Environmental
Consequences of the Bonnet Carre Spillway
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- Vegetation and Land
Use
- Wildlife
- Fish and Aquatic
resources
Vegetation
- 450 acres will be cleared
for off-road vehicle use
- sand hauling, vehicle
use, boat use, and visitors will lead to soil erosion and
subsidence and a change in vegetation
- the clearing of land will
contribute to soil loss
- plant distribution and
diversity will change
- Forested tracts will
become bottom land hardwoods and swamps will decrease
Wildlife
- removal of fallen trees
and debris from the lower borrow canal's bottom would affect 99.5
acres of aquatic habitat and lessen habitat for mink, raccoon, and
several other species of reptiles and amphibians
- an increase in crawfish
and finfish will provide more food for wading birds, such as the
great blue heron, green heron, great egret, snowy egret,
tricolored heron, yellow-crowned night heron and the white ibis.
Mink, raccoon, and river otter also benefit
- reptiles use the area for
spawning, nursery, and feeding
- the alligator and the
bullfrog are predators of crawfish nd their numbers should
increase with the number of crawfish
Fish and Aquatic
resources
- Habitat quality is lost
by the removal of 99.5 acres of aquatic habitat
- crawfish production will
increase by emphasis on fisheries enhancement, however low oxygen
zones in the swamps negatively affect crawfish
- A combination of better
water quality and an increase in crawfish production will increase
fisheries production since crawfish is the primary food for blue
catfish, yellow bull head, warm mouth, and largemouth bass during
high water and bowfish and garfish during low water. Flathead
catfish, blue gill and black crappie also feed on
crawfish
- The introduction of
oxygen rich waters will enhance habitat as a spawning and nursery
area for largemouth bass, gizzard shad and species of buffalo,
carp, catfish, gar, and sunfish
- the Mississippi will be
the main source of high oxygen level water
- The secondary source is
primary production from aquatic life. This results in the
stratification of levels of oxygen