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Salt River Channelization |
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Channelization of the Salt River was
completed in 1996 and recovered 843 acres of developable land from the
floodplain. The channelization, which was funded by the
Arizona
Department of Transportation (ADOT) and
Flood
Control District of Maricopa County (FCDMC) features eight-foot thick soil
cement on a lower 10-year flood levee (extending to the bottom of the channel)
and wire mesh-encased rock gabions on a 200-year flood levee.
These terraces comprise the north and south bank
linear parks. The lower terrace features a decomposed granite walking trail
around the lake and beyond its edges along the channel. The upper terrace is
landscaped to cover the gabions, provide shade for the lower path and enhance
the concrete bicycle path on top of the levee.
Channelization was designed to contain a 250,000
cubic feet per second (cfs), 220-year event flow from dam releases and floods
and still have four feet of freeboard (room within the channel before
overflowing the edges).
Recorded floods in the metropolitan
Phoenix area date back to 1891 with the largest recorded at 300,000 cfs (this
figure may vary due to technological limitations prior to the 1900's and
possible errors in recording). The channel varies in width from 800-to-1,200
feet wide. Grade-control structures were built in every mile to control scouring
caused by water flows. A 12-foot deep concrete structure is being used as part
of the foundation of the inflatable
dam at the west end of the lake. This particular grade-control structure can
be seen in the river channel.
Rock gabions consist of wire mesh (like chain link fence) pillows filled with
river rock and tied together along the slope of the levee.
Soil cement is a mixture of mostly sandy soil and a little cement. It is
combined as a stabilizer along the levee and tests at about 900 psi (pounds per
square inch) of force. It is not as strong as concrete, so some erosion can be
seen, but it is a much more natural looking material.
After starting construction of the Town Lake,
contractors were required to remove the outer layer of this soil cement.
However, the equipment being used had difficulty breaking through the material.
Material testing proved that the material had the strength of structural
concrete (2,500 psi) - much harder than what was called for during the
channelization project. A change in equipment and method finally allowed the
lake edge contractor to break through the surface and chisel it to the required
slope for pouring a hard edge lake treatment that now makes up the edge of Tempe
Town Lake.
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