Authorea (Authorea),
Journal Year:
2024,
Volume and Issue:
unknown
Published: March 27, 2024
Hyporheic
zones
regulate
biogeochemical
processes
in
streams
and
rivers,
but
high
spatiotemporal
heterogeneity
makes
it
difficult
to
predict
how
these
scale
from
individual
reaches
river
basins.Recent
work
applying
allometric
scaling
(i.e.,
power-law
relationships
between
size
function)
networks
provides
a
new
paradigm
develop
scalable
understanding
of
hyporheic
processes.We
used
reach-scale
aerobic
respiration
estimates
explore
patterns
across
two
basins,
related
watershed
characteristics.We
found
consistent
behaviors
at
lowest
highest
exchange
flux
(HEF)
quantiles,
HEF-dependent
elevation,
precipitation,
land-cover.Our
results
also
suggest
variability
allometry
for
middle
relation
findings
provide
initial
evidence
that
may
be
useful
predicting
dynamics
watersheds
reach
basin
scales.
Scientific
Significance
Statement:The
zone
is
control
point
like
are
important
determinants
move
process
carbon
nutrients.However,
the
characterized
by
spatial
heterogeneity,
which
functions
change
scales.This
study
applies
theory,
suggests
function
scales
predictable
way
with
size,
determine
if
area
basins
contrasting
some
tool
transferable
knowledge
note
site-specific
constrain
generalizability
this
method
other
regions
watersheds.
Abstract
Rising
water
temperatures
in
rivers
due
to
climate
change
are
already
having
observable
impacts
on
river
ecosystems.
Warming
has
both
direct
and
indirect
aquatic
life,
further
aggravates
pervasive
issues
such
as
eutrophication,
pollution,
the
spread
of
disease.
Animals
can
survive
higher
through
physiological
and/or
genetic
acclimation,
behavioral
phenological
change,
range
shifts
more
suitable
locations.
As
such,
those
animals
that
adapted
cool‐water
regions
typically
found
high
altitudes
latitudes
where
there
fewer
dispersal
opportunities
most
at
risk
future
extinction.
However,
sub‐lethal
animal
physiology
phenology,
body‐size,
trophic
interactions
could
have
significant
population‐level
effects
elsewhere.
Rivers
vulnerable
warming
because
historic
management
left
them
exposed
solar
radiation
removal
riparian
shade,
hydrologically
disconnected
longitudinally,
laterally,
vertically.
The
resilience
riverine
ecosystems
is
also
limited
by
anthropogenic
simplification
habitats,
with
implications
for
resource
use
resident
organisms.
Due
complex
ecosystems,
species‐specific
response
organisms
warming,
predicting
how
will
challenging.
Restoring
provide
connectivity
heterogeneity
conditions
would
a
expected
co‐occurring
pressures,
including
should
be
considered
priority
part
global
strategies
adaptation
mitigation.
This
article
categorized
under:
Science
Water
>
Environmental
Change
Life
Nature
Freshwater
Ecosystems
Stresses
Pressures
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(1)
Published: Jan. 1, 2024
Abstract
Non‐perennial
streams,
which
lack
year‐round
flow,
are
widespread
globally.
Identifying
the
sources
of
water
that
sustain
flow
in
non‐perennial
streams
is
necessary
to
understand
their
potential
impacts
on
downstream
resources,
and
guide
policy
management.
Here,
we
used
isotopes
(δ
18
O
δ
2
H)
two
different
modeling
approaches
investigate
spatiotemporal
dynamics
young
fractions
(
F
yw
)
a
stream
network
at
Konza
Prairie
(KS,
USA)
during
2021
summer
dry‐down
season,
as
well
over
several
years
with
varying
hydrometeorological
conditions.
Using
Bayesian
model,
found
substantial
amount
:
39.1–62.6%)
sustained
flows
headwaters
catchment
outlet
year,
while
2015–2022
contributions
estimated
using
sinusoidal
models
indicated
smaller
amounts
(15.3%
±
5.7).
Both
indicate
releases
highly
sensitive
hydrological
conditions,
shifting
older
dries.
The
shift
age
suggests
away
from
rapid
fracture
toward
slower
matrix
creates
but
localized
surface
presence
late
reflected
annual
outlet.
proportion
highlights
vulnerability
short‐term
hydroclimatic
change,
reveals
sensitivity
longer‐term
changes
groundwater
dynamics.
Combined,
this
local
may
propagate
through
networks
influence
availability
quality.
Hydrology and earth system sciences,
Journal Year:
2023,
Volume and Issue:
27(3), P. 809 - 836
Published: Feb. 15, 2023
Abstract.
Persistent
surface
water
pools
along
non-perennial
rivers
represent
an
important
resource
for
plants,
animals,
and
humans.
While
ecological
studies
of
these
features
are
not
uncommon,
rarely
accompanied
by
a
rigorous
examination
the
hydrological
hydrogeological
characteristics
that
create
or
support
persistent
river
pools.
Here
we
present
overarching
framework
understanding
hydrology
Perched
water,
alluvial
throughflow,
groundwater
discharge
key
hydraulic
mechanisms
control
persistence
channels.
Groundwater
can
be
further
categorized
into
controlled
geological
contact
barrier
topography.
Emphasis
is
put
on
clearly
defining
throughflow
different
drivers
discharge.
The
suite
regional-scale
pool-scale
diagnostic
tools
available
elucidating
summarized
critiqued.
Water
fluxes
to
supported
vary
spatially
temporally,
quantitatively
resolving
pool
balance
components
commonly
non-trivial.
This
allows
evaluation
susceptibility
channels
changes
in
climate
withdrawals.
Finally,
demonstrate
application
this
using
conduct
regional
assessment
Hamersley
Basin
north-western
Australia.
Abstract
Climate
change
is
interacting
with
water
resource
pressures
to
alter
the
frequency,
severity
and
spatial
extent
of
drought,
which
can
thus
no
longer
be
considered
a
purely
natural
hazard.
Although
particularly
severe
ecological
impacts
drought
have
occurred
in
drylands,
its
effects
on
temperate
ecosystems,
including
rivers,
are
also
considerable.
Extensive
research
spanning
diverse
range
UK
rivers
offers
an
opportunity
place
past
context
intensifying
climate
examine
likely
future
typically
cool,
wet
country.
Here,
manifests
instream
as
deficits
surface
water,
modified
flow
velocities,
and—increasingly—partial
or
complete
drying
previously
perennial
naturally
non‐perennial
reaches.
As
result,
causes
declines
taxonomic
functional
biodiversity
freshwater
communities
microorganisms,
algae,
plants,
invertebrates
fish,
altering
processes
associated
benefits
people.
recovered
quickly
after
previous
droughts,
increase
extremity
may
compromise
recovery
following
events.
The
risk
droughts
that
push
ecosystems
beyond
thresholds
persistent,
species‐poor,
functionally
simplified
states
increasing.
Research
monitoring
needed
enable
timely
identification
approaching
such
inform
interventions
pull
these
back
from
brink.
Management
actions
support
regimes
promote
diversify
habitats,
refuges,
crucial
within
river
they
adapt
changing
world.
This
article
categorized
under:
Water
Life
>
Nature
Freshwater
Ecosystems
Stresses
Pressures
Conservation,
Management,
Awareness
Nature Communications,
Journal Year:
2022,
Volume and Issue:
13(1)
Published: Nov. 24, 2022
Non-perennial
rivers
and
streams
-
those
that
periodically
cease
flowing
are
critical
components
of
aquatic
systems
comprise
over
half
global
river
stream
systems.
We
argue
for
coordinated,
collaborative,
standardized,
open
efforts
to
understand
their
unique
biogeochemical
behaviour,
which
is
becoming
ever
more
pressing
due
pronounced
shifts
between
wet
dry
as
the
climate
changes.
Rivers
increasingly
drying
with
change
impacts
may
be
important.
In
this
comment
authors
discuss
challenges
biogeochemistry
non-perennial
streams,
what
can
done
tackle
them.
Scientific Reports,
Journal Year:
2025,
Volume and Issue:
15(1)
Published: Feb. 5, 2025
Dissolved
organic
matter
(DOM)
is
vital
to
ecosystem
functions,
influencing
nutrient
cycles
and
water
quality.
Understanding
the
processes
driving
DOM
chemistry
variation
remains
a
challenge.
By
examining
these
through
community
ecology
perspective,
we
aim
understand
balance
between
stochastic
forces
(e.g.,
random
mixing
of
DOM)
deterministic
systematic
loss
certain
types
molecules)
shaping
chemistry.
Previous
research
on
influences
over
applied
null
models
aquatic
environments
subsurface
pore
water.
Our
study
extends
this
variably
inundated
riverbed
sediments,
which
are
widespread
globally.
We
studied
38
river
reaches
across
biomes,
finding
that
within
most
sites
was
governed
by
were
highly
localized
led
spatial
divergence
in
each
reach.
The
degree
determinism
varied
substantially
hypothesized
related
differences
sediment
moisture.
findings
partially
supported
this,
showing
upper
limit
decreased
with
increasing
integrated
our
results
previous
studies
develop
post-hoc
conceptual
model
proposing
assemblages
become
more
along
continuum
from
saturated
spaces
drier
sediments
or
soils.
This
aligns
work
linking
Damköhler
number
hydrologic
connectivity,
suggesting
generalizable
patterns
can
be
further
revealed
quantifying
stochastic-deterministic
space,
time,
scales.