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Last modified
7/14/2009 5:02:36 PM
Creation date
5/20/2009 3:22:13 PM
Metadata
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Template:
UCREFRP
UCREFRP Catalog Number
9605
Author
Schmidt, J. C. and e. al.
Title
Flow Recommendations for the White River, Utah-Colorado Draft Report.
USFW Year
2002.
USFW - Doc Type
Logan, UT.
Copyright Material
NO
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<br />Haines, and Tim Modde, U.S. Fish and Wildlife Service. The individual reports addressed <br /> <br />separate objectives and are presented as individual, complete studies that stand alone. <br /> <br />Study findings: <br /> <br />An integrated flow recommendation was determined through these two independent <br /> <br />stduies, one to evaluate the peak flows needed to maintain channel stability and diversity, and the <br /> <br />second to identify a minimum base flow needed to maintain habitat for the Colorado pikeminnow <br /> <br />population. <br /> <br />Channel maintenance flow/high flow recommendations: There are two approaches to <br /> <br />determining the discharges necessary to maintain channel diversity. One is to directly measure <br /> <br />channel bed movement measuring sediment transport and bed scour and fill in those parts of the <br /> <br />channel that are critical habitat. A second is to determine those discharges at which habitats are <br /> <br />maintained on typical alluvial streams. We pursued both in these studies. <br /> <br />Several lines of evidence indicated that a high-flow component of an instream flow <br /> <br />should preserve most of the natural flow regime greater than approximately 40 m3/s (~1 ,400 <br /> <br />ft3/s). <br /> <br />Historical discharge and depth records at our study site near the Watson, Utah U.S. Geological <br /> <br />Survey gage showed that flows of this magnitude scoured the bed, and thus flows greater than <br /> <br />this were capable of transporting fine bed sediment. We inferred that bedload movement <br /> <br />occurred at 51 m3/s (1,800 ft 3/S), because bedforms were detected on fathometer traces at those <br /> <br />cross sections with fine-grained bed material at this discharge. <br /> <br />The White River is a sediment supply-limited stream, becau~e much more suspended <br /> <br />4 <br />
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