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| Number of U.S.
states that have lost 50% or more of their original wetlands:
22 |
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| Reduction in volume
of water passing through Everglades because of development:
80% |
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| Decrease in wading
birds in Everglades National Park, 1930's-1990's: 90% |
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| Miles of canals
diverting water from Florida Everglades: ~1400 |
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| Length of Kissimmee
River, southern Florida, before vs. after channelization:
103:56 miles |
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Estimated cost
of ongoing project to restore Kissimmee River to unchannelized
state:
$372 million |
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Destruction of
Wetlands
- Most U.S. wetlands are in Alaska
- Wetland area in the lower 48 states has decreased by a little
over half since the 1600's
- Recently wetlands have been lost to agricultural and residential
development
- Hydraulic engineering projects have considerably altered the
interaction between surface and subsurface water systems in southern
Florida
- Wetlands south of Lake Okeechobee have been replaced by sugar
cane fields
- Development in southern Florida has resulted in less groundwater
recharge, salt-water intrusion alongeast coast, polluted run-off
from sugarcane fields, and reduced habitats for fish, birds, and
mammals
Distribution of wetlands
etlands cover approximately
103 million acres in the lower 48 states and an additional 170 million
acres in Alaska. In the lower 48, Florida (11 million acres), Minnesota
(9 million acres), and Texas (7.6 million acres) have the greatest
areas of wetlands. Wetlands areas have declined by approximately 55%
since the 1600's in the U.S. outside of Alaska. California (91%),
Ohio (90%), and Iowa (89%) have experienced the greatest proportional
losses of wetland area.
The principal reasons for wetland losses in recent years (1985-1995)
were the agricultural draining of wetlands (79% of losses) and draining
and infilling of wetlands as a result of urbanization and development
(21% of recent losses). The rate of wetland losses has declined from
nearly 500,000acres/yr (1950's) to 117,000 acres/yr (1985-1995).
Example: Florida Everglades
The Kissimmee River, Lake Okeechobee, and the Everglades are the key
components of the largest drainage basin in southern Florida. The
Kissimmee river feeds Lake Okeechobee which supplies water that flows
south through the Everglades, one of the world's largest freshwater
wetlands. Marjory Stoneman Douglas termed the slow, unchannelled
flow of water through the sawgrass prairie of the Everglades a "river
of grass". The bulk of the input of water into the Everglades
is from precipitation (89%) with the rest due to run-off. Most of
the outflow occurs by evapotranspiration (66%).
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View of Florida peninsula from the space shuttle. Original
image courtesy of NASA's Earth
from Space program.
Water flows down a gentle slope (3-6 cm/km) from Lake
Okeechobee toward the Everglades.
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Beginning in the early 1900's, development of southern Florida resulted
in the construction of thousands of miles of canals that diverted
water away from wetland environments. Development proceeded with four
goals (the 4 D's): dike it, dam it,divert it, drain it. The result
of this hydraulic engineering was greater flood control and expanded
agriculture. Although these were beneficial for land-owners, development
often had negative consequences for the local ecosystems. The original
Everglades wetland system was largely a consequence of a combination
of hydrological conditions defined by the hydroperiod
(duration of surface water) and hydropattern (depth
of water). Water management practices associated with the expansion
of farming and urban development altered flows in the Everglades and
changed both the hydroperiod and hydropattern.
Some consequence of these changes were:
- channelization (straightening) of Kissimmee River
destroyed wetlands and fish and wildlife habitat
- loss of transitional wetland habitat that provided feeding and
nesting habitat for wading birds
- polluted run-off from agricultural operations (e.g. sugar-cane
fields)
- decreasing soil formation and exposure of peat results in fire
hazard in dry periods (Spring) or during drought conditions
- salt-water intrusion along the east coast
- less groundwater recharge and reduced flow of water to Florida
Bay along the southern coast.
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| Changes in selected land
use patterns in southern Florida from 1900 to 1973. Note the
loss of wetland vegetation (sawgrass), growth of agriculture
(sugar cane) and expansion of coastal cities. |
The creation of artificial wetlands is necessary as urban growth
has destroyed natural wetland environments and population growth has
placed greater demands on groundwater sources. Water demand in Broward
County, Florida, increased by 40 million gallons per day from 1980
to 1990, as population increased by 200,000. The South Florida Water
Management District has purchased thousands of acres of land to be
used to enhance groundwater recharge in an effort to halt the decline
of groundwater levels.
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