Water Resources Research,
Journal Year:
2022,
Volume and Issue:
58(12)
Published: Dec. 1, 2022
Abstract
Future
increases
in
the
frequency
of
tidal
flooding
due
to
sea
level
rise
(SLR)
are
likely
affect
pore
water
salinities
coastal
aquifers.
In
this
study,
we
investigate
impact
increased
on
salinity
and
flow
dynamics
aquifers
using
numerical
variable‐density
variably‐saturated
groundwater
salt
transport
models.
Short
(sub‐daily)
long
(decadal)
period
tides
combined
with
SLR
projections
drive
continuous
80‐year
models
transport.
Results
show
that
encroaching
intertidal
zones
lead
both
periodic
long‐term
vertical
salinization
upper
aquifer.
Salinization
aquifer
forces
lower
interface
seaward,
even
under
SLR.
System
controlled
by
interplay
between
forcing
associated
perigean
spring
18.6‐year
lunar
nodal
cycle.
Periodic
substantially
enhances
saltwater‐freshwater
mixing,
resulting
a
6‐
10‐fold
expansion
mixing
area
across
scenarios.
The
onset
coincides
extreme
high
levels
from
cycling
constituent
amplitudes.
findings
first
demonstrate
effects
gradual
short
distributions,
reveal
competing
influences
saltwater
intrusion.
results
have
important
implications
for
ocean
chemical
fluxes
resources
as
intensifies
worldwide.
Water
resources
are
of
enormous
societal
and
ecological
importance.
In
coastal
areas,
they
under
ever
greater
pressure
due
to
population
growth,
more
affluent
lifestyles,
food
production
the
growing
tourism
industry.
Changes
landscape,
through
urbanisation
land
reclamation,
by
natural
processes
such
as
climate
change
sea
level
rise,
modify
interaction
between
seawater
groundwater
put
water
at
risk.
This
comprehensive
volume
covers
both
theory
practice
hydrogeology.
It
discusses
hydrochemistry;
submarine
discharge;
management;
palaeo-hydrology;
reclamation;
rise;
mathematical
models
variable-density
flow.
With
its
up-to-date
coverage
numerous
case
studies
that
illustrate
practical
implications,
it
is
perfect
for
students,
practitioners,
managers
researchers
who
wish
develop
an
in-depth
understanding
topics
relevant
sustainably
managing
resources.
Water Resources Research,
Journal Year:
2024,
Volume and Issue:
60(4)
Published: April 1, 2024
Abstract
Coastal
aquifers
are
commonly
layered,
and
thus,
a
clear
understanding
of
groundwater
flow
salt
transport
in
layered
coastal
is
important
for
managing
fresh
groundwater.
However,
the
influence
leakage
between
adjacent
on
processes
remains
largely
unknown
where
tides
considered.
This
study
used
laboratory
experiments
numerical
simulation
to
examine
within
tidal
aquifer‐aquitard
system
(i.e.,
an
unconfined
aquifer
underlain
by
semi‐confined
aquifer,
with
intervening
thin
aquitard).
The
laboratory‐scale
observations
current
first
offshore
aquifer.
results
close
agreement,
revealing
that
upward
from
into
saltwater
wedge
overlying
caused
buoyant
instabilities
form.
development
freshwater
fingers
created
complex
saltwater‐freshwater
mixing,
leading
mixed
influx‐efflux
patterns
across
sloping
aquifer‐ocean
interface.
Compared
non‐tidal
conditions,
forces
reduced
net
increased
horizontal
toward
sea,
which
turn
extent
higher
rates
both
saline
submarine
discharge
(SGD),
tides,
led
lower
ages
These
findings
have
implications
unveiling
characteristics
seawater
intrusion,
SGD
geochemical
hotspots
aquifers.
Hydrology and earth system sciences,
Journal Year:
2025,
Volume and Issue:
29(5), P. 1469 - 1482
Published: March 18, 2025
Abstract.
In
high-energy
beach
aquifers
fresh
groundwater
mixes
with
recirculating
saltwater
and
biogeochemical
reactions
modify
the
composition
of
discharging
to
sea.
Changing
morphology,
hydrodynamic
forces,
hydrogeological
properties
control
density-driven
flow
transport
processes
that
affect
distribution
chemical
reactants.
present
study,
modelling
a
generic
2-D
cross-shore
transect
was
conducted.
Boundary
conditions
aquifer
parameters
were
varied
in
systematic
manner
suite
24
cases.
The
objective
investigate
individual
effects
boundary
on
regime,
salt
distribution,
potential
for
mixing-controlled
system
temporally
variable
morphology.
Our
results
show
changing
morphology
causes
migration
infiltration
exfiltration
locations
along
transect,
leading
transient
patterns
subsurface,
thereby
enhancing
reactions.
shape
extent
zone
where
potentially
take
place,
as
well
spatiotemporal
variability
freshwater–saltwater
interfaces,
are
most
sensitive
storm
floods,
hydraulic
conductivity,
dispersivity.
study
advances
understanding
subsurface
flow,
transport,
mixing
dynamic
beneath
beaches.
These
regulate
nutrient
fluxes
coastal
ecosystems.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(4)
Published: April 1, 2021
Abstract
Recent
studies
have
confirmed
the
instability
of
tide‐induced
upper
saline
plume
(USP)
in
tidal
beach
aquifers.
A
systematic
understanding
how
unstable
USP
contributes
to
groundwater
flow
and
salinity
distribution
is
still
lacking.
Here
we
used
laboratory
experiments
numerical
simulations
examine
responses
submarine
discharge
(SGD)
flow.
The
results
revealed
that
changes
physical
forcing
conditions
(tides
inland
freshwater
input)
drove
transition
from
stable
states.
Meanwhile,
phase‐averaged
SGD
its
components
fluctuated
over
time,
their
oscillation
amplitudes
depended
on
conditions.
There
was
a
correlation
between
fluctuation
water
exchange
across
aquifer‐sea
interface.
fluxes
interface
under
usually
varied
considerably
time
with
lower
frequency
comparison
extent
seawater
intrusion
(SWI)
measured
by
total
salt
mass
stored
aquifer
also
especially
vibration
tendency
opposite
sum
circulation
efflux.
For
coastal
aquifers
affected
tides,
SWI
dominated
efflux,
followed
input
influx.
These
findings
lay
foundation
for
gaining
better
potential
implications.
Geophysical Research Letters,
Journal Year:
2020,
Volume and Issue:
47(17)
Published: Aug. 26, 2020
Abstract
Intertidal
aquifers
are
hotspots
of
biogeochemical
cycling
where
nutrients
and
contaminants
processed
prior
to
discharge
the
ocean.
The
nature
dynamic
subsurface
mixing
zone
is
a
critical
control
on
mitigating
reactions.
Simulation
density‐dependent,
variably
saturated
flow
salt
transport
incorporating
realistic
representations
aquifer
heterogeneity
was
conducted
within
Monte
Carlo
framework
investigate
influence
nonuniform
permeability
intertidal
groundwater
dynamics.
Results
show
that
coupled
with
tides
creates
transient
preferential
paths
zone,
evolving
multiple
circulation
cells
fingering‐type
salinity
distributions.
Due
heterogeneity,
strain‐dominated
(intense
mixing)
vorticity‐dominated
(low
regions
coexist
at
small
spatial
scales,
their
extent
reaches
peaks
high
tide
low
tide.
Such
topological
characteristics
reveal
complex
tempo‐spatial
patterns
for
localized
areas
intensities,
which
have
implications
processing.
Estuarine Coastal and Shelf Science,
Journal Year:
2023,
Volume and Issue:
290, P. 108418 - 108418
Published: June 24, 2023
Redox
conditions
are
a
major
control
for
the
concentrations
and
mass
fluxes
of
water
constituents,
e.g.,
nutrients,
metals
organic
molecules
within
subterranean
estuaries
(STE).
Due
to
transient
flow
transport
processes
in
STEs
as
well
variable
temperatures
input
redox
reactants,
zoning
STE
is
believed
be
highly
dynamic.
In
present
study
we
analyzed
individual
combined
effects
storm
floods,
seasonal
changes
groundwater
recharge
rates,
beach
morphodynamics
on
STE.
For
this
purpose,
2D
cross-shore
density-dependent
reactive
model
was
set
up
representing
aquifer
exposed
high-mesotidal
medium-to
high-energy
wave
conditions,
floods.
The
simulation
results
show
that
under
given
dynamics
may
occur
down
depth
20
m.
Morphodynamics
appear
most
important
factor
transience
zones
compared
other
factors.
Seasonal
meteoric
rates
least
relevant
STEs.