IInflatable Dams |
The Tempe Town Lake is contained by an inflatable dam system consisting of eight bladders,
four in a row at the east end (located between Rural and McClintock roads), and four in a
row at the west end (located between Mill Avenue and Hardy Drive). The location of the Rio
Salado dams was somewhat determined by the $40 million Flood Control District of Maricopa
County channelization project in 1989. Grade control structures were constructed at two
locations in the Tempe portion of Rio Salado: one between McClintock Drive and Rural Road,
and one between Mill Avenue and Hardy Drive. The Tempe Town Lake was designed to take
advantage of these structures.
The dams are made up of three main elements:
- a strong, flexible, rubber coated fabric tube which is fixed securely to a concrete base
slab by clamping bars and anchor bolts
- an operating system which controls inflation and deflation of the tube
- and an automatic safety device which ensures tube deflation in flood situations.
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Each section of dam, or bladder, is about 240 feet long, weighs 40 tons and is more
than one inch thick. At times, a small amount of water can be seen flowing over the top of
the west dams, creating a 19-foot waterfall. This water can be recaptured by a
recirculation system
and pumped back into the lake. The east dams are five feet high and sit on a
two-foot cement base.
The west dams are 16 feet high and sit on a three-foot base.
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Each section of rubber is imbedded with a fabric mesh and ceramic chips and is designed to
resist tearing. The rubber also contains a self-sealing material to re-close small holes.
These dams are built to resist floodwater and debris flowing at 250,000 cubic feet per
second (the highest recorded flood in Maricopa County is 200,000 cfs. in 1905. The most
recent significant water release was recorded at 129,000 cfs. in 1993).
Tempe's dams are computer controlled and maintain air pressure of six pounds per square
inch (an automobile tire holds about 35 psi). They can be controlled individually to
within a half inch and can be lowered incrementally depending on the flood conditions.
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The bladders have special ozone and ultraviolet ray protection for the southwestern
climate and have been tested extensively for durability. They have a thin fin on top,
which spreads water flow evenly over the surface of the dam. This patented design prevents
swaying of the bladder and tearing from its structure. In some locations, these dams have
been designed with airtight doors for people to enter into the bladder for dam tours. The
Tempe Town Lake does not have interior bladder access.
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The dams were shipped across the ocean from Japan, arriving on large spools, that were
transported by truck to Tempe. These spools were stored until construction of the
lake was ready for installation of the bladders. The spools were then moved by crane
into the river bottom, and unrolled into place.
Soil cement was used to stabilize the channel banks and rock gabions were installed to
create a second levee. The flood control levee was designed for a 100-year flood event, or
215,000 cubic feet per second, with an additional four feet of freeboard (levee space,
above this water flow). With improvements to Roosevelt Dam, the capacity to contain flow
within the channel is as high as 280,000 cfs. The purpose is to keep all water within the
flood channel, which is why there is no construction within the levees.
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One of the unique features of the inflatable dams is their ability to deflate
quickly and easily to prevent upstream flooding. The dams at Tempe Town Lake can be
deflated and inflated within 30 minutes, offering a high level of control and easy method
of releasing and recapturing water.
When water flows from upstream dams, such as the Roosevelt dam, notification is made to
clear downstream users of the Tempe Town Lake and the Salt River bed. The downstream dams
are then lowered, releasing water from the lake and westward down the Salt River channel.
Floodwater is then allowed to flow through the lake. The dams are inflated once the flood
nears its end, capturing the tail waters of the flood and refilling the lake.
Additional Uses
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Inflatable
dams have a multitude of uses. Among them are hydroelectricity,
groundwater recharge, water supply, flood control, sewage diversion, irrigation, water
diversion, water treatment, recreation and tidal barriers. The most common applications
are for expanding the capacity of existing dams and replacing older dam structures.
These dams are best used in small to medium sized watercourses where width is much
greater than height. The advantage of inflatable dams is that they allow for long spans of
barrier with few structural piers (that might interfere with floodwater). They can easily
attach to any side slope and are relatively simple to install. Inflatable dams have low
maintenance requirements and high longevity. Unlike other dam designs, these dams have few
moving parts which means there is less lubrication, replacement and repair costs and less
corrosion.
Where in the world
Just two manufacturers in the world make this product: Japan's
Bridgestone and Sumigate. The City of Tempe purchased a inflatable dam
system consisting of eight bladders from Bridgestone for the
Tempe Town Lake. It took a full year of the plant's capacity to produce and ship these
from the plant in Japan. |
Inflatable dam technology has been available for 30 years and more than 2,200
inflatable dams are in use around the world. Some of these locations are: |
IKjeldal, Lunde and Oslo, Norway
Sanvicente Lianera Nueva Ecija, Philippines
Hatsuka River in the Hyogo Prefecture, Hakone, Japan
Tsudae Dam at Lake Biwa, Japan
Suminose Dam at the Inou River, Japan
Mogami "Samidare" Weir, Japan
Brantas River, Indonesia
Kumhogang, Shin Chon #4 and Sa Yeon, Korea
Mirani and Boddington, Australia
Tauranga, New Zealand
Sissiboo Falls and Nairn Falls, Canada
Kan Tin and Yuen Long, and Beas River, Hong Kong
Reimei Irrigation and Peinan, Taiwan
Missouri River at Great Falls and Toston, Montana
Weeks Falls and Snoqualmie River, Washington
Detroit, Michigan
Altoona City and Susquehanna River Pennsylvania
Sand Creek, Kansas
Palmer Falls and Hudson River, New York
San Gabriel, Alameda County, Citrus, Felton Dam, Covina, Pico Rivera, Los Angeles and Pit
River, California
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