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Stream
Bank Erosion
Sometimes
controlling erosion seems like a never-ending battle. Precious soil seems to
slip away at an alarming rate, and along with it go property values. While some
stream bank erosion is due to natural stream flow, people’s actions speed up the
problem when they convert land from wooded land to pastures or even worse
commercial areas with lots of impervious surface, without preventing erosion
down stream. A large increase in impervious surfaces (paved roads, rooftops,
drive ways, parking lots, etc.) added with new development has increased
runoff — rain water or storm water that is not absorbed into the soil. The
increase in runoff translates to higher stream flows (deeper and faster moving
waters) and flash flooding that scours or washes away the stream banks. In
effect, stream banks are becoming unstable and eroding as streams become wider
or deeper to accommodate the increased flows.
Major
causes
Stream
banks are always in a state of fluctuation due to the natural process of
erosion, which means that soil is washed loose, transported and deposited in a
new location. However, some of our actions or a change in conditions can
increase the rate of and severity of erosion including:
· Vegetation
removal. The deep rooting
systems of native shrubs and trees help to hold the soil in place. Removing
this woody vegetation leaves the banks unprotected and more susceptible to
currents, damage from runoff, and wave action. Replacing woody vegetation with
lawns also accelerates bank erosion because the roots of common turf grasses are
too shallow to prevent bank erosion.
· Increased
stream flows. Stream bank erosion
results from the inability of soils and plants to handle increased water flow,
which is often related to development as vegetation is removed and replaced with
impervious surfaces.
· Wave
action from wind. Constant waves and
swells created by winds can loosen soil particles on shorelines and cause
erosion, especially along points and other areas exposed to wind.
· Overland
runoff. If unmanaged,
overland runoff may form deep gullies, depositing sediment in a nearby stream or
reservoir.
Effects
of erosion
Eroded
soil, sand, or gravel that is carried by water is called sediment, and the
process by which it accumulates in streams and reservoirs is called
sedimentation. In nature, there is a low level of erosion that is a normal part
of geological processes, but our actions can increase levels of sediment
entering streams which have negative impacts on water quality and stream
health.
Sediment
is transported downstream by streams and rivers. Some sediment eventually
reaches a reservoir where it settles and accumulates. Sediment is also deposited
directly into reservoirs by runoff and stream bank erosion. Sedimentation is the
largest source of nonpoint source pollution and a serious threat to water
quality because it can:
· Fill spaces between
rocks and gravel, suffocating aquatic organisms
· Destroy the habitat
of aquatic insects and other wildlife in the aquatic food chain
· Release nutrients
and toxic chemicals, which lower water quality, promote algal growth, and harm
aquatic wildlife
· Decrease the clarity
of water and limit the growth of beneficial aquatic plants
· Increase the cost of
municipal and industrial water treatment
· Reduce the
desirability of water for swimming and other types of recreation
· Fill natural stream
channels and cause an increase in bank erosion.
Erosion
control
The best
approach to controlling stream bank erosion depends on the severity and cause of
the problem. In some cases, woody vegetation and a good riparian or vegetative
buffer may be all that’s needed. In other cases, a combination of bioengineering
treatments and native vegetation or hard-armoring with rock riprap may be
necessary. Contact the City’s Stormwater Program Manager to find out more
information or take a look at the
Manual
for Erosion & Sediment Control in Georgia.
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