FLOOD
CONTROL
A. INTRODUCTION
In the U.S.,
floods
rank second only to earthquakes in
terms of the damages caused by
geologic processes.
This reflects two facts: (1)
floods are
widespread, and
(2) many people live within
floodplains. Consequently,
considerable time and money have been
invested in
efforts to control floods.
B. BACKGROUND
1. RUNOFF
Surface runoff occurs when rainfall intensity exceeds
the
rate at which water can soak into the ground. As
runoff
from a
drainage basin reaches a
stream, it will
cause a
rise in stream flow (or
discharge).
2. FLOODS
Floods occur when streams overflow their banks and
spill out onto their adjacent
floodplains.
This process
allows
streams to deposit some of their sediment load,
which
can create
natural levees.
Any
given stream discharge has a long-term, average
recurrence
interval. Natural streams in humid regions
overflow
their banks once every 2 to 3 years; and larger
floods occur less frequently. Because floods are truly
random, it is impossible to predict when they will occur.
C. RAINFALL AND RUNOFF
a. "Flashy" (Efficient) Drainage Basins
b. Inefficient Drainage Basins
2. INFLUENCE OF GEOLOGY
b. Topography
c. Permeability
3. INFLUENCE OF HUMANS
Urbanization and development lead to the removal of
forests
and wetlands, which serve to naturally retard
the
runoff of surface water. In contrast, the
pavement
and
storm sewers that accompany
urbanization
inhibit
infiltration
and send runoff to the nearest stream more
quickly
(thus decreasing
lag
time and
increasing peak
flows). Infiltration
basins are intended to counteract
these
effects of urbanization.
D. LIVING IN FLOODPLAINS
In "a perfect" world, people would live outside of
the
100-Year
Floodplain, which would reduce the risk of
flooding in any given year to 1 percent or less.
However, because many communities have grown up
within
100-year
floodplains, the approach has been to
build engineering structures that protect people living
in these communities.
2. FLOODPLAIN MANAGEMENT
Attempts
to control rivers through engineering are not
without their consequences, as rivers tend to adjust to
engineering structures in order to maintain a "graded"
condition.
a.
Levees,
Floodwalls (picture)
The situation in New Orleans: rebuilding plan
The
Lower Mississippi River
is an example of a river
where all of these approaches have been used.