implications
interpreting
strategies.