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Last modified
7/14/2009 5:02:28 PM
Creation date
5/20/2009 1:37:40 PM
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UCREFRP
UCREFRP Catalog Number
1400
Author
Simons, D. B., et al., ed.
Title
Proceedings
USFW Year
1980.
USFW - Doc Type
Workshop on Downstream River Channel Changes Resulting From Diversions or Reservoir Construction.
Copyright Material
NO
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<br /> <br /> <br />,~<~,...-..:..... ~ ~ ::~...-. <br /> <br />..<..;.-~:'i.-~~i~; ,~,~ ,'.' , <br /> <br />_< > _ ~- :,t -,',':.. -":'-_r~:<<_;_,:Y'"?::'{;'.-:>:____,,-;~ _.~'~ ,,; -: <br /> <br />~_".: .;: '.:., .i;'.-;;~,:-_.,4,,"~f',''''-'';'-- ..'lo,~::~'';:''~~i.~,~-_,;:.;,~r~';G..:\:;~i.~~~:':~5-:;'''-'\c;..~~;_......''':';:'.;_{_:'_;-,;~'" <br /> <br />with sand and gravel depending upon the extent of backwater from the <br />Little Snake River. <br /> <br />Far Reach No.3, significant changes could occur. The construction <br />of earns on the Yampa River will result in reduced bed material transport <br />capacity. Because the supply of bed load from the Little Snake will not <br />change, the Yampa may aggrade at the confl uence. Also, if the peak <br />flows on the Yampa are reduced significantly, then upstream progressing <br />degradation will occur on the Little Snake during corresponding high <br />flows (Figure 3). Therefore, it is probable that the Yampa River will <br />aggrade in Reach No.3, this would create backwater effects up the Yampa <br />a~d drown out the r1ffles. With this flow situation, sands and gravels <br />moved into the pools will probably stay there, at least until high flows <br />are released from the reservoi rs. In regard to channel confi gurat ion <br />and meander pattern in Reach No.3, it is difficult to predict changes <br />that may occur. The maps are inadequate to clearly ascertain historical <br />shifting of the ~hannel. Air photos over a time span are essential to <br />evaluate the lateral stability of the river. Also, the magnitude, <br />frequency and duration of releases from the reservoirs must be known in <br />order to attempt to predict future channel configuration. In qual ita- <br />t1vs terms, it appears that the channel pattern is controlled by <br />bQulders along the river banks and reduced flows will produce relatively <br />l1ttle change. However, if aggradation takes place at the confluence, <br />then the build-up of channel bars will deflect currents into the banks <br />resulting in some change to the channel pattern. The pattern below the <br />confluence is likely to have several distinct channels flowing adjacent <br />to bars and islands. <br /> <br />In order to carry out further detailed analysis, however, more data <br />are required. <br /> <br />ADDITIONAL DATA REQUIREMENTS <br /> <br />The fo 11 owi ng data are required in order to ana lyze the vari QUS <br />river reaches and tQ predict river changes. <br /> <br />Little Snake River <br /> <br />x <br />X <br /> <br />x <br /> <br />x <br /> <br /> <br /> <br />i <br /> <br />. <br /> <br />! <br />I <br />. ~.=..-: <br />
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