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Last modified
1/26/2010 12:55:06 PM
Creation date
10/12/2006 12:17:51 AM
Metadata
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Template:
Water Supply Protection
File Number
8210.110.60
Description
Colorado River Water Users Association
Basin
Colorado Mainstem
Date
12/6/1951
Author
CRWUA
Title
Proceedings of the 8th Annual Conference
Water Supply Pro - Doc Type
Annual Report
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<br />silt. Thorough investigation of the evaporation phenomenon is in progress. <br />Precise leveling disclosed that the whole country covered by the lake had <br />subsided a maximum of 7 inches. <br /> <br />Gradual filling of the storage space with sediment is not the only <br />silt problem introduced by construction of Hoover Dam and of Davis, Parker, <br />and Imperial Dams downstream. Through the centuries the bed of Colorado <br />River had adjusted itself to transportation of large volumes of silt. In <br />order to moye this weight, a relatively steep slope was required. As the <br />dams were closed, and silt deposited in their reservoirs, the water dis- <br />charged through the dams or power plants became clear. Since transport of <br />clear water'required a flatter slope than transport of a water and silt <br />mixture, the river began to readjust its slope. Establishment of the flatter <br />slope downstream meant lowering of the river bed below the dams. Silt thus <br />removed from the river bed is deposited in the reservoir next downstream. <br />In such depositions the coarser silt is deposited in the upper reaches of <br />the reservoirs, forming deltas similar to those where silt-laden rivers <br />enter the ocean. The result is that the river bed upstream from the reservoir <br />becomes aggraded, a phenomenon which, over a sufficient length of time, may <br />extend a gr~at distance. The initial result of removal of the silt load is, <br />therefore, that the river bed becomes lowered downstream from dams and raised <br />upstream from reservoirs. <br /> <br />Lowering of the river bed at an existing gravity diversion may <br />render the diversion no longer possible without a dam. This has occurred <br />at the point of diversion for the Palo Verde Irrigation District. To save <br />this fertile area from destruction due to lack of water, Congress appropriated <br />funds for construction of a temporary diversion dam to maintain the water sur- <br />face elevation at the canal intake in spite of the general lowering of the <br />river bed below Parker Dam. On the other hand, the river bed is increasing <br />its elevation at the drainage outlet from the District. Temporary river <br />rectification has been carried out to provide relief pending a more extensive <br />project. <br /> <br />A large storage dam may also cause serious problems downstream by <br />the elimination of flood flows which, in the natural state, served to clean <br />the river bed of accumulated vegetation and silt. This and other causes <br />brought about by construction of Hoover Dam, added to the delta formation <br />upstream from Parker Dam reservoir, created a serious situation along the <br />river between Needles, California, and Topock, Arizona. A true river bed <br />ceased to exist and the water found its way through innumerable sloughs, <br />creating a virtual swamp. To remedy this condition and protect Needles and <br />the Santa Fe Railroad, which parallels the river, the Government in 1948 began <br />a dredging project, which is nearing completion. The water surface at Needles <br />has already, dropped six feet. Large areas of land adjacent to the river, which <br />had become water-logged, are now suited for growing crops. <br /> <br />Th~s short outline of problems on the Colorado River shows that con- <br />struction of dams' to control floods and silt does not prevent other problems <br />from arising which require extensive and continuous remedial works and main- <br />tenance. <br /> <br />*********** <br /> <br />-37- <br />
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