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WSP05494
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Last modified
1/26/2010 2:18:36 PM
Creation date
10/12/2006 1:04:29 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8407.700
Description
Platte River Basin - River Basin General Publications - Republican General Publications
State
CO
Basin
South Platte
Water Division
1
Date
5/1/1963
Author
Corps of Engineers
Title
Review of Report on Republican River and Tributaries - Colorado-Nebraska and Kansas
Water Supply Pro - Doc Type
Report/Study
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<br />0022~_2 <br /> <br />. <br /> <br />SECTION VI - PRESENT CHANNEL CONDITION <br /> <br />17. FACTORS CONSIDERED <br /> <br />During the investigation, the problem of channel deterioration <br />was presented to the Missouri River Division Board of Sediment Con- <br />sultants to inquire if similar problems had been encountered else- <br />where and to solicit suggestions on various phases of the <br />investigation, especially the correlation with the sediment transport <br />characteristics of the stream. Although the Republican River may <br />be considered a typical, sand-bottom meandering stream with a <br />moderately heavy sediment load, a comparable channel deterioration <br />situation does not appear to have been encountered and rectified <br />elsewhere. Therefore the changes which have occurred during the <br />past decade, as compared with the natural stream regimen, were <br />studied as a basis for project formulation. The investigation <br />covered streamflow variations, sediment loads, the nature of the <br />bed and bank materials, the effects of reservoir operation, channel <br />configuration and hydraulic efficiency, and the probably efficacy <br />of an improvement project. A detailed discussion of the study is <br />given in Appendix IV: Hydrology and Hydraulics. <br /> <br />18. STREAMFLOW AND SEDIMENT TRANSPORT <br /> <br />~. Streamflow. As stated previously, the Republican River <br />has had a history.of extremes in the rate and amount of streamflow. <br />With these fluctuations, there have been changes in the channel <br />shape and capacity. In past years, the shifting channel has devel- <br />oped sandbars and islands, and during low-flow periods these have <br />supported a growth of willows and other vegetation. Then, subsequent <br />flood flows have denuded the bars and islands and even eroded them in <br />the meandering process. One result of these cycles has been a <br />fluctuation in the stage-discharge relationship, as the bankfull <br />capacity of the river increased and decreased. However, during the <br />past decade, flood flows were practically eliminated by reservoir <br />operation; the total runoff was diminished by the drought; willows, <br />cottonwoods and other vegetation became established within the chan- <br />nel, and the obstructions reduced the bankfull capacity of the <br />channel. Reservoir regulation will not only control floodflows at <br />the damsites and prevent all but residual flood damage, but also <br />will eliminate the flushing effect of major floodflows. As a result <br />of the curtailment of flushing, the deteriorated channel may be <br />expected to persist unless steps are taken to reestablish all or <br />part of the former capacity. <br /> <br />k. Sediment load and bed material. Streamflow and sediment. <br />load are closely related. A program of suspended sediment sampling <br />has been maintained on the Republican River since before the reser- <br />voir construction. On a few occasions in the past, samples have <br /> <br />. <br /> <br />23 <br />
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