JAWRA Journal of the American Water Resources Association,
Journal Year:
2018,
Volume and Issue:
54(2), P. 298 - 322
Published: March 1, 2018
Interest
in
connectivity
has
increased
the
aquatic
sciences,
partly
because
of
its
relevance
to
Clean
Water
Act.
This
paper
two
objectives:
(1)
provide
a
framework
understand
hydrological,
chemical,
and
biological
connectivity,
focusing
on
how
headwater
streams
wetlands
connect
contribute
rivers;
(2)
review
methods
quantify
hydrological
chemical
connectivity.
Streams
affect
river
structure
function
by
altering
material
fluxes
river;
this
depends
factors:
functions
within
that
fluxes;
(or
isolation)
from
rivers
allows
prevents)
transport
between
systems.
Connectivity
can
be
described
terms
frequency,
magnitude,
duration,
timing,
rate
change.
It
results
physical
characteristics
system,
e.g.,
climate,
soils,
geology,
topography,
spatial
distribution
components.
Biological
is
also
affected
traits
behavior
biota.
altered
human
impacts,
often
complex
ways.
Because
variability
these
factors,
not
constant
but
varies
over
time
space.
quantified
with
field-based
methods,
modeling,
remote
sensing.
Further
studies
using
are
needed
classify
ecosystems
impacts
Journal of the North American Benthological Society,
Journal Year:
2010,
Volume and Issue:
29(1), P. 26 - 40
Published: March 1, 2010
Over
the
last
25
y,
stream
ecosystem
theory
has
expanded
to
include
explicitly
vertical
dimension
of
surface–groundwater
linkages
via
hyporheic
zone
and
below
alluvial
floodplains.
Hydrological
exchange
between
mediates
transport
products
from
biogeochemical
activities
within
sediments.
Hot-spots
primary
productivity
in
surface
often
result
upwelling
nutrient-rich
water.
Conversely,
downwelling
water
supplies
organic
matter
dissolved
O2
invertebrates
microbes,
enhancing
productivity.
Many
papers
seminal
conceptual
empirical
advances
research
have
been
published
J-NABS,
reflecting
benthologists'
awareness
relevance
processes
biota
zone.
However,
major
gaps
remain.
One
is
need
for
further
data
test
predictions
several
current
frameworks
that
hypothesize
conditions
under
which
might
be
expected
contribute
most
metabolism,
especially
large
rivers
with
shallow
aquifers.
A
second
how
apply
findings
about
functional
significance
river
restoration
conservation.
restore
or
protect
habitats
probably
benefit
fauna
as
well,
but
this
prediction
should
tested.
Last,
sediments
occur
across
multiple
hierarchical
spatial
scales,
we
are
yet
understand
fully
these
interactions
extrapolate
successfully
scales.
J-NABS
continue
play
a
significant
role
publishing
on
extend
scope
applications
floodplain
management
restoration.
Journal of Environmental Quality,
Journal Year:
2009,
Volume and Issue:
38(5), P. 1942 - 1955
Published: Aug. 25, 2009
Ground
water
and
surface
interactions
are
of
fundamental
importance
for
the
biogeochemical
processes
governing
phosphorus
(P)
dynamics
in
riparian
buffers.
The
four
most
important
conceptual
hydrological
pathways
P
losses
from
retention
buffers
reviewed
this
paper:
(i)
diffuse
flow
path
with
ground
through
aquifer,
(ii)
overland
across
buffer
coming
adjacent
agricultural
fields,
(iii)
irrigation
tile
drainage
fields
where
disconnected
drains
irrigate
buffer,
(iv)
inundation
(floodplain)
river
during
short
or
longer
periods.
We
have
examined
how
different
paths
influence
mechanisms
theoretically
empirical
evidence.
determine
water-borne
compounds
meet
interact
iron
aluminum
oxides
other
minerals
geochemical
cycling
complex
dynamic
environment
that
constitutes
a
buffer.
main
physical
process
buffer-sedimentation-is
active
along
several
may
account
rates
up
to
128
kg
ha(-1)
yr(-1),
while
plant
uptake
temporarily
immobilize
15
yr(-1).
Retention
dissolved
is
not
as
pronounced
particulate
often
below
0.5
Several
studies
show
significant
release
(i.e.,
8
yr(-1)).
Nature Communications,
Journal Year:
2016,
Volume and Issue:
7(1)
Published: April 7, 2016
Environmental
transitions
often
result
in
resource
mixtures
that
overcome
limitations
to
microbial
metabolism,
resulting
biogeochemical
hotspots
and
moments.
Riverine
systems,
where
groundwater
mixes
with
surface
water
(the
hyporheic
zone),
are
spatially
complex
temporally
dynamic,
making
development
of
predictive
models
challenging.
Spatial
temporal
variations
zone
communities
a
key,
but
understudied,
component
riverine
function.
Here,
investigate
the
coupling
among
groundwater–surface
mixing,
biogeochemistry,
we
apply
ecological
theory,
aqueous
DNA
sequencing
ultra-high-resolution
organic
carbon
profiling
field
samples
collected
across
times
locations
representing
broad
range
mixing
conditions.
Our
results
indicate
stimulates
heterotrophic
respiration,
alters
composition,
causes
processes
shift
from
stochastic
deterministic
is
associated
elevated
abundances
taxa
may
degrade
suite
compounds.
Groundwater-surface
zones
link
critical
ecosystem
domains,
attendant
microbe-biogeochemistry-hydrology
interactions
poorly
known.
authors
show
groundwater-surface
shifts
ecology
deterministic.
Freshwater Biology,
Journal Year:
2010,
Volume and Issue:
55(11), P. 2215 - 2237
Published: June 9, 2010
Summary
1.
In
this
review,
we
first
summarize
how
hydrologic
connectivity
has
been
studied
for
riverine
fish
capable
of
moving
long
distances,
and
then
identify
research
opportunities
that
have
clear
conservation
significance.
Migratory
species,
such
as
anadromous
salmonids,
are
good
model
organisms
understanding
ecological
in
rivers
because
the
spatial
scale
over
which
movements
occur
among
freshwater
habitats
is
large
enough
to
be
easily
observed
with
available
techniques;
they
often
economically
or
culturally
valuable
can
fragmented
by
human
activities;
integrate
landscape
conditions
from
multiple
surrounding
catchment(s)
in‐river
conditions.
Studies
focussed
on
three
themes:
(i)
relatively
stable
connections
(connections
controlled
processes
act
broad
spatio‐temporal
scales
>1000
km
2
>100
years);
(ii)
dynamic
acting
fine
moderate
∼1–1000
<1–100
(iii)
anthropogenic
influences
connectivity,
including
actions
disrupt
enhance
natural
experienced
fish.
2.
We
outline
eight
challenges
role
ecology,
organized
under
foci:
addressing
constraints
river
structure;
embracing
temporal
complexity
connectivity;
managing
fishes.
Challenges
include
structure
stream
networks,
force
direction
flow,
scale‐dependence
shifting
boundaries,
behaviour
life
histories
quantifying
influence
aligning
management
goals.
As
discuss
each
challenge,
relevant
approaches
literature
provide
additional
suggestions
improving
3.
Specifically,
suggest
rapid
advances
possible
following
arenas:
incorporating
network
discharge
into
analyses;
increasing
explicit
consideration
scope
parsing
degrees
defining
acceptable
alterations.
Multiscale
analyses
most
likely
dominant
patterns
disconnections,
appropriate
at
focus
activities.
Canadian Journal of Fisheries and Aquatic Sciences,
Journal Year:
2015,
Volume and Issue:
72(8), P. 1272 - 1285
Published: April 16, 2015
A
better
understanding
is
needed
of
how
hydrological
and
biogeochemical
processes
control
dissolved
organic
carbon
(DOC)
concentrations
matter
(DOM)
composition
from
headwaters
downstream
to
large
rivers.
We
examined
a
DOM
dataset
the
National
Water
Information
System
US
Geological
Survey,
which
represents
approximately
100
000
measurements
DOC
concentration
at
many
sites
along
rivers
across
United
States.
Application
quantile
regression
revealed
tendency
towards
spatial
temporal
homogenization
shift
dominance
aromatic
in
more
aliphatic
downstream.
The
concentration–discharge
(C-Q)
relationships
each
site
slope
zero.
propose
that
despite
complexities
river
networks
have
driven
revisions
River
Continuum
Concept,
show
chemostasis
(C-Q
zero)
because
hydrologic
drivers
connect
terrestrial
sources
streams
instream
near-stream
result
preferential
losses
gains
DOM.
Frontiers in Marine Science,
Journal Year:
2017,
Volume and Issue:
4
Published: Jan. 31, 2017
The
purpose
of
this
review
is
to
highlight
progress
in
unraveling
carbon
cycling
dynamics
across
the
continuum
landscapes,
inland
waters,
coastal
oceans,
and
atmosphere.
Earth
systems
are
intimately
interconnected,
yet
most
biogeochemical
studies
focus
on
specific
components
isolation.
movement
water
drives
cycle,
and,
as
such,
waters
provide
a
critical
intersection
between
terrestrial
marine
biospheres.
Inland,
estuarine,
well
studied
regions
near
centers
human
population
Northern
hemisphere.
However,
many
world's
large
river
their
receiving
remain
poorly
characterized,
particularly
tropics,
which
contribute
disproportionately
fraction
transformation
organic
matter
dioxide,
Arctic,
where
positive
feedback
mechanisms
likely
amplify
global
climate
change.
There
gaps
current
coverage
environmental
observations
along
aquatic
continuum.
For
example,
tidally-influenced
reaches
major
rivers
near-shore
around
plumes
often
left
out
budgets
due
combination
methodological
constraints
poor
data
coverage.
We
suggest
that
closing
these
could
potentially
alter
estimates
CO2
outgassing
from
surface
atmosphere
by
several-fold.
Finally,
order
identify
constrain/embrace
uncertainties
budget
estimations
it
important
we
further
adopt
statistical
modeling
approaches
have
become
well-established
fields
oceanography
paleoclimatology,
for
example.
Water Resources Management,
Journal Year:
2015,
Volume and Issue:
30(1), P. 1 - 32
Published: Nov. 4, 2015
Scientists
and
practitioners
agree
that
integrated
water
resource
management
is
necessary,
with
an
increasing
need
for
research
at
the
regional
scale
(103
to
105
km2).
At
this
interactions
between
environmental
human
systems
are
fully
developed
global
change
linked
local
actions.
The
groundwater-surface
interaction
(GW-SW)
of
particular
interest.
Herein
we
review
scientific
journal
literature
examine
GW-SW
scale.
We
briefly
all
existing
on
GW-SW,
then
summarise
its
characteristics
different
scales
identify
specific
challenges
explore
whether
should
be
treated
differently
scales.
Regional
rarely
examined
in
experimental
field
studies,
which
almost
exclusively
cover
small
areas.
However,
often
integral
large
coupled
models.
Thus,
collate
information
about
models
their
applications.
Fully
coupled,
physics-based
have
great
potential
meet
technical
challenges.
limited
data
availability
hampers
application
complex
loosely
schemes
more
widely
applied.
Many
modelling
concepts
been
published,
but
none
applied
a
wide
range
settings.
it
impossible
compare
performance
approaches.
Comparative
analyses
context
geographic
conditions
needed.
Unfortunately,
peer-reviewed
no
longer
provides
representative
picture
subject
as
becoming
"too
big
published"
or
too
pragmatic.