Ecohydrology,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Oct. 2, 2024
ABSTRACT
Viticulture
is
an
essential
sector
in
agriculture
as
wine
production
plays
a
vital
role
the
socio‐economic
life
of
many
countries,
especially
Mediterranean
area.
Grapevines
are
valuable,
long‐lived
species
able
to
grow
hot
and
dry
regions.
We
currently
do
not
know
whether
rain‐fed
grapevines
entirely
rely
on
deep
soil
water
or
make
substantial
use
shallow
from
summer
precipitation
events.
Without
knowing
this,
we
poorly
understand
what
fraction
inputs
contributes
grapevine
transpiration.
This
has
implications
for
how
quantify
grapevine‐relevant
budgets
predicting
impacts
climate
change
grape
production.
investigated
vineyard
Chianti
region,
central
Italy.
During
growing
season
2021,
monitored
moisture
at
30‐
60‐cm
depth.
collected
over
250
samples
stable
isotope
analysis
rainfall,
soil,
plants.
Since
traditional
plant
sampling
problematic
grapevines,
shoots,
leaves,
condensed
leaf
transpiration
after
sealed
plastic
bags
were
wrapped
around
shoot.
these
alternative
reconstruct
isotopic
signal
xylem
infer
plant's
seasonal
origin
throughout
season.
The
revealed
that,
season,
received
disproportional
contributions
by
rain
that
had
fallen
winter,
even
when
compensating
Only
late
did
amounts
whose
contribution
occasionally
became
dominant.
These
results
provide
better
understanding
ecohydrological
interactions
uptake
dynamics
valuable
agroecosystems
such
vineyards.
Abstract
The
analysis
of
the
stable
isotopic
composition
hydrogen
and
oxygen
in
water
samples
from
soils
plants
can
help
to
identify
sources
vegetation
uptake.
This
approach
requires
that
heterogeneous
nature
plant
soil
matrices
is
carefully
accounted
for
during
experimental
design,
sample
collection,
extraction
analyses.
comparability
shortcomings
different
methods
extracting
analyzing
have
been
discussed
specialized
literature.
Yet,
despite
insightful
comparisons
benchmarking
methodologies
laboratories
worldwide,
community
still
lacks
a
roadmap
guide
extraction,
analyses,
many
practical
issues
potential
users
remain
unresolved:
example,
which
(soil
or
plant)
pool(s)
does
extracted
represent?
These
constitute
hurdle
implementation
by
newcomers.
Here,
we
summarize
discussions
led
framework
COST
Action
WATSON
(“WATer
isotopeS
critical
zONe:
groundwater
recharge
transpiration”—CA19120).
We
provide
guidelines
(1)
sampling
material
analysis,
(2)
laboratory
situ
(3)
measurements
composition.
highlight
importance
considering
process
chain
as
whole,
design
minimize
biased
estimates
relative
contribution
conclude
acknowledging
some
limitations
this
methodology
advice
on
collection
key
environmental
parameters
prior
article
categorized
under:
Science
Water
>
Hydrological
Processes
Environmental
Change
Extremes
Ecohydrology,
Journal Year:
2022,
Volume and Issue:
15(3)
Published: March 16, 2022
Abstract
The
stable
isotopes
of
hydrogen
and
oxygen
in
xylem
water
are
often
used
to
investigate
tree
sources.
But
this
traditional
approach
does
not
acknowledge
the
contribution
stored
phloem
transpiration
how
may
affect
source
interpretations.
Additionally,
there
is
a
prevailing
assumption
that
no
isotope
fractionation
during
transport.
Here,
we
systematically
sampled
at
daily
subdaily
resolutions
large
lysimeter
planted
with
Salix
viminalis
.
Stem
diurnal
change
storage
rates
were
also
measured.
Our
results
show
significantly
less
enriched
heavy
than
water.
At
resolution,
observed
larger
isotopic
difference
between
refilling
under
periods
deficit.
These
findings
contrast
expectation
heavy‐isotope
due
downward
transport
leaf
signatures.
Because
previous
evidence
aquaporin
mediated
higher
osmotic
permeability
lighter
isotopologues
across
aquaporins,
propose
radial
xylem–phloem
boundary
drive
relative
depletion
their
enrichment
xylem.
Hydrology and earth system sciences,
Journal Year:
2022,
Volume and Issue:
26(13), P. 3673 - 3689
Published: July 14, 2022
Abstract.
Recent
tracer-based
studies
using
stable
isotopes
of
hydrogen
and
oxygen
showed
that
different
methods
for
extracting
water
from
plant
tissues
can
return
isotopic
compositions
due
to
the
presence
organic
compounds
because
they
extract
domains.
One
most
used
is
cryogenic
vacuum
distillation
(CVD),
which
tends
total
water.
Conversely,
Scholander-type
pressure
chamber
(SPC),
commonly
by
tree
physiologists
measure
potential
in
determine
stress,
expected
only
more
mobile
(i.e.,
xylem
inter-cellular
water).
However,
few
reported
application
SPC
analyses,
therefore,
inter-method
comparisons
between
CVD
are
great
value.
In
this
work,
we
analyzed
variability
composition
extracted
CVD,
also
considering
signature
various
leaves,
twig
without
bark,
with
close
trunk
tree,
wood
core)
species
alder,
apple,
chestnut,
beech).
The
extraction
simple,
be
carried
out
field,
it
does
not
require
specific
laboratory
work
as
case
CVD.
main
limitation
very
small
volume
lignified
twigs
under
stress
conditions
compared
Our
results
indicated
were
significantly
different.
difference
obtained
two
was
smaller
beech
samples
chestnut
samples.
enriched
δ2H
δ18O,
respectively,
than
We
conclude
an
alternative
mostly
extracts
water,
whereas
retrieve
all
stored
sampled
tissue
both
living
dead
cells.
aiming
quantify
relative
contribution
soil
sources
transpiration
should
rely
on
(which
theoretically
SPC)
(sampled
CVD),
contains
a
fraction
could
longer
time.
Hydrological Processes,
Journal Year:
2023,
Volume and Issue:
37(1)
Published: Jan. 1, 2023
Abstract
Understanding
the
relative
importance
of
different
water
sources
that
replenish
soil
storage
is
necessary
to
assess
vulnerability
sub‐arctic
areas
changes
in
climate
and
altered
rain
snow
conditions,
reflected
timing
magnitude
infiltration.
We
examine
spatiotemporal
variability
seasonal
origin
at
soil‐vegetation
interface
Pallas
catchment,
located
northern
Finland.
The
field
study
was
conducted
from
May
2019
June
2020
over
two
snowmelt
seasons
one
summer
growing
season.
sampled
cores
up
a
1‐m
depth
stem
dominant
tree
species
four
sites
forests
forested
peatlands
for
stable
isotopes.
Seasonal
rainfall
variation
late
events
were
well
identifiable
well‐drained
soils
areas,
while
this
input
signal
heavily
attenuated
wetter,
peatland
areas.
Spatiotemporal
forest
similar,
whereas
controlled
by
extent
hydrologic
connectivity
adjoining
pools.
A
mixture
both
winter
precipitation
present
during
entire
period,
mineral
showed
an
ephemeral
response
got
nearly
fully
flushed
twice
hydrological
year.
Meltwater
after
early
spring
but
became
displaced
isotopically
enriched
summer.
evolution
pools
not
dynamics
offset
between
isotopic
signals
less
pronounced
peatlands.
This
data
set
uncovered
high
depth‐resolution,
quantifying
replenishing
sustaining
conditions.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(2), P. 599 - 612
Published: Jan. 30, 2023
Abstract.
The
stable
oxygen
(δ18Oleaf)
and
hydrogen
(δ2Hleaf)
isotopes
of
leaf
water
act
as
a
bridge
that
connects
the
hydroclimate
to
plant-derived
organic
matter.
However,
it
remains
unclear
whether
source
(i.e.,
twig
water,
soil
precipitation)
or
meteorological
parameters
temperature,
relative
humidity,
are
dominant
controls
on
δ18Oleaf
δ2Hleaf.
Here,
we
reported
seasonal
analysis
δ2Hleaf
together
with
from
potential
waters
along
an
elevation
transect
Chinese
Loess
Plateau.
We
found
values
were
more
closely
correlated
than
values,
whereas
similarly
transect.
Dual-isotope
showed
associated
because
their
similar
altitudinal
responses,
generating
well-defined
isotope
line
local
meteoric
(LMWL).
also
compared
measured
predicted
by
Craig–Gordon
model
no
significant
differences
between
them.
demonstrate
first-order
control
was
second-order
enrichment
biochemical
environmental
factors
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(4)
Published: March 22, 2021
Abstract
Closure
of
the
soil
water
balance
is
fundamental
to
ecohydrology.
But
closing
with
hydrometric
information
offers
no
insight
into
age
distribution
transiting
column
via
deep
drainage
or
combination
evaporation
and
transpiration.
This
a
major
challenge
in
our
discipline
currently;
tracing
needed
next
step.
Here
we
report
results
from
controlled
tracer
experiment
aimed
at
both
its
individual
components.
was
carried
out
on
2.5
m
3
lysimeter
planted
willow
tree.
We
applied
25
mm
isotopically
enriched
top
tracked
it
for
43
days
through
water,
bottom
drainage,
plant
xylem.
then
destructively
sampled
system
quantify
remaining
isotope
mass.
More
than
900
samples
were
collected
stable
analysis
trace
labeled
irrigation.
used
these
data
when
where
irrigation
became
source
uptake
percolation.
Evapotranspiration
dominated
outflow
(88%).
Tracing
transpiration
flux
showed
further
that
had
fallen
as
precipitation
1–2
months
prior.
The
breakthrough
complex
different
curves
observed
within
drainage.
Given
lack
direct
experimental
travel
time
transpiration,
provide
first
closure
all
relevant
outflows
are
traced.
Agricultural Water Management,
Journal Year:
2022,
Volume and Issue:
266, P. 107572 - 107572
Published: March 5, 2022
Improving
our
knowledge
on
the
relative
contribution
of
irrigation
water,
precipitation,
and
groundwater
to
tree
transpiration
is
necessary
for
an
efficient
sustainable
use
water
resources
in
agriculture.
For
this
purpose,
we
applied
deuterium
(2H)
enriched
trace
uptake
by
apple
trees
under
field
pot
conditions.
2H-enriched
was
supplied
Alpine
valley
mimicking
sprinkler
irrigation.
Labeled
infiltration
soil
presence
shoots
measured
over
a
week.
An
ancillary
experiment
using
potted
performed
elucidate
role
after
saturation
with
water.
Under
conditions,
infiltrated
maximum
depth
0.6
m,
where
most
fine
roots
were
present,
mixed
pre-irrigation
Sprinkler
taken
up
2–4
h
its
supply
shoot
content
increased
first
24
h,
then
it
leveled
off.
Tree
absorbed
from
layer
represented
average
48
±
3%
26
2%
total
axes
leaves,
respectively.
The
results
confirmed
allowed
us
speculate
that
conditions
(ca.
0.9
m
deep,
capillary
rise
expected
depth)
did
not
significantly
contribute
uptake.
Results
indicate
large
fraction
(52–74%)
derive
recent
uptake,
suggesting
rather
limited
mixing
within
organs.
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.
Plant Cell & Environment,
Journal Year:
2022,
Volume and Issue:
46(1), P. 133 - 149
Published: Oct. 28, 2022
The
isotopic
composition
of
xylem
water
(δX
)
is
considerable
interest
for
plant
source
studies.
In-situ
monitored
transpired
(δT
could
provide
a
nondestructive
proxy
δX
-values.
Using
flow-through
leaf
chambers,
we
2-hourly
δT
-dynamics
in
two
tropical
species,
one
canopy-forming
tree
and
understory
herbaceous
species.
In
an
enclosed
rainforest
(Biosphere
2),
observed
response
to
experimental
severe
drought,
followed
by
2
H
deep-water
pulse
applied
belowground
before
starting
regular
rain.
We
also
sampled
branches
obtain
-values
from
cryogenic
vacuum
extraction
(CVE).
Daily
flux-weighted
δ18
OT
were
good
OX
under
well-watered
drought
conditions
that
matched
the
rainforest's
source.
Transpiration-derived
mostly
lower
than
CVE-derived
values.
δ2
HX
relatively
high
compared
consistently
higher
values
during
drought.
Tracing
real-time
showed
distinct
uptake
transport
responses:
fast
strong
contribution
deep
canopy
transpiration
contrasting
with
slow
limited
species
transpiration.
Thus,
in-situ
method
promising
tool
capture
rapid
dynamics
use
both
woody
nonwoody