Hydrological Processes,
Год журнала:
2024,
Номер
38(3)
Опубликована: Март 1, 2024
Abstract
Long‐term
data
are
crucial
for
understanding
ecological
responses
to
climate
and
land
use
change;
they
also
vital
evidence
informing
management.
As
a
migratory
fish,
Atlantic
salmon
sentinels
of
both
global
local
environmental
change.
This
paper
reviews
the
main
insights
from
six
decades
research
in
an
upland
Scottish
stream
(Girnock
Burn)
inhabited
by
spring
population
dominated
multi‐sea‐winter
fish.
Research
began
1960s
providing
census
returning
adults,
juvenile
emigrants
in‐stream
production
salmon.
Early
pioneered
new
monitoring
techniques
into
ecology
dynamics.
These
studies
underlined
need
interdisciplinary
approaches
interactions
with
physical,
chemical
biological
components
habitats
at
different
life‐stages.
highlighted
variations
catchment‐scale
hydroclimate,
hydrology,
geomorphology
hydrochemistry
as
essential
freshwater
wider
landscape
context.
Evolution
has
resulted
remarkable
catalogue
novel
findings
underlining
value
long‐term
that
increases
time
modelling
tools
advance
leverage
more
“big
data”.
Data
available
on
fish
numbers,
sizes
ages
across
multiple
life
stages,
extending
over
many
covering
wide
range
stock
levels.
Combined
unusually
detailed
characterization
environment,
these
have
enabled
unique
process‐based
controls
bottlenecks
dynamics
entire
lifecycle
consequences
declining
marine
survival
ova
deposition.
Such
powerful
datasets,
methodological
enhancements
resulting
process
informed
supported
development
assessment
which
been
applied
aid
management
threatened
stocks
large‐catchment,
regional
national
scales.
Many
pioneering
developed
internationally.
history
shows
importance
integrating
discovery
science
policy
assessing
efficacy
options.
It
demonstrates
continue
resource
sites,
act
focus
inter‐disciplinary
innovation,
where
overall
greatly
exceeds
costs
individual
component
parts.
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,
Год журнала:
2022,
Номер
26(15), С. 4125 - 4146
Опубликована: Авг. 8, 2022
Abstract.
Isotope-based
approaches
to
study
plant
water
sources
rely
on
the
assumption
that
root
uptake
and
within-plant
transport
are
non-fractionating
processes.
However,
a
growing
number
of
studies
have
reported
offsets
between
source
stable
isotope
composition
for
wide
range
ecosystems.
These
isotopic
can
result
in
erroneous
attribution
used
by
plants
potential
overestimations
groundwater
vegetation.
We
conducted
global
meta-analysis
quantify
magnitude
these
explored
whether
their
variability
could
be
explained
either
biotic
or
abiotic
factors.
Our
database
compiled
112
spanning
arctic
tropical
biomes
dual
(δ2H
δ18O)
(stem)
water,
including
soil
(sampled
following
various
methodologies
along
variable
depths).
calculated
2H
two
ways:
line
conditioned
excess
(LC-excess)
describes
deviation
from
local
meteoric
(SW-excess)
line,
each
sampling
campaign
within
study.
tested
effects
climate
(air
temperature
content),
class,
traits
(growth
form,
leaf
habit,
wood
density,
parenchyma
fraction
mycorrhizal
habit)
LC-excess
SW-excess.
Globally,
stem
was
more
depleted
than
(SW-excess
<
0)
3.02±0.65
‰
(P
0.05
according
estimates
our
linear
mixed
model
weighted
sample
size
studies).
In
95
%
cases
where
SW-excess
negative,
indicating
had
not
undergone
evaporative
enrichment
(such
as
groundwater)
unlikely
explain
observed
soil–plant
offsets.
Soil
class
did
any
significant
effect
negative
cold
wet
sites,
whereas
it
positive
warm
sites.
The
climatic
suggest
methodological
artefacts
sole
cause
results
would
imply
may
lead
inaccuracies
when
using
bulk
proxy
infer
sources.
Water Resources Research,
Год журнала:
2022,
Номер
58(9)
Опубликована: Авг. 30, 2022
Abstract
Studies
of
tree
water
source
partitioning
have
primarily
focused
on
the
growing
season.
However,
little
is
yet
known
about
transpiration
before,
during,
and
after
snowmelt
when
trees
rehydrate
recommence
in
spring.
This
study
investigates
use
during
spring
following
tree's
winter
stem
shrinkage.
We
document
three
boreal
forest
species—
Pinus
banksiana
,
Picea
mariana
Larix
laricina—
by
combining
observations
weekly
isotopic
signatures
(
δ
18
O
2
H)
xylem,
soil
water,
rainfall
with
measurements
moisture
dynamics,
snow
depth
high‐resolution
temporal
radius
changes
sap
flow.
Our
data
shows
that
onset
rehydration
overlaps
for
evergreens.
During
onset,
xylem
at
canopy
reflected
a
constant
pre‐melt
signature
likely
showing
late
fall
conditions.
As
infiltrates
recharges
matrix,
rapid
shift
to
depleted‐snowmelt
values.
While
there
was
an
overlap
between
timing,
values
did
not
onset.
showed
1–2‐week
delay
from
clear
snowmelt‐depleted
evergreen
species.
appears
be
controlled
transit
time
order
9–18
days.
key
Hydrological Processes,
Год журнала:
2023,
Номер
37(1)
Опубликована: Янв. 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.
Plant Cell & Environment,
Год журнала:
2024,
Номер
47(12), С. 5252 - 5264
Опубликована: Авг. 23, 2024
Long-term
pure
forest
(PF)
management
and
successive
planting
has
result
resulted
in
"low-efficiency
artificial
forests"
large
areas.
However,
controversy
persists
over
the
promoting
effect
of
introduction
broadleaf
tree
species
on
production
efficiency
PF.
This
study
hypothesised
that
introduced
can
significantly
promote
both
water-nutrient
use
gross
primary
productivity
(GPP)of
Tree
ring
chronologies,
water
source,
GPP
were
analysed
coniferous
Cunninghamia
lanceolata
broadleaved
Phoebe
zhennan
growing
past
three
decades.
The
P.
into
C.
plantations
inter-specific
competition
for
water,
probably
because
similarity
main
source
these
two
species.
absorbed
more
with
a
higher
nutrient
level
from
40-60-cm
soil
layer
mixed
forests
(MF).
Although
co-existing
limited
basal
area
increment
growth
rates
MF
plots,
acquisition
dissolved
nutrients
fertile
topsoil
enhanced;
this
increased
plots.
To
achieve
better
ecological
benefits
GPP,
MFs
should
be
constructed
southern
China.
Abstract
In
most
tree
species,
xylem
consists
of
two
different
functional
parts:
sapwood
and
heartwood.
While
sapwood,
as
the
flowpath
for
sap,
has
received
more
attention
in
isotope
studies
assessing
water
sources
accessed
by
trees
(e.g.
soil
from
depths,
groundwater,
stream
or
a
mixture
these),
much
remains
unknown
about
heartwood
possible
exchange
between
parts.
We
investigated
four
species
(
Fagus
sylvatica
,
Quercus
petraea
Pseudotsuga
menziesii
Picea
abies
)
characterised
anatomy
timing
physiological
activity
to
evaluate
degree
differentiation
isotopic
composition
on
biweekly
time
scale.
found
that
all
displayed
concurrent
variation
their
throughout
growing
season
day‐night
scale
suggesting
are
not
isolated
compartments.
parts
display
consistent
difference
conifers,
they
similar
values
broadleaved
higher
exchange.
Furthermore,
we
have
also
observed
progressive
change
with
sampling
depth
rather
than
xylem.
Our
study
highlights
value
accounting
radial
variation,
which
might
potentially
lead
uncertainties
concerning
origin
extracted
uptake
studies.
Hydrology and earth system sciences,
Год журнала:
2022,
Номер
26(8), С. 2073 - 2092
Опубликована: Апрель 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.
Water Resources Research,
Год журнала:
2022,
Номер
58(8)
Опубликована: Авг. 1, 2022
Abstract
Cryogenic
vacuum
extraction
(CVE)
has
been
considered
as
the
standard
technique
for
analysis
of
plant
water
stable
isotopes
in
ecohydrological
research.
Recent
studies
reported
that
CVE
can
introduce
significant
bias
isotope
analyses,
yet
causes
and
influencing
factors
CVE‐induced
deuterium
offsets
remain
poorly
understood.
Here,
we
performed
rehydration
experiments
on
samples
from
two
species
three
organs
with
distinct‐isotopic
spiking
waters.
Centrifugation
high‐pressure
mechanical
squeezing
were
used
to
separate
sap
tissue
analyses.
Plant
waters
extracted
by
differed
significantly
reference
δ
2
H,
but
not
18
O.
The
H
was
linearly
correlated
xylem
content,
this
relationship
is
affected
organs/species
isotopic
signature
water.
Moreover,
induced
(−8.52
±
0.90‰)
greater
than
difference
between
(−3.33
0.76‰)
apple
stems
possessing
similar
contents.
Thus,
hydrogen‐exchange
organics
water,
heterogeneity
within
plants
both
contribute
negative
bias,
former
dominant
cause.
multiple
governing
make
it
difficult
establish
a
unified
correction
equation.
Our
results
question
usefulness
cryogenic
extraction.