Turbulent flow characteristics over gravel bed channel with submerged vegetation patches
Physics of Fluids,
Год журнала:
2025,
Номер
37(3)
Опубликована: Март 1, 2025
This
experimental
research
investigates
the
turbulent
flow
dynamics
in
a
narrow
open
channel
with
submerged
finite
uniform
patches
of
flexible
and
rigid
vegetation
placed
along
sides
at
equal
intervals.
A
Sontek
FlowTracker
2.0
Acoustic
Doppler
Velocimeter
was
used
to
collect
instantaneous
velocity
data
evaluate
essential
attributes,
including
profiles,
Reynolds
shear
stress,
higher-order
moments,
bursting
events.
The
findings
indicate
that
maximum
intensity
turbulence
occurs
inflection
point
immediately
above
plant's
canopy.
Vegetation
greatly
affects
structure,
reducing
zone
increasing
Compared
upstream
non-vegetation
zone,
depth-averaged
increased
by
24%
canopy,
diminished
19%
below
12%
downstream
non-vegetated
vegetation.
For
patches,
23%
25%
5%
as
compared
zone.
Quadrant
analysis
revealed
occurrence
sweeps
ejections
more
nearer
vegetated
bed.
Furthermore,
arrangement
placement
were
pivotal
diminishing
affecting
momentum
transfers
between
zones.
These
significantly
modifies
patterns,
dispersing
loads.
enhances
comprehension
flow-vegetation
natural
channels,
impacting
riverbank
stability
ecological
habitat
management.
Язык: Английский
Hydrodynamics and bed morphology in a double-layered partially vegetated mobile bed channel
Physics of Fluids,
Год журнала:
2025,
Номер
37(3)
Опубликована: Март 1, 2025
This
study
investigates
the
hydrodynamics
and
sediment
transport
in
a
double-layered
partially
vegetated
mobile
bed
channel,
focusing
on
impact
of
submerged
vegetation
with
submergence
ratio
61.53%
30.77%
flow
dynamics
morphology.
Experiments
were
conducted
straight,
tilting
rectangular
flume
staggered
double
layered
covering
half
channel
width.
The
three
dimensional
time-averaged
velocity
components,
turbulent
intensities,
secondary
current,
kinetic
energy,
Reynolds
shear
stress
are
measured
analyzed
using
contour
plots
along
outcomes
reveal
that
induces
significant
momentum
exchange
between
non-vegetated
sections.
In
section,
dampens
streamwise
intensity
near
bed,
promoting
deposition
enhancing
stability.
Momentum
transfer
at
interface
strengthens
shear,
increasing
turbulence
leading
to
greater
erosion.
Negative
streamwise-vertical
indicates
helical
flow,
while
transverse-vertical
peaks
bed.
Flow
diversion
intensifies
erosion
high-energy
vegetation-induced
drag
decelerates
causing
transition
deeper
section.
Double-layered
rivers
or
canals
is
more
effective
stabilizing
materials.
These
findings
provide
critical
insight
for
river
restoration
management,
emphasizing
necessity
integrated
management
strategies
balance
across
heterogeneous
environments.
Язык: Английский