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Last modified
1/26/2010 4:18:48 PM
Creation date
2/12/2008 12:55:19 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8282.300
Description
Colorado River Operations and Accounting - Lower Basin Administrative Procedures
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
8/1/1996
Author
DOI-BOR
Title
Description and Assessment of Operations-Maintenance and Sensitive Species of the Lower Colorado River - Volume II - Appendices-Etc - 08-01-96
Water Supply Pro - Doc Type
Report/Study
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Ou2541 <br /> <br />APPENDIX C - RIVER WORK AND MAINTENANCE <br /> <br />Introduction and Past History <br /> <br />Prior to construction of flood control and storage dams on the Colorado River, the lower <br />river from the present site of Hoover Dam to the Gulf was typical of a river carrying a heavy <br />sediment load over an alluvial bed. Before the dams, the river was actively building up the <br />alluvial valleys by repeated inundation when the spring snowmelt flowed from the upper <br />river basin. Each annual flood caused the river to meander across the alluvial valleys, <br />cutting and depositing material in the classical meander patterns. During the ebb of the flood <br />the river typically deposited a remainder of its sediment load on the valley floor. <br /> <br />The dams impounded the heavy load of sediment the river historically carried down from the <br />upper basin, and significantly reduced the flood flows which canied most of the sediment <br />through the system. The clear water released from the dams entered the channel practically <br />free of sediment and immediately began acquiring a new sediment load. The dams caused <br />the residual coarse sediment in the river to be redistributed with the result that farther <br />downstream, below each dam, the quantity of sediment was sufficient that the river continued <br />the natural process of meanders and aggradation. <br /> <br />Although river maintenance work started near Yuma, Arizona, prior to 1925, Congress did <br />not pass the CRFWLS Act until March 3, 1925. The present authority under which <br />Reclamation operates the Colorado River Front Work and Levee System is the Act of <br />June 28, 1946. This act authorized appropriations for controlling the floods, improving <br />navigation, maintaining the banks of the Colorado River, dredging and straightening the river <br />channel, and conducting studies necessary to fulfill the foregoing objectives. <br /> <br />The physical control and training of the lower Colorado River have generally been <br />accomplished by the construction of the system of levees, river realignment, and river <br />control structures. River control structures include bankline reinforcement, riprap, jetties, <br />and training structures. The dredging activities have been used for channel realignment, <br />development of material for levee construction, sediment control, and environmental <br />enhancement. <br /> <br />Reclamation's Yuma Area Office (Y AO) is responsible for maintenance of the Colorado <br />River from the SIB to Davis Dam which is approximately 276 river miles. Each year Y AO <br />performs an inspection of the Colorado River and identifies bankline areas, levees, and river <br />structures that require maintenance (Table C-I). For this ongoing maintenance activity on <br />the river and levees, Y AO has a need for up to 60,000 cubic yards of riprap and up to <br />20,000 cubic yards of gravel per year. Normally Reclamation crews perform the <br /> <br />Appendix C - 1 <br />
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