I.Do
nothing, no protection, leading to eventual abandonment:
This
option is very
environmental
friendly and
the only pollution produced is from the resettlement process. However
it does
mean losing a lot of land to the sea and people will lose their houses
and
their homes.
II.Managed
retreat or realignment: Managed retreat allows an area
that was not previously
exposed to flooding by the sea to become flooded. This process is
usually in
low lying estuarine or deltaic areas and almost always involves
flooding of
land that has at some point in the past been reclaimed from the sea.
The
technique is used when the land adjacent to the sea is low in value. A
decision
is made to allow the land to erode and flood, creating new sea,
inter-tidal and
salt-marsh habitats. This process may continue over many years and
natural
stabilization will occur.
III.Hold
the line,
shoreline protection, whereby seawalls
are constructed around the coastlines
IV.Move
seawards, by constructing new defenses seaward the
original ones
V.Limited
intervention, accommodation, by which adjustments are made
to be able to cope
with inundation, raising coastal land and buildings vertically
The
decision to choose a strategy is site-specific, depending on pattern of
relative sea-level change, geomorphologic setting, sediment
availability and
erosion, as well a series of social, economic and political factors.
Stabilization
techniques: Any
of the following three
stabilization techniques (viz. Hard
Stabilization,
Soft
Stabilization,
and relocation of
threatened structures) can be
adopted (based on the choice of strategy) for protection
against
coastline erosion and shoreline property damage: .
Hard
stabilization commonly involves the construction of
structures like seawalls,
breakwaters, revetments, and gabions. Generally these structures are
designed
to absorb some or all of the impact of waves crashing along the
shoreline. This
is done either at the edge of the actual beach or further out in the
water to
break up the incoming waves before they reach the shore. Hard
stabilization
methods have been moderately successful, but often come with a
considerable
downside including their large financial expense, adverse effects on
neighboring beaches, and degraded beach aesthetics.
Soft
stabilization techniques generally consist of depositing
sand from elsewhere to
supplement an eroding beach. This process adds to the size of the
physical
beach and provides a greater buffer for shoreline structures. Usually
the sand
is gathered from other offshore deposits or inland sand source. This
process does
halt the erosion temporarily, and improves recreation without all of
the
obtrusive environmental effects of hard stabilization. However, it has
proven
to be quite inefficient and again causes adverse effects to adjacent
beaches,
such as increased wave potency. Over 100 beaches on the United States
eastern coastline have employed this strategy, but the statistical
success in
unimpressive. On these beaches, 26% saw their imported sand disappear
after
just one year, and in only 12% of the cases did the replenished beaches
last
for more than five years. The average span of effectiveness for the
soft
stabilized, replenished beaches was only two to three years.
The
other viable option is relocation
of threatened structures. Obviously this is rarely
popular with private homeowners and businesses because of the expense.
However
this option poses minimal environmental damage and is usually a
one-time
expense if the relocation is done properly. Abandonment of threatened
coastline
structures is another option that may be cheaper for the private
landowner, but
becomes a considerable public cost.
Hard
stabilization, soft stabilization, and relocation are all methods that
are
currently being employed, but it remains unclear which of these
methods, or
which combination, is the best management practice for coastal erosion
situations. Perhaps measures to preserve the natural remedies for beach
erosion, such as the protective shoreline vegetation and coastal
forests,
should be factored more prominently into these methodologies.
These
techniques are briefly discussed below:
(a) Hard
Stabilization
Techniques: Hard
Stabilization techniques include the following:
(i)Construction
of groynes: Groynes
are wooden, concrete and/or rock barriers or walls
perpendicular to the sea.
A
view of Groynes in Sitges
(Spain)
(ii)
Construction of Seawalls:
Construction of Seawalls (usually of masonry, concrete or rock, built
at
the base of a cliff or at the back of a beach, or used to protect a
settlement
against erosion or
flooding.
Seawall is a structure
which is designed to protect a
shoreline
from flooding and erosion. Essentially, a seawall acts as a
layer between
the vulnerable coastline and the ocean. Wave action can beat at the
seawall
without eroding the coast, although the seawall itself will eventually
break
down and require repair or replacement. Seawalls also help to insulate
communities from flooding, although high waves can still breach most
seawalls.
A seawall can also provide a space for recreation, since the top of a
seawall
is often flat, allowing people to walk on it or to fish from it.
In
some cases, a seawall will be constructed on shore to break high waves
which
might otherwise damage structures and roads on the shore. In these
instances,
several lower barriers may precede the seawall, to help break up the
wave
energy before the waves hit the wall. Other sea walls are built in the
water
right next to a shoreline, as is the case on many islands. Some nations
also
build seawalls in the open water to act as flood barriers and to
dissipate
waves before they reach the shore, encouraging them to break more
gently.
Many
seawalls are curved, allowing waves to break against them while
reducing their
energy. Others are straight, and they are designed to bring waves to a
standstill. It is not uncommon to bury low mounds of rubble in front of
a
seawall to assist with the goal of reducing the power of waves as they
hit the
shore. In the case of a seawall which is meant to resist flooding, the
seawall
may be quite high so that it can cope with storm surge.
Traditional
seawalls are built from large rocks, pebbles, and other rubble; some
remains of
ancient seawalls built in this style can be seen in many communities. A
modern
seawall can be made from these materials, although it may also
integrate
concrete, metal bars, and other tools to make the seawall more sturdy.
Cheaper
seawalls may be made from wood and plastic, which provide some
protection
although they can potentially fail in heavy weather.
(iii)
Construction of
revetments: A
revetment is a type of structure that is built
along an embankment, shoreline
or steep facing slope in order to protect it against erosion generated
by wave or
current action. A revetment is like a common sea wall in that it is
designed to
maintain the location and shape of a shoreline. Instead of standing
vertically
like a sea wall, however, a revetment "coats" the shoreline with
protective material.
Starting
from the shoreline and extending on to shore, a revetment will
usually have a filter
cloth. A filter cloth allows groundwater to drain through
the
structure without
creating erosion channels that could weaken the revetment. On top of
the filter
cloth different grades of stone are layered. The base layer of stone,
called
"core stone", is smaller to allow for settling, while
the outermost
layer of stone, called "armor stone" is larger and heavier. The
filter cloth and core stone provide a stable base to build upon, and
the armor
stone protects the revetment (and thus the shoreline) from wave and ice
action.
The layers of stone extend above and below the shoreline surface, with
the top extending above the "high water level", the highest
anticipated water level based on historical data, preventing waves from
going
over the revetment. Likewise, the bottom of the revetment extends below
water
level. This "toe reinforcement" prevents waves from removing sand at
the revetment base and thus undermining the structure.
(iv) Use
of Rock Armour:
Large rocks are piled
or placed at the foot of dunes or cliffs,
which are
placed with native stones of the beach: — also known as rip
rap, rubble or shot
rock. The rock
used
will typically be a very hard igneous rock
that is
exceedingly resistant to erosion. When rock is placed on the beach it
is
arranged so that large void spaces are left. When waves hit the rock
they are
only partially reflected, and can flow round the rocks, expending their
energy
less quickly which reduces scour. Another advantage of using rock is
that if
the rocks are moved during heavy storms it is a simple procedure to
replace
them in the correct position. (Figure on the right shows piling of rock
armour,
groynes can also be seen). Rock armour is often used to
protect the base
of seawalls and prevents direct attack and damage of the wall.
Additionally the
rock provides support for the wall, improving its stability.
(v)
Use
of Gabions: Boulders and rocks are wired into
mesh cages and
usually
placed
in front of areas vulnerable to heavy to
moderate erosion.
Gabions are normally used on eroding cliff faces where their purpose is
two
fold. Firstly they provide stability to the cliff face, preventing
failure, and
secondly they permit water to drain away that might otherwise
contribute to
landsliding. Gabions are relatively cheap and easy to construct but
they are
not suitable for use in locations exposed to wave action because they
are too
flexible and are easily destroyed.
(vi)
Construction of
Offshore breakwater: Breakwaters are structures constructed
on
coasts as part of coastal defence or to protect
an
anchorage from the effects
of weather and longshore drift. Offshore breakwaters,
also called
bulkheads, reduce the intensity of wave action in inshore
waters and thereby
reduce coastal erosion. They are constructed some distance away from
the coast
or built with one end linked to the coast. The breakwaters may be small
structures, placed one to three hundred feet offshore in relatively
shallow
water, designed to protect a gently sloping beach. Breakwaters may be
either
fixed or floating: the choice depends on normal water depth and tidal
range.
(figure on the right shows 3 out of 4 breakwaters Forming Portland
Harbour, England)
When
oncoming waves hit these breakwaters, their erosive power is
concentrated on
these structures some distance away from the coast. In this way, there
is an
area of slack water behind the breakwaters. Deposition occurring in
these
waters and beaches can be built up or extended in these waters.
However, nearby
unprotected sections of the beaches do not receive fresh supplies of
eroded
sediments and may gradually shrink due to erosion.
Enormous
concrete blocks and natural boulders are sunk offshore to alter wave
direction
and to filter the energy of waves and tides. The waves break further
offshore
and therefore reduce their erosive power.
(b) Soft
Stabilization
Techniques: Soft
Stabilization techniques include the following:
(i)
Beach nourishment: A
beach is the perfect defence
against wave action and,
if a beach is poor, one
option may be to undertake beach nourishment. This basically involves
adding
large quantities of material to a beach in order to build it up. The
material added will need to be very similar to the material
naturally found on the beach
and will probably come from remote
sources. Offshore dredging can
provide a
good source of suitable material for beach nourishment schemes or
alternatively
the sediment can be obtained from land based quarries. Beach management
structures may also be necessary to ensure the extra material remains
on the
beach, and even so some will probably be lost through the natural
movement of
coastal sediments. This may mean further nourishment is required in the
future
to keep the beaches at the desired level. This involves importing alien
sand
off the beach and piling it on top of the existing sand. The imported
sand must
be of a similar quality to the existing beach material so it can
integrate with
the natural processes occurring there, without causing any adverse
effects.
Beach nourishment can be used alongside the groyne schemes. The scheme
requires
constant maintenance: 1 to 10 year life before first major recharge. It
is a
better way of managing the coast rather than using the Hard
Construction
Techniques. However, the procedure is costly and only temporary.
(ii)
Sand dune stabilization:
Sand dune stabilization is a coastal management
technique for preventing
erosion. Sand dunes trap sand
and beach material
washed and blown up, the rate
of erosion is slowed and an effective flood barrier is created.
Footpaths will
also have to be introduced to stop trampling. Sand dunes stabilisation
is economical, environmentally friendly, does not disrupt the coastline
further
on, creates natural habitats for animals and plants and is not regarded
as
unattractive. However, for successful dunes to be placed it must be
thoroughly
researched beforehand and will take a long time to establish. Sand
dunes may be
stabilized through the planting of vegetation. Vegetation encourages
dune
growth by trapping and stabilising blown sand.
(iii)
Beach face dewatering:
Beach drainage or
beach face dewatering lowers the water table locally beneath the beach
face.
This causes accretion of sand above the drainage system.
Basically
consists of
continuously pumping water away
from the beach face.
The system is based on the idea that, when the water table under
the beach is lower than under the ocean, sand accretion is enhanced. As
each
wave rushes up the beach, water from the wave easily drains through the
dry
beach, leaving part of its suspended sand load on the beach. Less water
drains
back into the ocean taking less sand with it.
How
beach face dewatering works: When the water table under
the beach is lowered,
water from the wave easily drains through the dry beach, leaving part
of the
suspended sand load on the beach. Thus, the beach accretes
A
specially designed drainage system is installed under the beach, with
pumps
removing groundwater from under the beach. When considering such
systems,
operation and maintenance costs must be taken into account. The pumps
should
run continuously.