Glen Canyon Dam viewed from inside lower Glen Canyon
Glen Canyon Dam, a concrete arch dam on the Colorado River in the American state of Arizona, is viewed as carrying a large amount of risk, most notably due to siltation.[citation needed] The Colorado and San Juan rivers deposit large volumes of silt into Lake Powell, slowly decreasing its capacity. The sediment will eventually build up against the dam and could affect its safe operation and lead to its failure.[1]
The dam, anchored in unstable[citation needed]Navajo sandstone (sometimes said to be "solidified sand dunes"),[2] nearly failed in 1983 as the result of a flood on the upper Colorado River that led to extended use of its tunnel spillways. The spillways, designed for short-term use, soon underwent cavitation and began to fail. Emergency installation of 8-foot (2.4m) flashboards and other efforts narrowly averted total failure.
Siltation, concrete degradation, spillway operational problems, and unstable dam abutments are all key factors that affect the safe operation of the dam.[3][failed verification] It is estimated that a breach of the dam would produce a floodwave that would overtop the Hoover Dam.[1][4] The dam's useful lifespan has been estimated by some to be 85 to 100 years, and was described as "America's most regretted environmental mistake" by David Brower, then-head of the Sierra Club.[5] Different estimates by the Bureau of Reclamation and others suggest a lifespan of between 500–700 years.[6]
Glen Canyon Dam is a concrete arch dam on the Colorado River in northern Arizona in the United States, just north of Page. The dam was built to provide hydroelectricity and regulate the flow of the river from the upper Colorado River Basin into the lower. The Lake Powellreservoir is the second largest artificial lake in the country, extending upriver well into Utah. The dam is named for Glen Canyon, a colorful series of gorges, most of which now are buried under the reservoir.
Construction of Glen Canyon Dam began in 1956 and was finished in 1966. When the reservoir filled, the dam began to deliver a steady, regulated flow of water downstream and generate a cheap, plentiful supply of electricity. In 1983, major floods nearly destroyed the two tunnel spillways that could have led to the dam's collapse, but disaster was averted by a close margin. By taming floods that were characteristic of the Colorado River, the dam has led to major physical and ecological changes in the lower river. Controversy continues over the positive and negative effects of the dam.
The Colorado River carries an estimated 45 million tons of sediment annually at Glen Canyon,[7] and as Lake Powell is the farthest large reservoir upstream on the Colorado River mainstem,[8] the sediment load is completely trapped in the reservoir as the Colorado discharges into it. This sediment is creating a steadily advancing "toe" of sediment, i.e. an underwater alluvial fan, that is advancing towards the dam. Some estimates by conservationists predict that the sediment will reach the dam base in about 80 to 100 years, while others made primarily by government agencies estimate it will take as long as 500 to 700 years.[1] It will take still longer for the sediment to accumulate to the point where it could clog the outlet works, which are the lowest openings in the upstream face of the dam.[1]
Some critics predict that if the water level then drops, it may fall below the penstock openings, which are higher up on the dam face, which will cause the release capacity of the dam to drop to zero. This would dewater the Colorado River bed below the dam which would remain dry until the next major spring inflow. Only springs, seeps and tributaries such as the Paria, Little Colorado and Virgin River would supply the river flow during these times, perhaps causing unprecedented drops in levels of Lake Mead as well.[1]
The primary failure mode for Glen Canyon dam will likely be an overtopping one spring caused by insufficient storage capacity (either a huge inflow, bigger than 1983, or insufficient storage capacity because the lake was too full of either water or sediment).[citation needed]
Colorado River Delta today, showing inflows mostly from the Hardy River and other Mexican tributaries
An example of the fast deposition rate of Colorado River sediment is found in Lake Mead itself, where, before the completion of Glen Canyon Dam, ten percent of its storage was already compromised by sediment. When Lake Powell levels drop, sediments deposited in its upper reaches are carried into the receding water by the Colorado and its tributaries. One large flash flood caused by heavy rainfall could move all or most of these sediments into Lake Powell, creating a sudden loss of storage capacity. One way to control sediment flow in the reservoir, without removing the dam outright, is by dredging.[9]
1983–84 flooding
In May 1983, three years after Lake Powell was first filled, an unusually long-lasting winter due to the 1982–83 El Niño event produced increased snowfall over the entire 108,335-square-mile (280,590km2) multi-state Colorado River basin. Dam engineers anticipated a normal winter, and maintained reservoir levels at their usual levels through the winter.[10]
Inflow capacity
Spring ended with a sudden influx of warm weather and then rain. The combination of rain and snowmelt eventually produced a combined inflow into Lake Powell of over 111,500 cubic feet (3,160m3) per second.[11]
The average annual peak flow prior to 1963 was 93,400 cubic feet (2,640m3) per second.[12] The Bureau of Reclamation states that the highest inflow the Glen Canyon Dam can withstand is 697,000 cubic feet (19,700m3) per second, almost seven times the 1983 total. [6]
Outflow capacity
Glen Canyon Dam has two tunnel spillways capable of allowing 276,000cuft/s (7,815m3/s) to bypass the dam's regular spillways.[13] The spillway tunnels were excavated around both abutments of the dam, dropping steeply from their control gates on Lake Powell to connect with the lower reaches of the diversion tunnels, which were utilized as the lower ends of the dam's spillways. This measure saved cost, but introduced a weak point at the elbow where the two tunnels intersected. The upper ends of the diversion tunnels were then sealed with a solid concrete "plug".[14]
While this made the spillways more economical to construct, they had less capacity in part because engineers must maintain at least 30 percent clearance between the water level and the tunnel ceiling.[15] in addition to the tunnel spillways, the dam has a set of river outlet works designed to release 15,000 cubic feet (420m3) per second.[6] The dam also releases water through the dam's power turbines, which are capable of releasing 31,500 cubic feet (890m3) per second.[16] The official spillway capacity is 208,000cuft/s (5,900m3/s).[17]
Tunnel spillways damaged
The releases from Glen Canyon Dam in May 1983
At first, as inflows exceeded normal levels, the US Bureau of Reclamation engineers opened penstocks to full release. When inflow rates continued to rise, they also opened the river outlet works. The reservoir continued to rise.
Reclamation Bureau officials met in late June and agreed that the maximum water level the dam could handle was 3,708 feet (1,130m). At that level they feared they could not control the spillway gates.[10] The engineers decided to raise the floodgates controlling the tunnel spillways. This became the first time that the spillways had ever been used for their intended purpose. Volume initially ran at 20,000 cubic feet (570m3) per second per tunnel. After several days, noticeable vibrations were felt in the dam wall and surrounding rock. Water exiting the spillways contained noticeable debris, including sandstone, signaling severe erosion taking place within the tunnels.[18]
Reclamation responded by reducing releases by half, however, the rumblings continued. The noise was so noticeable that a worker in the employee dining room, located near the power plant, reported that it "sounded like the barrages that he had experienced in Vietnam".[18] The engineers soon closed the spillways for an inspection.[15]
Cavitation damage found
Inspection crews were lowered down the spillway tunnels in a small cart to assess damage. They found that cavitation, a known risk associated with tunnel spillways, had severely damaged and eroded the 3-foot (0.91m)-thick concrete tunnel lining. In some locations the cavitation had exposed the soft sandstone.
The tunnels could not be kept closed as more rain fell in the Colorado River Basin and the reservoir continued to rise. Reclamation reopened the left spillway, allowing 12,000 cubic feet (340m3) per second; the right, which had suffered worse damage, was only permitted to carry 4,000 cubic feet (110m3) per second.
Emergency flashboards installed
As the reservoir level increased, plywood flashboards were installed on top of the spillway gates. They allowed reservoir water to rise 4 feet (1.2m) without increasing releases.
Tunnels damaged further
The left tunnel, however, was suffering further damage, described as a "surging, boiling flow that filled the portal".[15] The tunnel had formed a hydraulic jump as it was turned into a "pressure conduit" by the surging flow of water. The interior erosion threatened to collapse the tunnel. Engineers knew that increasing the flow would decrease the turbulence but would further damage to the tunnel walls. To increase the reservoir's capacity further, engineers began an emergency effort to add 8 feet (2.4m) to the height of the spillway gates, avoiding increasing the rate of water releases.[15]
Spillway gates at Glen Canyon Dam during 1983 flood. Note the flashboards installed atop to prevent water from overtopping the gates.
Diversion tunnel threatened
The force of the water at the left tunnel eroded concrete near the diversion plug, a device that blocked the diversion tunnel used during construction. The Bureau of Reclamation was concerned that the water would eventually erode the diversion plug altogether, creating a connection to the reservoir floor. This uncontrolled spillage would cause the reservoir to drain, creating a catastrophe.
As the discharges from Glen Canyon Dam reached almost 90,000 cubic feet (2,500m3) per second, with 32,000 cubic feet (910m3) per second racing through the left spillway,[11] the 9,500,000 acre-feet (11.7km3) of flood storage space behind Hoover Dam downstream was exhausted.[19]
Lake Powell reaches peak level
On July 15, 1983, Lake Powell reached its peak level, 3,708.34 feet (1,130.30m) about 8 inches (200mm) from where engineers thought they'd lose control. The water held steady for a few days and then gradually declined.[10] Inflows to Lake Powell topped 120,000 cubic feet (3,400m3) per second,[11][18] while releases from Glen Canyon Dam topped 92,000 cubic feet (2,600m3) per second. Eventually, Hoover Dam was also forced to open its gates; its discharge peaked at 40,000 cubic feet (1,100m3) per second and still caused downstream flooding. As inflow lessened at the end of the season, dam engineers were able to draw Lake Powell down below critical levels.
Tunnel spillways seriously damaged
Glen Canyon Dam during the 1984 flood
Inspections of both spillways found severe damage. In the more badly damaged left spillway, inspection crews discovered a 32 feet (9.8m) deep, 40 feet (12m) wide, and 150 feet (46m) long hole.[11][15][18]
Repairs and solutions
After the flood, it was suggested that the flashboards atop the spillway gates should be replaced with stronger boards and kept permanently; this would allow an "insurance" against a 1983-reminiscent flood.[16]
Air slots added to tunnels
Research by the Bureau of Reclamation found that an air slot at a specific point in each spillway tunnel would introduce air bubbles that would prevent cavitation and resultant shockwaves. Spillway upgrades and repairs commenced immediately after the 1983 floods receded and continued through the winter of 1983–84. Through the winter, heavy snowpack was reported in the upper Colorado basin. It was feared that this would produce a flood greater than the 1983 one, and as the spillway repairs continued, water was constantly released through the dam power plant and outlet works, a rate of roughly 45,000 cubic feet (1,300m3) per second. [20]
1984 floods possible
The engineers allowed Lake Powell's level to fall to allow for the next winter's snowmelt. When the snowpack began to melt in spring of 1984, water levels reached several inches below the top of the flashboards in late June. As summer continued, inflows decreased and the reservoir level began to decrease.
On August 12, 1984, construction teams completed repairs to the left spillway. It was tested at 50,000 cubic feet (1,400m3) per second for several days. No noticeable damage was found in the spillways.[21]
Lake Powell with "bathtub ring"
Aftermath
The 1983 flood, although it nearly caused a catastrophic disaster, was a "relatively small flood".[22] It was, in fact, only a 25-year flood, or a flood that has a four percent chance of occurring in any given year.[11][18]
Impact of dam failure
In 1990, the Bureau of Reclamation prepared a study of a Glen Canyon Dam failure. They predicted that if Lake Powell were at high pool, about 27,000,000 acre-feet (33km3) of water would surge out of Lake Powell at an initial depth of over 500 feet (150m). Downstream communities and possibly every dam along the river, including Hoover Dam forming Lake Mead, Davis Dam forming Lake Mohave, Parker Dam forming Lake Havasu, Palo Verde Dam, and other dams and reservoirs, as well as riverside lowlands, would be inundated or severely damaged.[8] The resulting flood would scour the bottom few hundred feet of the Grand Canyon.[1]
Glen Canyon Dam is the central element of the Colorado River Storage Project. If it failed, the resulting damage could limit or completely cut off water supply to residences or farmlands along the Colorado River, and depending on damage to canal headworks, even cut off water to southern California.[8]
Related Research Articles
The Colorado River is one of the principal rivers in the Southwestern United States and in northern Mexico. The 1,450-mile-long (2,330 km) river, the 5th longest in the United States, drains an expansive, arid watershed that encompasses parts of seven U.S. states and two Mexican states. The name Colorado derives from the Spanish language for "colored reddish" due to its heavy silt load. Starting in the central Rocky Mountains of Colorado, it flows generally southwest across the Colorado Plateau and through the Grand Canyon before reaching Lake Mead on the Arizona–Nevada border, where it turns south toward the international border. After entering Mexico, the Colorado approaches the mostly dry Colorado River Delta at the tip of the Gulf of California between Baja California and Sonora.
Mansfield Dam is a dam located across a canyon at Marshall Ford on the Colorado River, 13 miles (21 km) northwest of Austin, Texas. The groundbreaking ceremony occurred on February 19, 1937, with United States Secretary of the Interior Harold L. Ickes attending. The dam was a joint project by the Lower Colorado River Authority (LCRA) and the United States Bureau of Reclamation, with partial funding provided by the Public Works Administration. Brown and Root, headed by James E. Walters, Sr., was the prime contractor. The dam was completed in 1941. Originally called Marshall Ford Dam, the name was changed in 1941 in honor of United States Representative J.J. Mansfield. The reservoir behind Mansfield Dam is named Lake Travis. The dam is owned and operated by the LCRA.
Glen Canyon Dam is a concrete arch-gravity dam in the southwestern United States, located on the Colorado River in northern Arizona, near the city of Page. The 710-foot-high (220 m) dam was built by the Bureau of Reclamation (USBR) from 1956 to 1966 and forms Lake Powell, one of the largest man-made reservoirs in the U.S. with a capacity of more than 25 million acre-feet (31 km3). The dam is named for Glen Canyon, a series of deep sandstone gorges now flooded by the reservoir; Lake Powell is named for John Wesley Powell, who in 1869 led the first expedition to traverse the Colorado River's Grand Canyon by boat.
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1 2 3 4 5 "Canyon Legacy"(PDF). Journal of the Dan O' Laurie Museum of Moab. www.riversimulator.org. Archived(PDF) from the original on 2012-07-26. Retrieved 2009-05-28.
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