Earth Surface Processes and Landforms,
Journal Year:
2022,
Volume and Issue:
48(1), P. 104 - 118
Published: Nov. 15, 2022
Abstract
Debris
flow
is
one
of
the
dominant
processes
distributing
large
wood
(LW)
within
mountainous
catchments.
However,
little
has
been
reviewed
on
wood‐laden
debris
(WLDF),
presumably
owing
to
limited
reviewable
works.
This
article,
therefore,
navigates
international
readers
through
40
years
WLDF
studies,
most
which
have
published
only
in
Japanese.
Firstly,
we
historical
development
Japanese
particularly
focusing
1980s
and
1990s.
A
series
post‐disaster
fieldworks
from
July
1982
Nagasaki
flood
1990
Kumamoto
provided
32
catchment‐scale
budgeting
data;
empirical
relationships
among
drainage
area,
tree
species,
sediment
yield,
loads
associated
with
single
disasters
were
illustrated.
Secondly,
characteristics
summarized
based
relevant
previous
studies
recruitment,
transport,
deposition
LW
during
flows.
Thirdly,
discussed
connectivity
between
those
by
relating/contrasting
their
research
approaches
spatiotemporal
scales.
In
contrast
global
trends,
almost
exclusively
regarded
as
hazardous
materials
(i.e.,
“driftwood”
or
“woody
debris”)
that
need
be
retained
upstream
inhabited
areas.
Those
practice‐oriented
concentrated
areas
10
−2
0
km
2
,
representing
1–6
orders
magnitude
smaller
spatial
scales
than
generally
covered
existing
studies.
Strongly
motivated
engineering
requirements,
“dynamic”
interactions
flows
floods
also
physically
presented,
mainly
unique
laboratory
experiments
involving
steep
flume
(>
0.05)
mobile
bed
conditions.
Finally,
some
future
works
for
briefly
stated
practical
scientific
perspectives.
By
“rediscovering”
domestically
developed
channels
since
1980s,
a
more
comprehensive
understanding
dynamics
river
system
may
achieved.
River Research and Applications,
Journal Year:
2024,
Volume and Issue:
40(6), P. 887 - 942
Published: April 4, 2024
Abstract
In
this
article,
we
track
the
evolution
of
fluvial
biogeomorphology
from
middle
20th
century
to
present.
We
consider
emergence
as
an
interdisciplinary
research
area
that
integrates
knowledge
drawn
primarily
geomorphology
and
plant
ecology,
but
with
inputs
hydrology
landscape
ecology.
start
by
assembling
evidence
for
field
a
keyword
search
Web
Science
detailed
analysis
papers
published
in
two
scientific
journals:
journal—Earth
Surface
Processes
Landforms;
multidisciplinary
river
science
journal—River
Research
Applications.
Based
on
evidence,
identify
three
distinct
time
periods
development
biogeomorphology:
‘early
years’
before
1990;
transitional
decade
1990s;
period
rapid
expansion
diversification
themes,
methods
investigation
scales
since
2000.
Because
literature
is
vast,
can
only
summarize
developments
each
these
periods,
refer
recent
in‐depth
reviews
conceptual
perspectives
relevant
topics.
Thus,
rather
than
full
deep
review,
present
annotated
bibliographic
overview
biogeomorphology,
whereby
text
describes
broad
trends
supported
tables
citations
deliver
greater
detail.
end
brief
consideration
likely
future
developments.
The Science of The Total Environment,
Journal Year:
2022,
Volume and Issue:
838, P. 156354 - 156354
Published: May 29, 2022
Macroplastic
storage
in
mountain
rivers
remains
unexplored
and
it
is
unknown
how
river
morphology
different
surface
types
of
areas
modulate
this
process.
Therefore,
we
sampled
macroplastic
debris
stored
on
the
emergent
with
vegetation
cover
wood
jams
a
channelized,
single-thread
reach
an
unmanaged,
multi-thread
Dunajec
River
Polish
Carpathians.
Total
amounts
retained
these
reaches
were
then
estimated
basis
mean
mass
deposited
unit
area
each
type
given
reach.
Exposed
sediments
covered
herbaceous
significantly
lower
(0.6
0.9
g
per
1
m2
average)
than
wooded
islands
(respectively
6
113
m2).
The
exceeded
19,
129
180
times
those
found
islands,
exposed
sediments.
Wooded
covering
16.7%
1.5%
43.8%
41.1%,
respectively,
total
amount
that
reach,
whereas
practically
absent
channelized
Consequently,
2.4
wider
neighbouring
36
greater
km
length.
Our
study
demonstrated
controlled
by
channel
management
style
resultant
morphology,
which
hydrodynamics
longitudinal
pattern
zones
transport
retention
conveyed
flow.
Earth Surface Processes and Landforms,
Journal Year:
2021,
Volume and Issue:
47(1), P. 32 - 57
Published: June 30, 2021
Abstract
In
the
last
30
years,
work
on
large
wood
(LW)
has
expanded
and
matured
considerably,
river
scientists,
managers
practitioners
now
have
a
better
appreciation
of
role
LW
in
maintaining
ecosystems,
forming
or
stabilizing
riverine
landforms,
interacting
with
morphodynamics.
We
gained
understanding
hazards
posed
by
recruitment
transport
channel
associated
infrastructure.
While
dynamics
traditionally
been
studied
natural
environment,
innovations
laboratory
techniques
enabled
important
advances
process
dynamics,
using
physical
scale
models,
new
sensors,
scanners
sophisticated
model
boundary
conditions.
Current
trends
research
focus
(1)
mobilization
logs,
(2)
trapping
deposition
sediment
presence
(3)
contribution
to
hydraulic
flow
resistance.
Ultimately,
combined
is
needed
assess
impacts
upon
infrastructure
erodible
boundaries,
such
as
bridge
piers
retention
racks.
this
review,
we
present
critical
analysis
emerging
experimental
obtained
through
modelling
studies.
put
recent
context
global
management
challenges.
particular,
set
our
environmental
engineering
issues
that
confront
catchment
resource
Switzerland
New
Zealand.
show
how
improved
models
incorporating
transport,
accumulation
scouring
processes
are
contribute
more
reliable
hazard
risk
assessment
LW‐prone
systems.
Water Resources Research,
Journal Year:
2021,
Volume and Issue:
57(9)
Published: Sept. 1, 2021
Abstract
Log
jams
alter
gradients
in
hydraulic
head,
increase
the
area
available
for
hyporheic
exchange
by
creating
backwater
areas,
and
lead
to
formation
of
multiple
channel
branches
bars
that
drive
additional
exchange.
Here,
we
numerically
simulated
stream‐groundwater
interactions
two
constructed
flume
systems—one
without
one
with
a
series
three
jams—to
quantify
effects
interacting
jam
structures
on
at
stream
flow
rates.
In
simulations
jams,
average
rates
ranged
from
2.1
×
10
−4
2.9
m/s
various
discharge
scenarios,
but
increased
range
1.3
−3
–3.5
m/s.
Largely
due
these
rates,
connectivity
or
decreased
turnover
length
water
travels
before
zone,
an
order
magnitude,
drove
long
paths
connected
threads.
Decreased
lengths
corresponded
greater
reaction
significance
per
km,
measure
potential
zone
influence
chemistry.
For
low‐flow
conditions,
log
km
five‐fold,
0.07
0.35.
Jams
larger
volumes
led
longer
residence
times
path
exhibited
scales
Additionally,
longest
connecting
occurred
reach
branches.
These
findings
suggest
large
gains
hydrologic
can
be
achieved
promoting
in‐stream
wood
accumulation
natural
both
branching
channels.