Difference between revisions of "WATER QUALITY"

The combination of the record five-year drought (1999-2004) and above average runoff into Lake Powell during the spring and summer of 2005 put large amounts of sediment and organic matter from the reservoir's delta into the lake. These substances consumed oxygen as they decay which, in turn, resulted in declining dissolved oxygen concentrations in the Colorado River immediately below the dam. While this phenomenon occurs to some degree every summer and fall, oxygen levels in 2005 reached a level that caused concern for the health of the trout fishery in the river below the dam.

As the river moves downstream, the water cascades through rapids, quickly raising the dissolved oxygen levels, so there is less impact or concern for endangered native fish in the reaches of the Grand Canyon. However, there may be some impact to the non-native trout fishery as fish remaining near the dam become lethargic or temporarily move downstream to more oxygen-rich waters.

Reclamation conducted short-term experiments to evaluate the relationship between dam operations and dissolved oxygen concentrations. Researchers from the Grand Canyon Monitoring and Research Center determined if low releases spread among varying numbers of generating units will inject more oxygen into the water. The turbines draw some air during operation, especially when operated at very low output levels. Various operational combinations of three to five units were tested.

While some changes in dissolved oxygen were been noted as a result of the experiments, a concern also has emerged. Operating the units at very low levels is both inefficient and damaging. Because the generating units were designed to operate efficiently only at higher releases, normal operations for low flows would be met by using fewer units. If the units are operated at too low a level, the risk of damage to the turbines increases significantly. While units have been operated that low in the past for various system and emergency reasons, every effort possible has been made to minimize the length of such operations to protect the generating units. Additionally, such "rough operation" also is inefficient in both the generation of power and the use of water.

The results of these studies indicate the turbines can contribute to improved dissolved oxygen concentrations in the water being released from the reservoir. The studies remain inconclusive concerning the best balance of turbine operations, or whether other alternatives should be developed.

The issue of declining dissolved oxygen becomes less of an issue by October or early November when the water in Lake Powell "turns over." This happens when the cooling air temperatures and seasonal winds mix reservoir waters, essentially causing the upper, better oxygenated water to mix with the lower level water that contains low oxygen. [1]

• Colorado River at Lees Ferry
• Colorado River at 30 mile
• Colorado River above LCR
• Bright Angel Creek
• Kanab Creek
• Havasu Creek
• Colorado River abv National Canyon
• Colorado River bl Diamond Creek
• Colorado River abv Spencer rm246

2015

• Water Quality in Lake Mead and Upstream Influences: Dissolved Oxygen during 2014
• Streamflow, Water Quality, and Sediment Transport in the Colorado River Ecosystem
• Glen Canyon Physical Environment Update – Water Quality, Tributary Influences & Channel Analyses & Flows

2014

• How the 2014 HFE and other types of operations affect water quality parameters such as dissolved oxygen (DO) and temperature below Glen Canyon Dam.

2005

• Reclamation to continue experimental operations at Glen Canyon Dam; Efforts address low dissolved oxygen levels below dam

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