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WSP04469
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Last modified
1/26/2010 12:55:36 PM
Creation date
10/12/2006 12:22:46 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8062
Description
Federal Water Rights
State
CO
Basin
Statewide
Date
2/20/1988
Author
J Schall P Lagasse
Title
Application of the Forest Service Channel Maintenance Flow Procedure
Water Supply Pro - Doc Type
Report/Study
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<br />0_( . <br /> <br />','. <br />...r'. <br />. <br />.. <br />~j'.. i <br />~.t .", /' <br /> <br />1723 <br /> <br />. fraction. (Fig. 4) were typical of all size classes and indicated that. <br />transport capacity was 1-2-orders of magnitude greater than supply. <br /> <br />The next step was to evaluate how much tbe discharge could be reduced <br />under post-project conditions without occurrence of aggradation. It was <br />assumed that the reservoir would trap all particles in the gravel size <br />fraction. .Additionalry, based on Andrews' conclusions and lack of signifi- <br />cant tributary sediment sources below the reservoir (within the forest <br />boundary), it was assumed that there would be an insignificant supply of <br />the gravel size fraction below the reservoir. Using the calibrated trans- <br />port relationships, the discharge required to move the remaining sediment <br />supply was then evaluated for both sites A and B. Results indicated that <br />85 cfs would be required below Site A to move all the pre-project supply of <br />sed1cent finer than gravel, while 10 cfs would be required below Site B. <br />To move all pre-project sediment supply (including gravels) would require <br />30 cfs below Site B, a value that is considered a very conservative main- <br />tenance flow requirement. Cnannel stability under .these flow conditions <br />waS not considered to be impacted since the existing channel. (supply. <br />limited) is stable.. probably due to armoring by coarse particles, <br /> <br />VEGETATION ENCROACHMENT <br /> <br />The above results suggested that a relatively small discharge would <br />adequately prevent sediment deposition in the channel downstream of the <br />project. Therefore, the flows required to minimize vegetation encroachment <br />became the controlling factor in defining required bypass flows. It is <br />generally accepted that established vegetation cannot survive long periods <br />of submergence or mean velocities higher than 5-& fps. Under pre-project <br />bankfull conditions (190 cfs), the mean velocity was 3.7 fps; therefore, it <br />was concluded that a 16-day bypass time period (calculated from strict <br />application of the Chapter 30 procedure) provided an adequate length of <br />submergence to minimize vegetation encroachment. Under the post-project 85 <br />cfs flow necessary to prevent aggradation below Site A, the velocity is <br />only 2.5 fps. Therefore, this flow would also be required for 16 days to <br />minimize vegetation encroachment below the waterline. The 85 ds flow <br />covers 98 percent of the pre-project bankfull wetted perimeter; conse- <br />..quently, it can be concluded that a post-project flow of 85 ds below Site <br />A is as effective as a channel maintenance flow as 190 cfs was for the <br />pre-project condition. <br /> <br />For Site B the 10 cfs flow required .to prevent aggradation leaves a <br />large portion of the channel bed exposed which could be encroached on by <br />vegetation. Under the 30 cfs flow required to transport all the pre-project <br />sediment supply, 74 percent of the pre-project wetted perimeter is covered. <br />To provide a more significant submergence factor would require about 50 <br />cfs, for which 89 percent of the pre-project wetted perimeter is covered. <br />Based on these results, a 50 cfs bYPass for 16 days was considered neces- <br />sary to control a majority of the vegetation encroachment below Site B. <br />
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